{"status":"ok","message-type":"work-list","message-version":"1.0.0","message":{"facets":{},"total-results":1150,"items":[{"indexed":{"date-parts":[[2022,4,3]],"date-time":"2022-04-03T11:48:28Z","timestamp":1648986508684},"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\/1519","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 Bibliography"],"prefix":"10.4138","volume":"2","member":"12607","published-online":{"date-parts":[[1966,9,30]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1519\/1887","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1519\/1887","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T17:02:14Z","timestamp":1638464534000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1519"}},"issued":{"date-parts":[[1966,9,30]]},"references-count":0,"journal-issue":{"issue":"4","published-online":{"date-parts":[[1966,9,30]]}},"URL":"https:\/\/doi.org\/10.4138\/1519","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1966,9,30]]}},{"indexed":{"date-parts":[[2022,3,29]],"date-time":"2022-03-29T21:29:09Z","timestamp":1648589349774},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"2\/3","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"abstract":"<jats:p>Striations and dispersal patterns for till clasts and matrix geochemistry are used to de\ufb01ne \ufb02ow directions of glacial transport across an area of about 800km2 in the Charlo-Atholville area of north-central New Brunswick. A total of 170 clast samples and 328 till matrix samples collected for geochemical analysis across the region, were analyzed for a total of 39 elements. Major lithologic contacts used here to delineate till clast provenance were based on recent bedrock mapping. Eleven known mineral occurrences and a gossan are used to de\ufb01ne point source targets for matrix geochemical dispersal trains and to estimate probable distance and direction of transport from unknown sources. Clast trains are traceable for distances of approximately 10 km, whereas till geochemical dispersal patterns are commonly lost within 5 km of transport. Most dispersal patterns re\ufb02ect more than a single direction of glacial transport.\n          \n\t\t\tThese data indicate that a single till sheet, 1\u20134 m thick, was deposited as the dominant ice-\ufb02ow direction \ufb02uctuated between southeastward, eastward, and northward over the study area. Directions of early \ufb02ow represent changes in ice sheet dominance, \ufb01rst from the northwest and then from the west. Locally, eastward and northward \ufb02ow represent the maximum erosive phases. The last directions of \ufb02ow are likely due to late glacial ice sheet drawdown towards the valley outlet at Baie des Chaleurs.\n\t\t\t\n\t\t\tR\u00c9SUM\u00c9\n\t\t\t\n\t\t\tL'\u00e9quipe utilise les striures et les trac\u00e9s de dispersion des clastes de till ainsi que les caract\u00e9ristiques g\u00e9ochimiques de la gangue pour d\u00e9\ufb01nir les orientations d'\u00e9coulement du transport glaciaire dans un secteur d'environ 800 kilom\u00e8tres carr\u00e9s de la r\u00e9gion de Charlo-Atholville, dans le centre-nord du Nouveau-Brunswick. On a pr\u00e9lev\u00e9 dans la r\u00e9gion au total 170 \u00e9chantillons de clastes et 328 \u00e9chantillons de gangue du till en vue d'analyses g\u00e9ochimiques, et on a analys\u00e9 leur teneur en 39 \u00e9l\u00e9ments particuliers. Les principales zones de contact lithologique utilis\u00e9es dans le cadre de cet exercice pour d\u00e9limiter la provenance des clastes de till ont \u00e9t\u00e9 bas\u00e9es sur de r\u00e9cents travaux de cartographie du substrat rocheux. Onze venues min\u00e9rales reconnues et un chapeau ferrugineux servent \u00e0 d\u00e9\ufb01nir les objectifs des sources ponctuelles des trac\u00e9s de dispersion g\u00e9ochimique de la gangue de m\u00eame qu'\u00e0 estimer l'orientation et la distance probables du transport \u00e0 partir des sources inconnues. Il est possible de retracer les tra\u00een\u00e9es de clastes sur des distances d'une dizaine de kilom\u00e8tres, tandis que les trac\u00e9s de dispersion g\u00e9ochimique du till s'effacent g\u00e9n\u00e9ralement avant moins de cinq kilom\u00e8tres. La majorit\u00e9 des trac\u00e9s de dispersion \u00e9voquent plus d'une direction de transport glaciaire.\n\t\t\t\n\t\t\tCes donn\u00e9es r\u00e9v\u00e8lent qu'une nappe de till particuli\u00e8re d'une \u00e9paisseur d'un \u00e0 quatre m\u00e8tres s'est d\u00e9pos\u00e9e pendant que l'orientation pr\u00e9dominante des \u00e9coulements de glaces a vari\u00e9 entre le sud-est, l'est et le nord \u00e0 l'int\u00e9rieur du secteur d'\u00e9tude. Les orientations de l'\u00e9coulement primitif repr\u00e9sentent les changements survenus dans la nappe glaciaire pr\u00e9dominante, l'\u00e9coulement provenant d'abord du nord-ouest, puis de l'ouest. L'\u00e9coulement vers l'est et vers le nord repr\u00e9sente par endroits des phases d'\u00e9rosion maximale. Les derni\u00e8res orientations de l'\u00e9coulement sont probablement li\u00e9es \u00e0 un appauvrissement de la nappe tardiglaciaire en direction de la d\u00e9charge de la vall\u00e9e dans la baie des Chaleurs.\n\t\t\t\n\t\t\t[Traduit par la r\u00e9daction.]\n\t\t<\/jats:p>","DOI":"10.4138\/1042","type":"journal-article","created":{"date-parts":[[2014,9,24]],"date-time":"2014-09-24T19:44:32Z","timestamp":1411587872000},"source":"Crossref","is-referenced-by-count":2,"title":["Comparison of clast and matrix dispersal in till: Charlo-Atholville area, north-central New Brunswick"],"prefix":"10.4138","volume":"40","author":[{"given":"M. L.","family":"Dickson","sequence":"first","affiliation":[]},{"given":"B. E.","family":"Broster","sequence":"additional","affiliation":[]},{"given":"M. A.","family":"Parkhill","sequence":"additional","affiliation":[]}],"member":"12607","published-online":{"date-parts":[[2004,10,10]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1042\/1398","content-type":"text\/html","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1042\/1399","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1042\/1399","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T14:05:50Z","timestamp":1638453950000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1042"}},"issued":{"date-parts":[[2004,10,10]]},"references-count":0,"journal-issue":{"issue":"2\/3","published-online":{"date-parts":[[2004,10,10]]}},"URL":"https:\/\/doi.org\/10.4138\/1042","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[2004,10,10]]}},{"indexed":{"date-parts":[[2022,4,5]],"date-time":"2022-04-05T06:50:50Z","timestamp":1649141450668},"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\/1435","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":["Stratigraphy, Sediment Dispersal and Facies Analysis of the Pennsylvanian Pictou Group in New Brunswick"],"prefix":"10.4138","volume":"9","author":[{"given":"H. W.","family":"Van De Poll","sequence":"first","affiliation":[]}],"member":"12607","published-online":{"date-parts":[[1973,12,12]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1435\/1803","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1435\/1803","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:25:59Z","timestamp":1638458759000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1435"}},"issued":{"date-parts":[[1973,12,12]]},"references-count":0,"journal-issue":{"issue":"3","published-online":{"date-parts":[[1973,12,12]]}},"URL":"https:\/\/doi.org\/10.4138\/1435","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1973,12,12]]}},{"indexed":{"date-parts":[[2022,4,6]],"date-time":"2022-04-06T00:09:52Z","timestamp":1649203792583},"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\/1802","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":["Chemical,   Mineralogical and Textural Variations in Sediments from the Scotian Shelf"],"prefix":"10.4138","volume":"5","author":[{"given":"C. V.G.","family":"Phipps","sequence":"first","affiliation":[]},{"given":"L. H.","family":"King","sequence":"additional","affiliation":[]}],"member":"12607","published-online":{"date-parts":[[1969,12,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1802\/2166","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1802\/2166","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:37:09Z","timestamp":1638459429000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1802"}},"issued":{"date-parts":[[1969,12,1]]},"references-count":0,"journal-issue":{"issue":"3","published-online":{"date-parts":[[1969,12,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1802","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1969,12,1]]}},{"indexed":{"date-parts":[[2022,4,6]],"date-time":"2022-04-06T03:34:49Z","timestamp":1649216089015},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/18414","type":"journal-article","created":{"date-parts":[[2013,11,1]],"date-time":"2013-11-01T16:36:08Z","timestamp":1383323768000},"page":"9-53","source":"Crossref","is-referenced-by-count":0,"title":["Atlantic Geoscience Society Abstracts 37th Annual Colloquium &amp; Annual General Meeting 2011"],"prefix":"10.4138","volume":"47","member":"12607","published-online":{"date-parts":[[2011,4,15]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/18414\/19890","content-type":"text\/html","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/18414\/19891","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/18414\/19891","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T16:55:00Z","timestamp":1638464100000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/18414"}},"issued":{"date-parts":[[2011,4,15]]},"references-count":0,"URL":"https:\/\/doi.org\/10.4138\/18414","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[2011,4,15]]}},{"indexed":{"date-parts":[[2022,4,4]],"date-time":"2022-04-04T00:48:37Z","timestamp":1649033317919},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"abstract":"<jats:p>Robert Albert Stuart, the High Sheriff of Charlotte County, deserves credit for establishing the black granite monument industry in New Brunswick. In the late 19th to early 20th centuries, he opened three quarries in mafic plutonic rocks in the vicinity of the Chickahominy Mountain, north of St. Andrews: the Bocabec black granite quarry (1893), the Steen Lake black granite quarry (1895), and the Glenelg porphyry quarry (1906). Much of the information in brief articles in local newspapers lacks sufficient detail to gain a full understanding of the historical development of these quarries. To obtain a clearer timeline for production of stone from the quarries, the rock type in each was examined and compared to black granite monuments in nearby cemeteries known to be sourced from these specific quarries. Previous investigations did not entirely rule out the possibility that the Stuart quarries may have been a source for the headstones placed in the Fairview Lawn Cemetery in Halifax, Nova Scotia, to mark the graves of some of those who were lost when the Titanic sank in 1912. Our detailed analysis of rock textures and production histories leads us to conclude that none of the Stuart quarries could have been a source for the Titanic headstones and supports the previous assessment that they came from Charles Hanson quarry.<\/jats:p>","DOI":"10.4138\/atlgeol.2020.008","type":"journal-article","created":{"date-parts":[[2021,4,20]],"date-time":"2021-04-20T14:13:25Z","timestamp":1618928005000},"page":"189-206","source":"Crossref","is-referenced-by-count":0,"title":["Investigation of Sheriff Stuart\u2019s black granite quarries in Charlotte County, southwestern New Brunswick: implications for the source of the titanic headstones in Halifax, Nova Scotia"],"prefix":"10.4138","volume":"56","author":[{"given":"Leslie R.","family":"Fyffe","sequence":"first","affiliation":[]},{"given":"William W.","family":"Gardiner","sequence":"additional","affiliation":[]}],"member":"12607","published-online":{"date-parts":[[2020,9,13]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/31205\/1882526535","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/31205\/1882526535","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,4,20]],"date-time":"2021-04-20T14:13:25Z","timestamp":1618928005000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/31205"}},"issued":{"date-parts":[[2020,9,13]]},"references-count":0,"URL":"https:\/\/doi.org\/10.4138\/atlgeol.2020.008","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[2020,9,13]]}},{"indexed":{"date-parts":[[2022,4,4]],"date-time":"2022-04-04T01:00:41Z","timestamp":1649034041759},"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 South Mountain Batholith (SMB) is a large, ca. 370 Ma, composite intrusion which was emplaced after deformation associated with the Middle Devonian Acadian Orogeny. Structures in the SMB include primary flow features, .NE-trending faults (\u2248045\u00b0) and fractures (at 040\u00b0 and 062\u00b0) and NW-trending faults and joints (at 315\u00b0, 325\u00b0 and 335\u00b0). Joint trends are regional in nature, showing no relationship to intrusive features. Granite-related dykes, veins, alteration and mineralization in the faults and joints indicate a primary-regional status for these structures. NE-trending fractures are interpreted as P and R shears (Riedel geometry) associated with dextral displacement on the NE-trending faults, whereas NW-trending joints are interpreted as tension joints and attending conjugate-shear joints of small dihedral angle reflecting NW-transpression during intrusion. Repetitive joint and fault development continued into the Permian, implying a fixed regional stress through this interval.&#x0D;\n\t\t\t&#x0D;\nThe joint and fault systems in the SMB strongly influenced the localization and character of granite-related mineralization. Sn-W-Cu-Mo quartz-greisen veins occur in NW-trending joints, whereas U-Mn mineralization occurs in NE-trending faults and associated fractures.&#x0D;\n\t\t\t&#x0D;\nLocalization of the batholith is inferred to have been strongly influenced by regional, NE-trending faults which were active during granite intrusion and responsible for localization of some of the later piutons. Final emplacement was largely accomplished by stoping, which was strongly influenced by NE- and NW-trending structures developed in the country rocks and early units of the batholith.&#x0D;\n\t\t&#x0D;\n\t\t\tR\u00c9SUM\u00c9&#x0D;\n\t\t\tLe batholite du mont South est une intrusion composite volumineuse, dat\u00e9e \u00e0 environ 370 Ma, qui s'est mise en place apr\u00e8s la d\u00e9formation associ\u00e9e \u00e8 l'orog\u00e9n\u00e8se acadienne du D\u00e9vonien moyen. Les \u00e9l\u00e9ements structuraux observ\u00e9s dans le batholite comprennent des structures d'\u00e9coulement primaires, des failles (\u00e0 environ 045\u00b0) et des fractures (\u00e0 040\u00b0 et 062\u00b0) de direction nord-est et des failles et des joints de direction nord-ouest (\u00e0 315\u00b0, 325\u00b0 et 335\u00b0). Les directions des joints correspondent aux orientations r\u00e9gionales et ne montrent pas de relation avec les structures intrusives. Les dykes, les veines, l\u2019alt\u00e9ration, la min\u00e9ralisation reli\u00e9s au granite dans les failles et les joints indiquent qu'il s'agit de structures primaires a distribution r\u00e9gionale. Les fractures nord-est sont interpr\u00e9ters comme \u00e9tant des cisaillements P et R (g\u00e9om\u00e9trie de Riedel) reli\u00e9s \u00e0 un d\u00e9facement dextre des failles nord-est, tandis que les joints nord-ouest sont interpr\u00e9ts comme \u00e9tant des joints d\u2019extension auxquels sont associ\u00e9s des joints de cisaillement conjugu\u00e9s de petit angle di\u00e8dre qui refletent une transpression nord-ouest pendant l\u2019intrusion. Le d\u00e9velopp\u00e9ment r\u00e9pet\u00e9 de joints \u00e9tde failles a continu\u00e9 jusqu'auPermien, indicant une contrainte r\u00e9gionale fixe pendant cet intervalle.&#x0D;\n&#x0D;\n\t\t\tLes syst\u00e8mes de failles et de joints dans le batholite du mont South ont fortement influenc\u00e9 la position et le caract\u00e9re de la min\u00e9ralisation rli\u00e9e au granite. Les veines de greisen quartzif\u00e8re  \u00e0 Sn-W-Cu-Mo occupent des joints nord-ouest tandis que la min\u00e9ralisation en U-Mn se retrouv\u00e9 dans des failles nord-est et des fractures associ\u00e9es.&#x0D;\n\t\t\t&#x0D;\nLa position du batholite est interpr\u00e9ted comme ayant \u00e9t\u00e9 fortement influenced par les failles r\u00e9gionales nord-est qui \u00e9taient actives lors de l\u2019intrusion des granites et qui sont responsables de la localisation de certains plutons tardifs. La mise en place finale s'est effectu\u00e9e en grande partie par effondrement du toil, qui a \u00e9t\u00e9 fortement influenc\u00e9 par les structures nord-est et nord-ouest d\u00e9velopp\u00e9es dans les roches encaissantcs et les unit\u00e9s pr\u00e9coces du batholite.&#x0D;\n&#x0D;\n[Traduit par le journal]<\/jats:p>","DOI":"10.4138\/1849","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":["Structure and emplacement of the South Mountain Batholith, southwestern Nova Scotia"],"prefix":"10.4138","volume":"28","author":[{"given":"R. J.","family":"Home","sequence":"first","affiliation":[]},{"given":"M. A.","family":"MacDonald","sequence":"additional","affiliation":[]},{"given":"M. C.","family":"Corey","sequence":"additional","affiliation":[]},{"given":"L. J.","family":"Ham","sequence":"additional","affiliation":[]}],"member":"12607","published-online":{"date-parts":[[1992,3,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1849\/2213","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1849\/2213","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T14:31:44Z","timestamp":1638455504000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1849"}},"issued":{"date-parts":[[1992,3,1]]},"references-count":0,"journal-issue":{"issue":"1","published-online":{"date-parts":[[1992,3,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1849","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1992,3,1]]}},{"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":[[2022,3,29]],"date-time":"2022-03-29T07:22:42Z","timestamp":1648538562134},"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\/1902","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":"6","member":"12607","published-online":{"date-parts":[[1970,12,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1902\/2266","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1902\/2266","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T17:01:39Z","timestamp":1638464499000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1902"}},"issued":{"date-parts":[[1970,12,1]]},"references-count":0,"journal-issue":{"issue":"3","published-online":{"date-parts":[[1970,12,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1902","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1970,12,1]]}},{"indexed":{"date-parts":[[2022,4,6]],"date-time":"2022-04-06T02:43:15Z","timestamp":1649212995701},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","issue":"3","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"abstract":"<jats:p>Bottom sediment samples   (depths to 25m) from St.   Mary's River,   Gegogan,   Wine Bay, Indian and Holland's Harbours, Nova Scotia,   identified for the Foraminifera by Habbishaw in 1970,   were factor-vector analyzed.     Based on   'total' populations 4 benthonic foraminiferal assemblages,   not strictly biocenoses,   are recognized. Assemblage 1,   dominated by Miliammina  fusca,   has a mean diversity of 4.75,   a mean depth of 1.85 m,   a mean pH  (substrate)  of 6.7,   and the  substrate is coarse-grained.     This assemblage is found in  the  Upper Estuarine   (intertidal)   Zone in St.  Mary's River,   south of Sherbrooke.     Assemblage  2,  dominated by Eggerella advena,   has a mean diversity of 12.5,  a mean depth of 7 m,   a mean pH  (substrate) of 8.16,  and the substrate is very fine-grained.     It is found in  the Lower Estuarine  Zone in  the  lower reaches of St.  Mary's River,   Wine Harbour Bay,   the western and northern areas of Gegogan Harbour,  and the eastern shore south of Port Bickerton.     Assemblage 3, dominated by Elphidium clavatum, has a mean diversity of 14.3,   a mean depth of 9m,  a mean pH  (substrate)  of 7.2,  and the substrate is coarse-  to fine-grained sand.    It occurs in the Marginal Marine Zone   (Scott) or Nearshore Biofacies  (Bartlett)  in St.  Mary's River (3 to 5 km from the mouth) and at the head and near the mouth of Indian Harbour.    Assemblage 4 dominated by Cibicides lobatulus,  Eggerella advena and Elphidium clavatum, has a mean diversity of 19.9,  a mean depth of 12.2m,  a mean pH  (substrate)  of 7.16,  and the substrate is medium- to fine-grained sand.    It occurs in the Open Ocean-Nearshore Zone   (Scott)  or the Open Bay Biofacies   (Bartlett),   inside and outside Holland's Harbour,   the southwest and central area of Indian Harbour,  at the mouth of St. Mary's River,  on  the eastern side of Gegogan Harbour,  and east of Crook Point.<\/jats:p>","DOI":"10.4138\/1964","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":["Distribution of Foraminiferida South of Sherbrooke, Nova Scotia"],"prefix":"10.4138","volume":"14","author":[{"given":"Kenneth","family":"Hooper","sequence":"first","affiliation":[]}],"member":"12607","published-online":{"date-parts":[[1978,12,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1964\/2328","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1964\/2328","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:11:49Z","timestamp":1638457909000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1964"}},"issued":{"date-parts":[[1978,12,1]]},"references-count":0,"journal-issue":{"issue":"3","published-online":{"date-parts":[[1978,12,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1964","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1978,12,1]]}},{"indexed":{"date-parts":[[2022,3,30]],"date-time":"2022-03-30T21:53:33Z","timestamp":1648677213423},"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\/1459","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":["Clay Mineral Composition of Bottom Sediments: Western Great South Bay and South Oyster Bay, Long Island; New York"],"prefix":"10.4138","volume":"10","author":[{"given":"Neal R.","family":"O'Brien","sequence":"first","affiliation":[]},{"given":"Syed A.","family":"Ali","sequence":"additional","affiliation":[]}],"member":"12607","published-online":{"date-parts":[[1974,12,12]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1459\/1827","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1459\/1827","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:23:47Z","timestamp":1638458627000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1459"}},"issued":{"date-parts":[[1974,12,12]]},"references-count":0,"journal-issue":{"issue":"3","published-online":{"date-parts":[[1974,12,12]]}},"URL":"https:\/\/doi.org\/10.4138\/1459","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1974,12,12]]}},{"indexed":{"date-parts":[[2022,3,29]],"date-time":"2022-03-29T19:10:29Z","timestamp":1648581029854},"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\/1787","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":["Preliminary Comments on Linear Sand-Surface Features,   Onslow Bay,   North Carolina Continental Shelf:    Problems in Making Detailed Sea-Floor Observations"],"prefix":"10.4138","volume":"5","author":[{"given":"Ian G.","family":"MacIntyre","sequence":"first","affiliation":[]},{"given":"Orrin H.","family":"Pilkey","sequence":"additional","affiliation":[]}],"member":"12607","published-online":{"date-parts":[[1969,1,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1787\/2151","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1787\/2151","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:37:36Z","timestamp":1638459456000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1787"}},"issued":{"date-parts":[[1969,1,1]]},"references-count":0,"journal-issue":{"issue":"1","published-online":{"date-parts":[[1969,1,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1787","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1969,1,1]]}},{"indexed":{"date-parts":[[2022,4,1]],"date-time":"2022-04-01T12:51:58Z","timestamp":1648817518390},"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\/1855","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":["1992 Symposium"],"prefix":"10.4138","volume":"28","author":[{"name":"Atlantic Geoscience Society","sequence":"first","affiliation":[]}],"member":"12607","published-online":{"date-parts":[[1992,3,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1855\/2219","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1855\/2219","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:10:54Z","timestamp":1638457854000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1855"}},"issued":{"date-parts":[[1992,3,1]]},"references-count":0,"journal-issue":{"issue":"1","published-online":{"date-parts":[[1992,3,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1855","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1992,3,1]]}},{"indexed":{"date-parts":[[2022,4,2]],"date-time":"2022-04-02T15:53:11Z","timestamp":1648914791287},"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\/1511","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":["Snow Cover Depletion in the North Nashwaaksis Stream Basin, N.B."],"prefix":"10.4138","volume":"2","author":[{"given":"Dale I.","family":"Bray","sequence":"first","affiliation":[]}],"member":"12607","published-online":{"date-parts":[[1966,9,30]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1511\/1879","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1511\/1879","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:45:26Z","timestamp":1638459926000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1511"}},"issued":{"date-parts":[[1966,9,30]]},"references-count":0,"journal-issue":{"issue":"4","published-online":{"date-parts":[[1966,9,30]]}},"URL":"https:\/\/doi.org\/10.4138\/1511","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1966,9,30]]}},{"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":[]},{"given":"Rachel J.","family":"Beane","sequence":"additional","affiliation":[]}],"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":[[2022,4,3]],"date-time":"2022-04-03T07:13:49Z","timestamp":1648970029016},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"DOI":"10.4138\/20421","type":"journal-article","created":{"date-parts":[[2013,11,1]],"date-time":"2013-11-01T16:36:08Z","timestamp":1383323768000},"page":"104-117","source":"Crossref","is-referenced-by-count":0,"title":["Geological Association of Canada Abstracts, Newfoundland Section \u2013 2013 Spring Technical Meeting"],"prefix":"10.4138","volume":"49","member":"12607","published-online":{"date-parts":[[2013,7,16]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/20421\/24304","content-type":"text\/html","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/20421\/23545","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/20421\/23545","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:09:29Z","timestamp":1638457769000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/20421"}},"issued":{"date-parts":[[2013,7,16]]},"references-count":0,"URL":"https:\/\/doi.org\/10.4138\/20421","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[2013,7,16]]}},{"indexed":{"date-parts":[[2022,4,3]],"date-time":"2022-04-03T02:24:31Z","timestamp":1648952671574},"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\/1775","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":"4","member":"12607","published-online":{"date-parts":[[1968,12,1]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1775\/2139","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1775\/2139","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T17:01:56Z","timestamp":1638464516000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1775"}},"issued":{"date-parts":[[1968,12,1]]},"references-count":0,"journal-issue":{"issue":"3","published-online":{"date-parts":[[1968,12,1]]}},"URL":"https:\/\/doi.org\/10.4138\/1775","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1968,12,1]]}},{"indexed":{"date-parts":[[2022,3,29]],"date-time":"2022-03-29T13:21:13Z","timestamp":1648560073441},"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\/1470","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":["Ship and Airborne Magnetometer Results from the Scotia Shelf, Grand Banks and Flemish Cap"],"prefix":"10.4138","volume":"2","author":[{"given":"Peter","family":"Hood","sequence":"first","affiliation":[]}],"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\/1470\/1838","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1470\/1838","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:48:15Z","timestamp":1638460095000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1470"}},"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\/1470","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":"2022-04-03T05:15:21Z","timestamp":1648962921105},"reference-count":0,"publisher":"University of New Brunswick Libraries - UNB","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["atgeol"],"abstract":"<jats:p>The type and only specimen of the ichnospecies Megapezia longipes, from the Pennsylvanian Rhode Island Forma-tion of Plainville, Massachusetts, consists of two poorly defined tracks, one made by a manus and the other by a pes, rather than a single pedal imprint. Whereas the type species of Megapezia, Megapezia pineoi, has tetradactyl pedal imprints, the pes imprint of Megapezia longipes is pentadactyl, a feature that precludes assignment to this ichnogenus. Rather, the tracks share two characteristics with the ichnogenus Matthewichnus, namely elongate digits II and III on the manus, and a pes imprint oriented anterolaterally to the manus imprint, and are thus tentatively reassigned to that ichnogenus. Cf. Matthewichnus longipes is retained as a separate ichnospecies pending the collection of additional ma-terial that can be compared with other species within the ichnogenus. With the tentative reassignment of the Plainville tracks to Matthewichnus, Megapezia becomes monospecific and is no longer recorded in New England. The tracks are the first known occurrence of Matthewichnus from this region.<\/jats:p>","DOI":"10.4138\/atlgeol.2016.006","type":"journal-article","created":{"date-parts":[[2016,5,10]],"date-time":"2016-05-10T08:51:11Z","timestamp":1462870271000},"page":"119","source":"Crossref","is-referenced-by-count":0,"title":["Megapezia longipes Willard and Cleaves 1930 from the Pennsylvanian Rhode Island Formation of Massachusetts: ichnotaxonomic status"],"prefix":"10.4138","volume":"52","author":[{"given":"Patrick R.","family":"Getty","sequence":"first","affiliation":[]}],"member":"12607","published-online":{"date-parts":[[2016,4,10]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/viewFile\/24338\/28425","content-type":"text\/html","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/viewFile\/24338\/28372","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/viewFile\/24338\/28425","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/viewFile\/24338\/28372","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2016,5,10]],"date-time":"2016-05-10T08:51:11Z","timestamp":1462870271000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/24338"}},"issued":{"date-parts":[[2016,4,10]]},"references-count":0,"URL":"https:\/\/doi.org\/10.4138\/atlgeol.2016.006","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[2016,4,10]]}},{"indexed":{"date-parts":[[2022,4,5]],"date-time":"2022-04-05T19:26:46Z","timestamp":1649186806398},"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\/1508","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":"2","author":[{"given":"Deryck J.C.","family":"Laming","sequence":"first","affiliation":[]}],"member":"12607","published-online":{"date-parts":[[1966,9,30]]},"container-title":["Atlantic Geology"],"link":[{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1508\/1876","content-type":"application\/pdf","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/download\/1508\/1876","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2021,12,2]],"date-time":"2021-12-02T15:46:11Z","timestamp":1638459971000},"score":0.0,"resource":{"primary":{"URL":"https:\/\/journals.lib.unb.ca\/index.php\/ag\/article\/view\/1508"}},"issued":{"date-parts":[[1966,9,30]]},"references-count":0,"journal-issue":{"issue":"4","published-online":{"date-parts":[[1966,9,30]]}},"URL":"https:\/\/doi.org\/10.4138\/1508","ISSN":["1718-7885","0843-5561"],"issn-type":[{"value":"1718-7885","type":"electronic"},{"value":"0843-5561","type":"print"}],"published":{"date-parts":[[1966,9,30]]}}],"items-per-page":20,"query":{"start-index":0,"search-terms":null}}}