{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,10,20]],"date-time":"2026-10-20T17:51:13Z","timestamp":1792518673076,"version":"4.5.0"},"reference-count":40,"publisher":"American Geophysical Union (AGU)","issue":"7","license":[{"start":{"date-parts":[[2007,7,24]],"date-time":"2007-07-24T00:00:00Z","timestamp":1185235200000},"content-version":"vor","delay-in-days":23,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Geochem Geophys Geosyst"],"published-print":{"date-parts":[[2007,7]]},"abstract":"<jats:p>The 2,500\u2010km Kermadec\u2010Tonga arc is the longest submarine arc on the planet. Here, we report on the second of a series of cruises designed to investigate large\u2010scale controls on active hydrothermal venting on this arc. The 2002 NZAPLUME II cruise surveyed 12 submarine volcanic centers along \u223c580 km of the middle Kermadec arc (MKA), extending a 1999 cruise that surveyed 260 km of the southern Kermadec arc (SKA). Average spacing between volcanic centers increases northward from 30 km on backarc crust along the SKA, to 45 km on backarc crust along the southern MKA, to 58 km where the MKA joins the Kermadec Ridge. Volcanic cones dominate in the backarc, and calderas dominate the Kermadec Ridge. The incidence of venting is higher along the MKA (83%, 10 of 12 volcanic centers) than the SKA (67%, 8 of 12), but the relative intensity of venting, as given by plume thickness, areal extent, and concentration of dissolved gases and ionic species, is generally weaker in the MKA. This pattern may reflect subduction of the \u223c17\u2010km\u2010thick oceanic Hikurangi Plateau beneath the SKA. Subduction of this basaltic mass should greatly increase fluid loss from the downgoing slab, initiating extensive melting in the upper mantle wedge and invigorating the hydrothermal systems of the SKA. Conversely, volcanic centers in the southern MKA are starved of magma replenishment and so their hydrothermal systems are waning. Farther north, where the MKA centers merge with the Kermadec Ridge, fewer but larger magma bodies accumulate in the thicker (older) crust, ensuring more widely separated, caldera\u2010dominated volcanic centers.<\/jats:p>","DOI":"10.1029\/2006gc001495","type":"journal-article","created":{"date-parts":[[2007,7,23]],"date-time":"2007-07-23T19:59:10Z","timestamp":1185220750000},"source":"Crossref","is-referenced-by-count":93,"title":["Submarine hydrothermal activity along the mid\u2010Kermadec Arc, New Zealand: Large\u2010scale effects on venting"],"prefix":"10.1029","volume":"8","author":[{"given":"C. E. J.","family":"de Ronde","sequence":"first","affiliation":[{"name":"GNS Science  P.O. Box 30\u2010368, Lower Hutt New Zealand"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"E. T.","family":"Baker","sequence":"additional","affiliation":[{"name":"Pacific Marine Environmental Laboratory National Oceanic and Atmospheric Administration  7600 Sand Point Way NE, Building 3, Seattle Washington 98115\u20106349 USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"G. J.","family":"Massoth","sequence":"additional","affiliation":[{"name":"GNS Science  P.O. Box 30\u2010368, Lower Hutt New Zealand"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"J. E.","family":"Lupton","sequence":"additional","affiliation":[{"name":"Pacific Marine Environmental Laboratory National Oceanic and Atmospheric Administration  2115 S.E. OSU Drive, Newport Oregon 97365\u20105258 USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"I. C.","family":"Wright","sequence":"additional","affiliation":[{"name":"National Institute of Water and Atmospheric Research  P.O. Box 14\u2010901, Wellington New Zealand"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"R. J.","family":"Sparks","sequence":"additional","affiliation":[{"name":"GNS Science  P.O. Box 30\u2010368, Lower Hutt New Zealand"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"S. C.","family":"Bannister","sequence":"additional","affiliation":[{"name":"GNS Science  P.O. Box 30\u2010368, Lower Hutt New Zealand"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"M. E.","family":"Reyners","sequence":"additional","affiliation":[{"name":"GNS Science  P.O. Box 30\u2010368, Lower Hutt New Zealand"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"S. L.","family":"Walker","sequence":"additional","affiliation":[{"name":"Pacific Marine Environmental Laboratory National Oceanic and Atmospheric Administration  7600 Sand Point Way NE, Building 3, Seattle Washington 98115\u20106349 USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"R. R.","family":"Greene","sequence":"additional","affiliation":[{"name":"Pacific Marine Environmental Laboratory National Oceanic and Atmospheric Administration  2115 S.E. OSU Drive, Newport Oregon 97365\u20105258 USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"J.","family":"Ishibashi","sequence":"additional","affiliation":[{"name":"Faculty of Science Kyushu University  8128581 Fukuoka Japan"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"K.","family":"Faure","sequence":"additional","affiliation":[{"name":"GNS Science  P.O. Box 30\u2010368, Lower Hutt New Zealand"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"J. A.","family":"Resing","sequence":"additional","affiliation":[{"name":"Pacific Marine Environmental Laboratory National Oceanic and Atmospheric Administration  7600 Sand Point Way NE, Building 3, Seattle Washington 98115\u20106349 USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"G. T.","family":"Lebon","sequence":"additional","affiliation":[{"name":"Pacific Marine Environmental Laboratory National Oceanic and Atmospheric Administration  7600 Sand Point Way NE, Building 3, Seattle Washington 98115\u20106349 USA"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"13","published-online":{"date-parts":[[2007,7,24]]},"reference":[{"key":"e_1_2_6_2_1","series-title":"Geol. Soc. London Spec. Publ.","first-page":"141","volume-title":"Intra\u2010oceanic Subduction Systems: Tectonic and Magmatic Processes","author":"Baker E. T.","year":"2003"},{"key":"e_1_2_6_3_1","doi-asserted-by":"publisher","DOI":"10.1029\/97JB02474"},{"key":"e_1_2_6_4_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0040-1951(00)00211-0"},{"key":"e_1_2_6_5_1","doi-asserted-by":"publisher","DOI":"10.1016\/0025-3227(94)90117-1"},{"key":"e_1_2_6_6_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0012-821X(01)00534-9"},{"key":"e_1_2_6_7_1","first-page":"91","volume-title":"Giggenbach Memorial Volume","author":"de Ronde C. E. J.","year":"2003"},{"key":"e_1_2_6_8_1","doi-asserted-by":"publisher","DOI":"10.2113\/gsecongeo.100.6.1097"},{"key":"e_1_2_6_9_1","doi-asserted-by":"publisher","DOI":"10.1038\/nature04762"},{"key":"e_1_2_6_10_1","doi-asserted-by":"publisher","DOI":"10.1080\/00288306.2006.9515184"},{"key":"e_1_2_6_11_1","doi-asserted-by":"publisher","DOI":"10.1029\/GM063p0251"},{"key":"e_1_2_6_12_1","doi-asserted-by":"publisher","DOI":"10.1029\/1999GL002325"},{"key":"e_1_2_6_13_1","doi-asserted-by":"publisher","DOI":"10.1007\/978-1-4615-1843-3_2"},{"key":"e_1_2_6_14_1","first-page":"40","article-title":"Hydrochemical methods for the discovery and study of submarine volcanic activity (in Russian)","volume":"5","author":"Gavrilenko G. M.","year":"1984","journal-title":"Volcanol. Seismol."},{"key":"e_1_2_6_15_1","doi-asserted-by":"publisher","DOI":"10.1029\/150GM08"},{"key":"e_1_2_6_16_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0377-0273(96)00031-5"},{"key":"e_1_2_6_17_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0016-7037(96)00304-3"},{"key":"e_1_2_6_18_1","doi-asserted-by":"publisher","DOI":"10.1006\/rwos.2001.0162"},{"key":"e_1_2_6_19_1","doi-asserted-by":"publisher","DOI":"10.1029\/96JB03553"},{"key":"e_1_2_6_20_1","doi-asserted-by":"publisher","DOI":"10.1029\/98JC00146"},{"key":"e_1_2_6_21_1","doi-asserted-by":"publisher","DOI":"10.1006\/rwos.2001.0165"},{"key":"e_1_2_6_22_1","doi-asserted-by":"publisher","DOI":"10.1029\/JB079i008p01196"},{"key":"e_1_2_6_23_1","series-title":"Geol. Soc. London Spec. Publ.","first-page":"119","volume-title":"Intra\u2010oceanic Subduction Systems: Tectonic and Magmatic Processes","author":"Massoth G. J.","year":"2003"},{"key":"e_1_2_6_24_1","doi-asserted-by":"publisher","DOI":"10.1016\/0304-4203(95)00022-J"},{"key":"e_1_2_6_25_1","doi-asserted-by":"publisher","DOI":"10.1029\/95JB03037"},{"key":"e_1_2_6_26_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0016-7037(97)00095-1"},{"key":"e_1_2_6_27_1","doi-asserted-by":"publisher","DOI":"10.1021\/ac00046a006"},{"key":"e_1_2_6_28_1","first-page":"1867","article-title":"Al and pH anomalies in the Manus Basin reappraised: Comments on the paper by T. Gamo et al., \u201cHydrothermal plumes in the eastern Manus Basin, Bismark Sea: CH4, Mn, Al, and pH anomalies,\u201d Deep Sea Res.","volume":"43","author":"Resing J. A.","year":"1996","journal-title":"Part I"},{"key":"e_1_2_6_29_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.epsl.2004.07.028"},{"key":"e_1_2_6_30_1","doi-asserted-by":"publisher","DOI":"10.1111\/j.1365-246X.2006.02897.x"},{"key":"e_1_2_6_31_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0012-821X(98)00142-3"},{"key":"e_1_2_6_32_1","doi-asserted-by":"publisher","DOI":"10.1029\/JB076i011p02562"},{"key":"e_1_2_6_33_1","series-title":"Geol. Soc. London Spec. Publ.","first-page":"99","volume-title":"Intra\u2010oceanic Subduction Systems: Tectonic and Magmatic Processes","author":"Smith I. E. M.","year":"2003"},{"key":"e_1_2_6_34_1","series-title":"Ber. Rep. Ser. 1","volume-title":"Cruise Report R\/V Sonne 135 Cruise","author":"Stoffers P.","year":"1999"},{"key":"e_1_2_6_35_1","doi-asserted-by":"publisher","DOI":"10.1130\/G22227.1"},{"key":"e_1_2_6_36_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0012-821X(02)00465-X"},{"key":"e_1_2_6_37_1","doi-asserted-by":"publisher","DOI":"10.1029\/JB094iB04p04697"},{"key":"e_1_2_6_38_1","doi-asserted-by":"publisher","DOI":"10.1017\/CBO9780511807442"},{"key":"e_1_2_6_39_1","doi-asserted-by":"crossref","unstructured":"Vogt P. R. A.Lowrie D. R.Bracey andR. N.Hey(1976) Subduction of aseismic oceanic ridges: Effects on shape seismicity and other characteristics of consuming plate boundaries Geol. Soc. Am. Spec. Pap. 172 59 pp.","DOI":"10.1130\/SPE172-p1"},{"key":"e_1_2_6_40_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.jvolgeores.2005.03.021"},{"key":"e_1_2_6_41_1","first-page":"735","article-title":"An ultratight fluid sampling system using cold\u2010welded copper tubing","volume":"64","author":"Young C.","year":"1983","journal-title":"Eos Trans. AGU"}],"container-title":["Geochemistry, Geophysics, Geosystems"],"original-title":[],"language":"en","link":[{"URL":"https:\/\/api.wiley.com\/onlinelibrary\/tdm\/v1\/articles\/10.1029%2F2006GC001495","content-type":"unspecified","content-version":"vor","intended-application":"text-mining"},{"URL":"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/pdf\/10.1029\/2006GC001495","content-type":"unspecified","content-version":"vor","intended-application":"similarity-checking"}],"deposited":{"date-parts":[[2023,10,12]],"date-time":"2023-10-12T20:22:56Z","timestamp":1697142176000},"score":1,"resource":{"primary":{"URL":"https:\/\/agupubs.onlinelibrary.wiley.com\/doi\/10.1029\/2006GC001495"}},"subtitle":[],"short-title":[],"issued":{"date-parts":[[2007,7]]},"references-count":40,"journal-issue":{"issue":"7","published-print":{"date-parts":[[2007,7]]}},"alternative-id":["10.1029\/2006GC001495"],"URL":"https:\/\/doi.org\/10.1029\/2006gc001495","archive":["Portico"],"relation":{},"ISSN":["1525-2027","1525-2027"],"issn-type":[{"value":"1525-2027","type":"print"},{"value":"1525-2027","type":"electronic"}],"subject":[],"published":{"date-parts":[[2007,7]]},"article-number":"2006GC001495"}}