{"status":"ok","message-type":"work-list","message-version":"1.0.0","message":{"facets":{},"total-results":1152,"items":[{"indexed":{"date-parts":[[2022,3,31]],"date-time":"2022-03-31T22:01:59Z","timestamp":1648764119130},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"1","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/2074","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Special Issue: Magdalen Basin Project - Foreword"],"prefix":"10.4138","volume":"32","author":[{"given":"Peter S.","family":"Giles","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Graham L.","family":"Williams","sequence":"additional","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1996,4,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/2074\/2438","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/2074\/2438","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T14:19:55Z","timestamp":1638454795000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/2074"}},"issued":{"date-parts":[[1996,4,1]]},"references-count":0,"journal-issue":{"issue":"1","published-online":{"date-parts":[[1996,4,1]]}},"URL":"https:\/\/doi.org\/10.4138\/2074","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1996,4,1]]}},{"indexed":{"date-parts":[[2022,3,31]],"date-time":"2022-03-31T10:50:11Z","timestamp":1648723811992},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"1","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/1925","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Editor's Page"],"prefix":"10.4138","volume":"13","author":[{"given":"B. R.","family":"Pelletier","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1977,4,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1925\/2289","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1925\/2289","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:14:23Z","timestamp":1638458063000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1925"}},"issued":{"date-parts":[[1977,4,1]]},"references-count":0,"journal-issue":{"issue":"1","published-online":{"date-parts":[[1977,4,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1925","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1977,4,1]]}},{"indexed":{"date-parts":[[2022,3,30]],"date-time":"2022-03-30T10:43:53Z","timestamp":1648637033518},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"2","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/1765","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Meetings"],"prefix":"10.4138","volume":"4","member":"12607","published-online":{"date-parts":[[1968,7,31]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1765\/2129","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1765\/2129","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T17:01:58Z","timestamp":1638464518000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1765"}},"issued":{"date-parts":[[1968,7,31]]},"references-count":0,"journal-issue":{"issue":"2","published-online":{"date-parts":[[1968,7,31]]}},"URL":"https:\/\/doi.org\/10.4138\/1765","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1968,7,31]]}},{"indexed":{"date-parts":[[2022,4,1]],"date-time":"2022-04-01T23:56:09Z","timestamp":1648857369642},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"1","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"abstract":"<jats:p>Lead isotope analyses have been determined for galenas which occur in small quantities in quartz veins in the Goldenville Formation of the Meguma Terrane, and also for five whole rock samples from this formation- The ten least radiogenic galenas are homogeneous in isotopic composition, and they plot close to the average terrestrial growth curve of Stacey and Kramers and the \"orogene\" curve of Doe and Zartman. The mean model ages are 550 Ma (Stacey and Kramers) and 600 Ma (Doe and Zartman), which are in approximate agreement with the Cambro-Ordovician age of deposition of the sediments. The close position of the galena compositions to these average growth curves suggests that these compositions were established by mixing processes as envisaged in the Doe and Zartman \"plumbotectonics\" model. The isotopic analyses of the whole rocks indicate that small amounts of radiogenic lead are present in non-mineralized sections of the sedimentary sequence- Three galenas from veins in rocks metamorphosed to biotite and staurolite-andalusite grades, and from late veins (post-dating deformation, metamorphism and plutonism) are significantly more radiogenic than the majority of the samples. We interpret the isotopic characteristics of these galenas to be the result of extraction of lead from Meguma metasediments or of additions of radiogenic lead to less radiogenic lead during remobllization. Other interpretations consistent with the isotopic data are possible.&#x0D;\n\t\t\t&#x0D;\n\t\t\tR\u00c9SUM\u00c9&#x0D;\n\t\t\tDes analyses aux isotopes de plomb ont \u00e9t\u00e9 d\u00e9termin\u00e9 pour les gal\u00e8nes qui se trouvent en petite quantiti\u00e9's dans les veines de quartz de la formation Goldenville du terrane Meguma, et aussi pour cinq \u00e9chantillons de roches entieres de cette formation. Les dix gal\u00e8nes les moins radiog\u00e8niques sont homog\u00e8nes en composition isotopique, et elles ont une trace proche de la courbe de croissauce terreste moyenne de Stacey et Kramers, et de la courbe \"orog\u00e8ne\" de Doe et Zartman. Le \u00e2ges moyens des modules sont de 550 Ma (Stacey et Kramers) et de 600 Ma (Doe et Zartman), ce qui s'accorde approximativement avec l'\u00e2ge Cambro-Ordovicien du d\u00e9p\u00f4t des s\u00e9diments. La position proche des compositions de la gal\u00e8ne avec ces courbes moyennes de croissance, indique que ces compositions ont \u00e9t\u00e9 \u00e9tablies par un processus de m\u00e9langes, comme le propose le mod\u00e8le \"Piumbotectonique\" de Doe et Zartman. Les analyses isotopiques de roche entiere indiquent que de petites quantiti\u00e9's de plomb radiogenique sont pr\u00e9sences dans les sections non-min\u00e9ralisees de la s\u00e9quence s\u00e9dimentaire. Trois gal\u00e8nes, provenant de veines de roches m\u00e9tamorphos\u00e9e au d\u00e9gris de biotite et de staurolite-anda lusite, et de veines avanc\u00e9es (post-datant la d\u00e9formation, le m\u00e9tamorphisine et le plutonisme) sont d'une maniere significative plus radiog\u00e8niques que la majoriti\u00e9 des \u00e9chantillons. Nous interpr\u00e8tons les caract\u00e9ristiques isotopiques de ces gal\u00e8nes comme le r\u00e9sultat de l'extraction de plomb des m\u00e9ta-s\u00e9diments Meguma, ou a L\u2019addition de plomb radiog\u00e8nique au plomb moins radiog\u00e8nique durant la remobilisation.     D'autres   Interpr\u00e8tations   en  accord  avec   les  donn\u00e9s  isotopiques  sont  possible.&#x0D;\n\t\t\t\t&#x0D;\n[Traduit par le journal]<\/jats:p>","DOI":"10.4138\/1599","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Lead Isotope Data for Gold-Bearing Veins and Their Host Metasedimentary Rocks of the Goldenville Formation, Eastern Nova Scotia"],"prefix":"10.4138","volume":"22","author":[{"given":"R. M.","family":"Farquhar","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"S. J.","family":"Haynes","sequence":"additional","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1986,4,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1599\/1965","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1599\/1965","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T14:45:40Z","timestamp":1638456340000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1599"}},"issued":{"date-parts":[[1986,4,1]]},"references-count":0,"journal-issue":{"issue":"1","published-online":{"date-parts":[[1986,4,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1599","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1986,4,1]]}},{"indexed":{"date-parts":[[2022,4,1]],"date-time":"2022-04-01T03:24:19Z","timestamp":1648783459850},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"1\/2\/3","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"abstract":"<jats:p>The Albert Formation in the Moncton Subbasin of southern New Brunswick was essentially deposited in a complex series of spatially and temporally inter-related alluvial fan, fluvial-deltaic and \"deep\" water lacustrine depositional environments and which have all previously been described in detail. Herein we describe three depositional environments and their lithofacies which have not previously been described in any great detail, but constitute an integral part of the succession. These are the algal swamp, marginal (shoreface and carbonate mudflat) and shallow evaporitic lacustrine environments and their lithofacies.&#x0D;\n\t\t\t&#x0D;\nAlgal swamp lithofacies are characterized by kerogenous mudstones and inorganically precipitated nodular and phylloid or stromatolitic algal carbonates. Marginal lacustrine lithofacies are represented by two distinctive assemblages, namely carbonate mudflat and shoreface lithofacies. The former are characterized by dolomitic shales and interbeds of argillaceous limestones, aphanitic dolostones, siltstones and rare kerogenous and sub-kerogenous mudstones. The latter are characterized by 0.5-lm thick sandstones and interbedded shales or mudstones. Both exhibit evidence of ephemeral exposure. Evaporitic lacustrine lithofacies are characterized by halite, gypsum, glauberite, anhydrite and dolostone with associated shales and siltstones containing molds of evaporite minerals replaced by calcite.&#x0D;\n&#x0D;\nUsing surface and available drill data an assessment of the spatial distribution, both within the Moncton Subbasin itself and with respect to associated depositional environments, of these lithofacies is made.&#x0D;\n\t\t&#x0D;\nR\u00c9SUM\u00c9&#x0D;\n\t\t\tLa Formation d'Albert dans le sous-bassin de Moncton s'est accumul\u00e9e essentiellement dans une s\u00e9rie complexe d'environnements de d\u00e9p\u00f4t, genres c\u00f4ne de d\u00e9jection, fluviodeltaique et milieu lacustre \u00e0 tranche d'eau \"profonde\". Ces derniers ont tous fait l'objet de descriptions ant\u00e9rieures d\u00e9taill\u00e9es et l'on peut les mettre en corr\u00e9lation spatiale et ternporelle. Dans cet article on d\u00e9crit trois milieux de d\u00e9p\u00f4t ainsi que leurs faci\u00e8s lithologiques qui n'ont auparavant fait l'objet d'aucune description en d\u00e9tail mais qui font cependant partie integrante de la succession. Ce sont les environnements de mar\u00e9cage algaire, de milieu lacustre marginal (shoreface et vasi\u00e8re \u00e0 carbonates) et \u00e9vaporitique peu profond. &#x0D;\n&#x0D;\nLes types faciologiques du mar\u00e9cage algaire sont principalement des mudstones \u00e0 k\u00e9rog\u00e8ne, des carbonates algolamin\u00e9s (stromatolithes) et des carbonates noduleux ou en plaquettes pr\u00e9cipit\u00e9s de facon inor-ganique. On retrouve deux assemblages distincts de lithofacies de bord de lac, ce sont, respectivement, la vasiere \u00e0 carbonates et le shoreface. Le premier se caract\u00e9rise par des argilites dolomitiques interludes avec des calcaires argileux, des dolomies cryptocristallines, des siltstones et de rares mudstones plus ou moins riches en k\u00e9rog\u00e8ne. Le second assemblage comprend des bancs de gr\u00e8s de 0.5-1.0m d'\u00e9paisseur interlites avec des argilites ou des mudstones. Tous deux pr\u00e9sentent des marqu\u00e9s \u00e9videntes d'\u00e9xposition subaerienne sporadique. Le lithofaci\u00e8s lacustre \u00e0 \u00e9vaporites contient surtout de la halite, du gypse, de la glaub\u00e9rite, de l'anhydrite et de la dolomite associ\u00e9s \u00e0 des argilites et des siltstones qui renferment des moulages de min\u00e9raux \u00e9vaporitiques remplac\u00e9s par de la calcite.&#x0D;\n\t\t\t&#x0D;\nL'utilisation des donn\u00e9es de la g\u00e9ologie de surface ainsi que des forages disponibles, tant dans le sous-bassin de Moncton m\u00eame qu'en ce qui concerne les milieux de d\u00e9p\u00f4t qui lui sont associ\u00e9s, permet une \u00e9valuation de la distribution de ces lithofaci\u00e8s dans L\u2019espace.&#x0D;\n\t\t\t\t\t\t&#x0D;\n[Traduit par le journal]<\/jats:p>","DOI":"10.4138\/1588","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":1,"title":["Algal swamp, marginal and shallow evaporitic lacustrine lithofacies from the late Devonian - early Carboniferous Albert Formation, southeastern New Brunswick, Canada"],"prefix":"10.4138","volume":"21","author":[{"given":"D. C.","family":"Carter","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"R. K.","family":"Pickerill","sequence":"additional","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1985,1,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1588\/1954","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1588\/1954","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T14:45:57Z","timestamp":1638456357000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1588"}},"issued":{"date-parts":[[1985,1,1]]},"references-count":0,"journal-issue":{"issue":"1\/2\/3","published-online":{"date-parts":[[1985,1,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1588","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1985,1,1]]}},{"indexed":{"date-parts":[[2023,10,29]],"date-time":"2023-10-29T19:22:58Z","timestamp":1698607378761},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"2","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"abstract":"<jats:p>Hamilton Sound is a shallow, wave-exposed embayment on the northeast coast of Newfoundland. Four seismostratigraphic units are recognised: (1) bedrock (acoustic basement); (2) a unit with incoherent reflections, interpreted as Late Wisconsinan glacial diamicton or till, which in places forms small drumlins; (3) a thin, acoustically stratified, draped unit found in the deepest parts of the eastern sound, interpreted as glacimarine gravelly mud; and (4) an uppermost unit with an acoustically stratified, ponded facies, and a fades which can be acoustically incoherent. Unit 4 consists of sandy mud, muddy sand, sand and gravel, and results from reworking of units 2 and 3. Three types of seabed occur (1) bedrock; (2) bouldery gravel or gravel, sub-angular to rounded, which overlies, and is derived from, glacial diamicton of acoustic unit 2. The coralline alga Lilholhamnion sp. coats some clasts on their upper surfaces and some clasts completely. This, together with the occurrence of gravel ripples in several areas, is evidence of intermittent sediment mobility, and (3) gravelly sand, sand, muddy sand, or sandy mud, located in basins. Seabed features in this zone include dunes, iceberg furrows and pits. The regional relative sea-level curve is constrained by two types of morphological evidence: rounded drumlin crests at depths below 19 m which would have been truncated if sea level had fallen below -18.S m, and (wave-cut) terraces at depths of 17 to 21 m. These data are indicative of a -17 m lowstand of relative sea level. Radiocarbon dates from a vibracore suggest that the lowstand occurred prior to 8.6 ka B.P. During the lowstand Fogo Island was connected to the mainland by a narrow isthmus.&#x0D;\n&#x0D;\nR\u00c9SUM\u00c9&#x0D;\n\t\tLe d\u00e9froit d'Hamilton est une bale peu profonde et expos\u00e9e aux vagues sur la c\u00f4te nord de Terre-Neuve. Quatre unit\u00e9s sismostratigraphiques sont distingu\u00e9es : (1) la roche de fond (le socle acoustique); (2) une unit\u00e9 montrant des r\u00e9flections d\u00e9ordonn\u00e9es, interpr\u00e9t\u00e9e comme \u00e9tant un diamicton glaciaire ou un till du Wisconsinien tardif et qui form\u00e9 localement de petits drumlins; (3) une unit\u00e9 mince et \u00e9tendue, montrant une stratification acoustique et qui se retrouve dans les parties les plus profondes du segment est du d\u00e9troit; cette unite est interpr\u00e9t\u00e9e comme \u00e9tant une boue graveleuse glaciomarine; et (4) une unit\u00e9 sommitale comprenant un faci\u00e8s d'\u00e9tendue restreinte, stratift\u00e9 acoustiquement, et un faci\u00e8s qui peut montrer un d\u00e9sordr\u00e9 acoustique. L'unit\u00e9 4 consiste en boue sableuse, sable boueux, sable et gravier et provient du remaniement des unit\u00e9s 2 et 3. Il y a trois types de fond marin : (1) la roche de fond; (2) du gravier a blocs ou du gravier, subanguleux \u00e0 arrondi, qui recouvre et est d\u00e9riv\u00e9 du diamicton glaciaire de l'unit\u00e9 acoustique 2. L'algue corallienne Lithothamnion sp. recouvre certains clastes sur leur partie sup\u00e9rieure ou d'autres completement. Cet \u00e9l\u00e9ment, combind \u00e0 la pr\u00e9sence d'ondulations dans le gravier \u00e0 plusieurs endroits, est une indication d'une mobilit\u00e9 intermittente du s\u00e9diment; (3) du sable graveleux, sable, sable boueux ou boue sableuse, situis dans des bassins. Les caract\u00e9ristiques du fond marin comprennent des dunes, des sillons traces par les icebergs et des fosses. La courbe r\u00e9gionale du niveau relatif de la mer est bas\u00e9e sur deux types de donn\u00e9es morphologiques: des cretes de drumlins arrondies \u00e0 des profondeurs sup\u00e9rieures a 19 m qui auraient \u00e9t\u00e9 tronqu\u00e9es si le niveau de la mer avait baissd sous -18,5 m, et des terrasses (coup\u00e9es par les vagues) \u00e0 des profondeurs de 17 \u00e0 21 m Ces domt\u00e9es indiquent un minimum du niveau relatif de la mer \u00e0 - 17 m. Les datations radiochronologiques du carbone d'un sondage sugg\u00e8rent que ce minimum a eu lieu avant 8,6 ka Av. Pr. \u00c0 ce moment, l'ile de Fogo \u00e9tait reli\u00e9e \u00e0 la terre ferme par un isthme \u00e9troit.&#x0D;\n&#x0D;\n[Traduit par la r\u00e9daction]<\/jats:p>","DOI":"10.4138\/2123","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":5,"title":["Surficial sediments and post-glacial relative sea-level history, Hamilton Sound, Newfoundland"],"prefix":"10.4138","volume":"30","author":[{"given":"J.","family":"Shaw","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"K. A.","family":"Edwardson","sequence":"additional","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1994,7,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/2123\/2487","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/2123\/2487","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T14:24:20Z","timestamp":1638455060000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/2123"}},"issued":{"date-parts":[[1994,7,1]]},"references-count":0,"journal-issue":{"issue":"2","published-online":{"date-parts":[[1994,7,1]]}},"URL":"https:\/\/doi.org\/10.4138\/2123","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1994,7,1]]}},{"indexed":{"date-parts":[[2022,3,30]],"date-time":"2022-03-30T12:19:09Z","timestamp":1648642749199},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"1","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/1462","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Maritime Sediments, 1966"],"prefix":"10.4138","volume":"2","author":[{"given":"Deryck J.C.","family":"Laming","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1966,1,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1462\/1830","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1462\/1830","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:49:43Z","timestamp":1638460183000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1462"}},"issued":{"date-parts":[[1966,1,1]]},"references-count":0,"journal-issue":{"issue":"1","published-online":{"date-parts":[[1966,1,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1462","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1966,1,1]]}},{"indexed":{"date-parts":[[2022,4,3]],"date-time":"2022-04-03T23:52:11Z","timestamp":1649029931343},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"2","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/1702","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Erratum: An Arenig graptolite from Bell Island, eastern Newfoundland - its biostratigraphic and paleogeographic significance"],"prefix":"10.4138","volume":"26","member":"12607","published-online":{"date-parts":[[1990,7,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1702\/2068","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1702\/2068","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:11:05Z","timestamp":1638457865000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1702"}},"issued":{"date-parts":[[1990,7,1]]},"references-count":0,"journal-issue":{"issue":"2","published-online":{"date-parts":[[1990,7,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1702","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1990,7,1]]}},{"indexed":{"date-parts":[[2024,7,24]],"date-time":"2024-07-24T04:41:17Z","timestamp":1721796077688},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"1","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"abstract":"<jats:p>The North River pluton is one of a series of upper Devonian - lower Carboniferous granite and gabbro\/diorite plutons in the Cobequid Highlands. It lies within a regional zone of east-west strike-slip faulting associated with the Cobequid Fault. The pluton consists of a single main granite unit that intruded small marginal bodies of gabbro. The southern part of the pluton is locally foliated and pervasively fractured. Diabase and microgranite sheets and dykes cut the pluton and adjacent country rock. A relative sequence of intrusion can be determined from cross-cutting relationships with foliated or fractured granite. Hybrid rocks demonstrate that some of the mafic magma was intruded synchronously with granitic magma.&#x0D;\n\t\t\t&#x0D;\nThe pluton is geochemically similar to other Devono-Carboniferous plutons in the Cobequid Highlands, although it represents a deeper structural level than most of the other plutons. The granite is a subalkalic A-type granite. The mafic rocks show \"within-plate\" geochemical characteristics; early intrusions resemble olivine-normative continental tholeiites, but later dykes are highly fractionated and show strong enrichment in incompatible elements. Enrichment in Rb and K in the northeastern part of the pluton reflects a late metasomatic event associated with the growth of secondary biotite.&#x0D;\n\t\t\t&#x0D;\nThe Devono-Carboniferous plutons of the Cobequid Highlands differ from other published examples of shear zone plutonism in that magma generation appears to have been related to either local or more probably regional extension rather than the shear zone having tapped a magma that originally resulted from either subduction or continental collision.&#x0D;\n\t\t\t&#x0D;\n\t\t\tR\u00c9SUM\u00c9&#x0D;\n\t\t\tLe pluton de North River est l'un des batis d\u00e9voniens sup\u00e9rieurs \u00e0 carbonif\u00e8res inf\u00e9rieurs constituent une suite de plutons granitiques et gabbrolques\/dioritiques pr\u00e9sente dans les Monts Cobequid. Il git au sein d'une zone r\u00e9gionale de d\u00e9crochement est-ouest associ\u00e9e \u00e0 la faille de Cobequid. Le pluton consiste en une unit\u00e9 principale unique de granite qui fit intrusion dans de petits batis gabbrolques marginaux. La portion m\u00e9ndionale du pluton montre une foliation locale et une fracturation penetrative. Des lames ainsi que des flkms de diabase et de microgranite recoupent le pluton et la roche encaissante adjacente. Les recoupements du granite foli\u00e9 ou fractur\u00e9 permettent de d\u00e9terminer une s\u00e9quence relative d'intrusion. Des roches hybrides d\u00e9montrent qu'une fraction du magma mafique fit intrusion au m\u00eame moment que le magma granitique.&#x0D;\n\t\t\t&#x0D;\nLa g\u00e9ochimie du pluton est semblable \u00e0 celle des autres plutons d\u00e9vono-carbonif\u00e8res pr\u00e9sents dans les Monts Cobequid, et ce bien qu'il repr\u00e9sente un niveau structural plus profond que celui des autres plutons. Le granite est un granite subalcalin de type A. Les roches mafiques montrent des caract\u00e9ristiques g\u00e9ochimiques \"intraplaques\"; les intrusions pr\u00e9coces ressemblent \u00e0 des thol\u00e9iites continentales \u00e0 olivine normative mais les filons plus tardifs ont subi un fractionnement prononc\u00e9 et ils sont fortement enrichis en \u00e9l\u00e9ments incompatibles. Un enrichissement en Rb et en K dans la r\u00e9gion nord-est du pluton reflete un \u00e9v\u00e9nement m\u00e9tasomatique tardif associ\u00e9 \u00e0 la croissance d'une biotite secondaire.&#x0D;\n\t\t\t&#x0D;\nLes plutons d\u00e9vono-carbonif\u00e8res des Monts Cobequid diff\u00e8rent des autres exemples publi\u00e9s de plutonisme associ\u00e9 \u00e0 une zone de cisaillement en ce que la venue du magma semble avoir \u00e9t\u00e9 reli\u00e9e \u00e0 une extension locale ou, de fa\u00e7on plus vraisemblable, r\u00e9gionale plut\u00f4t qu'au captage par la zone de cisaillement d'un magma r\u00e9sultant \u00e0 l'origine soil d'une subduction, so it d'une collision continentale.&#x0D;\n&#x0D;\n[Traduit par le journal]<\/jats:p>","DOI":"10.4138\/1717","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":5,"title":["Granite and associated mafic phases, North River pluton, Cobequid Highlands, Nova Scotia"],"prefix":"10.4138","volume":"27","author":[{"given":"Georgia","family":"Pe-Piper","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1991,3,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1717\/2083","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1717\/2083","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T14:33:26Z","timestamp":1638455606000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1717"}},"issued":{"date-parts":[[1991,3,1]]},"references-count":0,"journal-issue":{"issue":"1","published-online":{"date-parts":[[1991,3,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1717","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1991,3,1]]}},{"indexed":{"date-parts":[[2022,4,1]],"date-time":"2022-04-01T17:09:51Z","timestamp":1648832991762},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"1","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"abstract":"<jats:p>The Hurricane Mountain m\u00e9lange, Maine, marks the suture zone between the suspected Boundary Mountain and Gander terranes. To the west the Hurricane Mountain m\u00e9lange is bounded by the Boil Mountain ophiolite complex, and on the southeast it is overlain by the Dead River flysch. This ophiolite- m\u00e9lange -flysch sequence may mark a terrane suture that trends northeast from the northern New Hampshire border across west-central Maine and into New Brunswick.&#x0D;\n&#x0D;\n\t\t\tThe matrix of the Hurricane Mountain m\u00e9lange includes mafic volcanic, felsic volcanic, metasedimentary and serpentinitc blocks Major and trace element analysis of the igneous blocks in m\u00e9lange shows strong geochemical similarities to mafic volcanic, felsic volcanic and ultramafic units of the Boil Mountain ophiolite complex. Analysis of relict clinopyroxene grains further supports a correlation between the mafic m\u00e9lange blocks and the upper mafic unit of the Boil Mountain ophiolite complex. Overall, the field, petrographic, and geochemical data suggest that the Boil Mountain ophiolite complex is the probable source for the exotic blocks in the Hurricane Mountain m\u00e9lange.&#x0D;\n\t\t&#x0D;\n\t\t\tR\u00c9SUM\u00c9&#x0D;\n\t\t\tLe m\u00e9lange du mont Hurricane, au Maine, marque la zone de suture entre les terranes pr\u00e9sum\u00e9s du mont Boundary et de Gander. \u00c0 l'ouest. Ic m\u00e9lange du mont Hurricane est limit\u00e9 par le cort\u00e8ge ophiolitique du mont Boil, et \u00e0 partir du sud-ouest, il est rccouvert par le flysch de la rivi\u00e8re Dead Ce cort\u00e8ge ophiolite-m\u00e9lange-flysch pourrait marquer un terrane de suture orient\u00e9 vers le nord-csi \u00e0 partir de la fronti\u00e8re septentrionale du New Hampshire et traversant le centre-ouest du Maine jusqu'a 1'interieurdu Nouveau-Brunswick&#x0D;\n&#x0D;\n\t\t\tLes blocs a l'interieur de la matricc du m\u00e9lange du mont Hurricane comprennent des roches volcanomafiques, des roches volcanofelsiques. des blocs m\u00e9tasedimentaires et des serpentinites. Les analyses des elements majeure et des \u00e9l\u00e9ments traces des blocs du m\u00e9lange r\u00e9v\u00e8lent des similarit\u00e9s g\u00e9ochimiques marquees avec les unites volcanomafiques, volcanofelsiques et ultramafiques du cortege ophiolithique du mont Boil. Une analyse de grains de clinopyroxene r\u00e9siduels appuie elle aussi une corr\u00e9lation entre les blocs du m\u00e9lange mafique et l'unit\u00e9 mafique sup\u00e9rieure du cort\u00e9ge ophiolitique du mont Boil. En somme les donn\u00e9es de terrain et les donn\u00e9es p\u00e9trographiques et g\u00e9ochimiques laissent supposer que le cort\u00e8ge ophiolitique du mont Boil constitue la source probable des blocs du m\u00e9lange exotique du mont Hurricane&#x0D;\n\t\t\t&#x0D;\nTraduit par la r\u00e9daction<\/jats:p>","DOI":"10.4138\/1969","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Geochemical comparison of mafic, felsic, and ultramafic rocks in the Hurricane Mountain m\u00e9lange to the Boil Mountain ophiolite complex, west-central Maine"],"prefix":"10.4138","volume":"37","author":[{"given":"Harriet E.","family":"Van Vleck","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Rachel J.","family":"Beane","sequence":"additional","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[2001,3,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1969\/2333","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1969\/2333","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T14:12:15Z","timestamp":1638454335000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1969"}},"issued":{"date-parts":[[2001,3,1]]},"references-count":0,"journal-issue":{"issue":"1","published-online":{"date-parts":[[2001,3,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1969","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[2001,3,1]]}},{"indexed":{"date-parts":[[2022,3,29]],"date-time":"2022-03-29T17:58:21Z","timestamp":1648576701510},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"2","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/1730","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Atlantic Geological Society"],"prefix":"10.4138","volume":"27","member":"12607","published-online":{"date-parts":[[1991,9,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1730\/2096","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1730\/2096","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:10:59Z","timestamp":1638457859000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1730"}},"issued":{"date-parts":[[1991,9,1]]},"references-count":0,"journal-issue":{"issue":"2","published-online":{"date-parts":[[1991,9,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1730","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1991,9,1]]}},{"indexed":{"date-parts":[[2022,4,4]],"date-time":"2022-04-04T23:48:19Z","timestamp":1649116099011},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"2\/3","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/1540","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["A Continuous Seismic Profile from Halifax Harbour,   Nova Scotia"],"prefix":"10.4138","volume":"3","author":[{"given":"A. C.","family":"Grant","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1967,4,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1540\/1906","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1540\/1906","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:43:45Z","timestamp":1638459825000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1540"}},"issued":{"date-parts":[[1967,4,1]]},"references-count":0,"journal-issue":{"issue":"2\/3","published-online":{"date-parts":[[1967,4,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1540","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1967,4,1]]}},{"indexed":{"date-parts":[[2022,4,5]],"date-time":"2022-04-05T20:37:41Z","timestamp":1649191061560},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"3","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/1503","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Current Research"],"prefix":"10.4138","volume":"2","member":"12607","published-online":{"date-parts":[[1966,6,30]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1503\/1871","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1503\/1871","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T17:02:21Z","timestamp":1638464541000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1503"}},"issued":{"date-parts":[[1966,6,30]]},"references-count":0,"journal-issue":{"issue":"3","published-online":{"date-parts":[[1966,6,30]]}},"URL":"https:\/\/doi.org\/10.4138\/1503","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1966,6,30]]}},{"indexed":{"date-parts":[[2022,4,4]],"date-time":"2022-04-04T02:16:11Z","timestamp":1649038571108},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"4","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/1552","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Salt-Water Intrusion Studies in the Maritimes"],"prefix":"10.4138","volume":"3","author":[{"given":"P. A.","family":"Carr","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1967,9,30]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1552\/1918","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1552\/1918","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:43:20Z","timestamp":1638459800000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1552"}},"issued":{"date-parts":[[1967,9,30]]},"references-count":0,"journal-issue":{"issue":"4","published-online":{"date-parts":[[1967,9,30]]}},"URL":"https:\/\/doi.org\/10.4138\/1552","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1967,9,30]]}},{"indexed":{"date-parts":[[2024,7,24]],"date-time":"2024-07-24T05:20:36Z","timestamp":1721798436110},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"abstract":"<jats:p>The ichnogenus Conopsoides, established in the Nineteenth Century, was differentiated from other ichnogenera by the presence of mounds of sediment associated with the tracks, but this characteristic is now considered an invalid ichnotaxobase by some invertebrate ichnologists. Consequently, Conopsoides has been compared to other ichnogenera in the Hitchcock collection in order to determine if other characteristics could be used to differentiate it. As a result, the morphologies exhibited by Conopsoides are seen in two other ichnogenera, Acanthichnus and Bifurculapes. Specifically, the morphologies seen in the type species, Conopsoides larvalis, are observed in Acanthichnus cursorius and Acanthichnus saltatorius, and therefore different specimens of Conopsoides larvalis are considered to belong to these two ichnospecies. Similarly, the morphology observed in Conopsoides curtus is observed in Bifurculapes laqueatus, so the former ichnospecies is considered a junior subjective synonym of the latter.<\/jats:p>","DOI":"10.4138\/atlgeol.2019.014","type":"journal-article","created":{"date-parts":[[2020,3,4]],"date-time":"2020-03-04T14:30:58Z","timestamp":1583332258000},"page":"389-398","source":"Crossref","is-referenced-by-count":2,"title":["Conopsoides Hitchcock 1858: an ichnological chimera of Acanthichnus and Bifurculapes"],"prefix":"10.4138","volume":"55","author":[{"given":"Patrick","family":"Getty","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"John","family":"Burnett","sequence":"additional","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[2019,12,8]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/28994\/1882526157","content-type":"text\/html","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/28994\/1882525785","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/28994\/1882525785","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2020,3,4]],"date-time":"2020-03-04T14:30:58Z","timestamp":1583332258000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/28994"}},"issued":{"date-parts":[[2019,12,8]]},"references-count":0,"URL":"https:\/\/doi.org\/10.4138\/atlgeol.2019.014","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[2019,12,8]]}},{"indexed":{"date-parts":[[2022,3,31]],"date-time":"2022-03-31T17:45:39Z","timestamp":1648748739922},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"2","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/1487","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":1,"title":["Manganese-Iron Concretions in Nova Scotia Lakes"],"prefix":"10.4138","volume":"2","author":[{"given":"Harold L.","family":"Beals","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1966,4,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1487\/1855","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1487\/1855","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:47:49Z","timestamp":1638460069000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1487"}},"issued":{"date-parts":[[1966,4,1]]},"references-count":0,"journal-issue":{"issue":"2","published-online":{"date-parts":[[1966,4,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1487","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1966,4,1]]}},{"indexed":{"date-parts":[[2022,4,1]],"date-time":"2022-04-01T10:48:43Z","timestamp":1648810123072},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"2","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"abstract":"<jats:p>The tests of 18 benthonic and one planktonic species of modern Foraminifera from 8 bottom samples recovered from the eastern Canadian shelf fall    into two, or perhaps three groups with respect to mean mole percent MgCO3,  as follows: Group  1 - 0 to 2.5 % MgCO3 ;  Group 2  - 2 to 5 % MgCO3;  and Group 3 - 5  to 9 % MgCO3 .    The watermass characteristics and depth of each population are:    Upper Water mass,  -1 to 3 or  5 C,  33 o\/oo salinity, 62 m and 73 m: Intermediate Watermass, 0 C,   34 o\/oo salinity, 99m;  and Deep WatennasB,  4 to 5 C, 35 o\/oo salinity, 263 n, 431 m, 475 m, 479 m and 509 m.&#x0D;\n\t\t\t&#x0D;\nIn the samples   examined low magnesium forms (Group 1) occur in all three water-masses and in a late-glacial beach sample.    The intermediate magnesium form Ephidiella arctica (Group 2) and the high magnesium form   (Group 3) Quinqueloculina arctica and 0. seminulum occur in the Upper Watermass.     Populations of the low magnesium species Buccella inusitata, Islandiella helenae and Nonionellina labradorica are each found in both Upper and Deep Watermasses.    The low magnesium value of Quinqueloculina stalkeri may indicate that the form should be placed in another genus.<\/jats:p>","DOI":"10.4138\/1961","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Magnesium in 19 Species of Eastern Canadian Holocene Foraminifera"],"prefix":"10.4138","volume":"14","author":[{"given":"Kenneth","family":"Hooper","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1978,8,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1961\/2325","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1961\/2325","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:11:54Z","timestamp":1638457914000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1961"}},"issued":{"date-parts":[[1978,8,1]]},"references-count":0,"journal-issue":{"issue":"2","published-online":{"date-parts":[[1978,8,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1961","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1978,8,1]]}},{"indexed":{"date-parts":[[2022,4,3]],"date-time":"2022-04-03T07:38:57Z","timestamp":1648971537788},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"2\/3","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/1547","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Hither and Yon"],"prefix":"10.4138","volume":"3","author":[{"given":"Bernard R.","family":"Pelletier","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1967,4,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1547\/1913","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1547\/1913","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:43:30Z","timestamp":1638459810000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1547"}},"issued":{"date-parts":[[1967,4,1]]},"references-count":0,"journal-issue":{"issue":"2\/3","published-online":{"date-parts":[[1967,4,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1547","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1967,4,1]]}},{"indexed":{"date-parts":[[2022,3,30]],"date-time":"2022-03-30T14:00:33Z","timestamp":1648648833874},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"1","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"abstract":"<jats:p>A long history of dextral transcurrent shear on the Cobequid-Chedabucto Fault System is indicated by structures in Meguma Zone phyllite and granite, and late veins, which outcrop close to the present Chedabucto Fault trace. The phyllite deformed first upon collision of Meguma with Avalonia during the Acadian Orogeny, and progressively since that time by ductile deformation mechanisms for almost the total deformational history of the rocks. Its foliation is due to transposition and dynamic recrystallization. Granite vas intruded syntectonically, as shown by contact oetamorphic formation of syntectonic porphyroblasts in the phylllte which are rotated, and progressive development of an inhomogeneous shear zone foliation towards the phyllite-granite contact. This foliation is approximately parallel to that developed in the phyllite. Quartz veins, which overprint all earlier structures, were deformed and accomodated by ductile mechanisms while being rotated in the continued  progressive dextral   shear  regime.&#x0D;\n\t\t\t&#x0D;\n\t\t\tR\u00c9SUM\u00c9&#x0D;\n\t\t\tUne longue histoire de cisaillent transversale dextrale, sur les syst\u00e8mes de failles Cobequid-chedabucto, est indlque par des structures dans les phylites et les granites Meguma et les jeunes veines qui affleurent pr\u00e8s de la trace de la faille Chedabucto actuelle. La phylite c'est d'abord d\u00e9form\u00e9 \u00e0 la suite de la collision entre Meguma et Avalonia pendant l'orog\u00e9n\u00e8se Acadienne, et d\u00e9puis par des m\u00e9canismes progressifs de d\u00e9formation ductile pendant presque toute la dur\u00e9e de l'histoire d\u00e9formationelle des roches. Sa foliation est attribute \u00e0 la transposition et \u00e0 la recristalisation dynamique. Le granite a \u00e9t\u00e9 p\u00e9n\u00e9tr\u00e9 syntectoniquement, comme le demontre la formation de porphyroblastes syntectoniques par moyen de m\u00e9tamorphisme de contact, dans les phylites retourn\u00e9es, et par le d\u00e9veloppement progressif d'une foliation de zone de cisaillement inhomog\u00e8ne vers le contact phylite-granite. Cette foliation est plus ou mollis paral\u00e8lle \u00e0 celle qui est d\u00e9velopp\u00e9e dans la phylite. Des veines de quartz, qui surimpose toutes les structures pr\u00e9cedences, ont \u00e9t\u00e9 d\u00e9form\u00e9es et accomod\u00e9es par des m\u00e9canismes ductile, pendant qu'elles \u00e9taitant retourn\u00e9es par le  r\u00e9gime  progressif de cisaillement d\u00e9xtral&#x0D;\n\t\t&#x0D;\n[Traduit par le journal]<\/jats:p>","DOI":"10.4138\/1597","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["Structural Study of Highly Deformed Meguma Phyllite and Granite Vicinity of White Head Village, S.E. Nova Scotia"],"prefix":"10.4138","volume":"22","author":[{"given":"C. K.","family":"Mawer","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"P. F.","family":"Williams","sequence":"additional","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1986,4,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1597\/1963","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1597\/1963","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T14:45:42Z","timestamp":1638456342000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1597"}},"issued":{"date-parts":[[1986,4,1]]},"references-count":0,"journal-issue":{"issue":"1","published-online":{"date-parts":[[1986,4,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1597","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1986,4,1]]}},{"indexed":{"date-parts":[[2022,3,30]],"date-time":"2022-03-30T17:43:45Z","timestamp":1648662225990},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"1","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/1292","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":0,"title":["A Current Study of Sedimentation, Bay of Fundy"],"prefix":"10.4138","volume":"1","author":[{"given":"Donald J.P.","family":"Swift","sequence":"first","affiliation":[],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"12607","published-online":{"date-parts":[[1965,1,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1292\/1667","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1292\/1667","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:54:34Z","timestamp":1638460474000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1292"}},"issued":{"date-parts":[[1965,1,1]]},"references-count":0,"journal-issue":{"issue":"1","published-online":{"date-parts":[[1965,1,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1292","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1965,1,1]]}}],"items-per-page":20,"query":{"start-index":0,"search-terms":null}}}