Research Article| January 01, 2005 New hydrothermal activity and alkalic volcanism in the backarc Coriolis Troughs, Vanuatu Timothy F. McConachy; Timothy F. McConachy 1Commonwealth Scientific and Industrial Research Organisation, Exploration and Mining, PO Box 136, North Ryde, Sydney NSW 1670, Australia Search for other works by this author on: GSW Google Scholar Richard J. Arculus; Richard J. Arculus 2Department of Earth and Marine Sciences, Australian National University, Canberra ACT 0200, Australia Search for other works by this author on: GSW Google Scholar Christopher J. Yeats; Christopher J. Yeats 3Commonwealth Scientific and Industrial Research Organisation, Exploration and Mining, PO Box 136, North Ryde, Sydney NSW 1670, Australia Search for other works by this author on: GSW Google Scholar Raymond A. Binns; Raymond A. Binns 4Commonwealth Scientific and Industrial Research Organisation, Exploration and Mining, PO Box 136, North Ryde, Sydney NSW 1670, Australia, and Department of Earth and Marine Sciences, Australian National University, Canberra ACT 0200, Australia Search for other works by this author on: GSW Google Scholar Fernando J.A.S. Barriga; Fernando J.A.S. Barriga 5Department of Geology, University of Lisbon, Edificio, Piso 5, Campo Grande, 1749-016 Lisboa, Portugal Search for other works by this author on: GSW Google Scholar Brent I.A. McInnes; Brent I.A. McInnes 6Commonwealth Scientific and Industrial Research Organisation, Petroleum Resources, PO Box 136, North Ryde, Sydney NSW 1670, Australia Search for other works by this author on: GSW Google Scholar Stephen Sestak; Stephen Sestak 6Commonwealth Scientific and Industrial Research Organisation, Petroleum Resources, PO Box 136, North Ryde, Sydney NSW 1670, Australia Search for other works by this author on: GSW Google Scholar Robina Sharpe; Robina Sharpe 7Centre for Ore Deposit Research, University of Tasmania, PO Box 252-79, Hobart, Tasmania 7001, Australia Search for other works by this author on: GSW Google Scholar Brooks Rakau; Brooks Rakau 8Department of Geology, Mines and Water Resources, Private Mail Bag 001, Port Vila, Republic of Vanuatu Search for other works by this author on: GSW Google Scholar Tony Tevi Tony Tevi 8Department of Geology, Mines and Water Resources, Private Mail Bag 001, Port Vila, Republic of Vanuatu Search for other works by this author on: GSW Google Scholar Geology (2005) 33 (1): 61–64. https://doi.org/10.1130/G20870.1 Article history received: 29 Jun 2004 rev-recd: 17 Sep 2004 accepted: 22 Sep 2004 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Timothy F. McConachy, Richard J. Arculus, Christopher J. Yeats, Raymond A. Binns, Fernando J.A.S. Barriga, Brent I.A. McInnes, Stephen Sestak, Robina Sharpe, Brooks Rakau, Tony Tevi; New hydrothermal activity and alkalic volcanism in the backarc Coriolis Troughs, Vanuatu. Geology 2005;; 33 (1): 61–64. doi: https://doi.org/10.1130/G20870.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract The Vanuatu Australia Vents Expedition (VAVE) to the Coriolis Troughs in southern Vanuatu during September 2001 aboard the RV Franklin discovered a new hydrothermal vent field—herein informally named Nifonea—and recent alkalic volcanic activity. The Nifonea field in the central Vate Trough was located by coincident light transmission and CH4 anomalies in a hydrothermal plume of ∼60 km2 extent, best developed between 1600 and 1750 m depth at ∼150 m above the seafloor. Extensive hydrothermal fauna and yellow-brown crusts and mounds cover an area of ∼1 km2. Very fresh, glassy, variably vesicular, sparsely phyric and aphyric basalt, trachybasalt, and basaltic trachyandesite (with ∼5– 6 wt% combined alkalies at ∼51%–53% SiO2 and enriched light rare earth elements, Nb, and Zr) samples were dredged from youthful curtain, tube, and sheet flows, plus iron oxyhydroxide deposits. The alkalic composition of lavas in this tectonic setting is unique and attributed to thin ocean crust being developed in an incipient rifting phase involving a relatively low percentage of source-mantle melting. The Coriolis Troughs are among Earth's most youthful backarc basins and thus provide valuable insights to incipient rifting and hydrothermal processes. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.