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• W2093738971 abstract "Research Article| December 01, 2014 Metallogenesis and Mineralization of Intraoceanic Arcs II: The Aeolian, Izu-Bonin, Mariana, and Kermadec Arcs, and the Manus Backarc Basin—Introduction C. E. J. de Ronde; C. E. J. de Ronde † 1GNS Science, P.O. Box 30-368, Lower Hutt, New Zealand †Correesponding author: e-mail, Cornel.deRonde@gns.cri.nz Search for other works by this author on: GSW Google Scholar J. R. Hein; J. R. Hein 2U.S. Geological Survey, 400 Natural Bridges Dr., Santa Cruz, California 95060 Search for other works by this author on: GSW Google Scholar D. A. Butterfield D. A. Butterfield 3University of Washington, Joint Institute for the Study of the Atmosphere and Oceans, Box 354925, Seattle, Washington 98195 Search for other works by this author on: GSW Google Scholar Economic Geology (2014) 109 (8): 2073–2077. https://doi.org/10.2113/econgeo.109.8.2073 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation C. E. J. de Ronde, J. R. Hein, D. A. Butterfield; Metallogenesis and Mineralization of Intraoceanic Arcs II: The Aeolian, Izu-Bonin, Mariana, and Kermadec Arcs, and the Manus Backarc Basin—Introduction. Economic Geology 2014;; 109 (8): 2073–2077. doi: https://doi.org/10.2113/econgeo.109.8.2073 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 SocietyEconomic Geology Search Advanced Search It is estimated that ~75% of Earth’s volcanism occurs on the seafloor, especially at divergent plate boundaries like the East Pacific Rise and the mid-Atlantic Ridge (Crisp, 1984). These features are known as mid-ocean ridges (MORs), which are large-scale lineaments marking areas of seafloor spreading where lavas are extruded onto the seafloor, and subseafloor dike emplacement is common. A metaphor commonly ascribed to this process is “conveyor belt,” where newly formed oceanic crust, invariably of basaltic composition, moves inexorably away from the axis of the MORs as the forces of plate tectonics take hold. Conversely, at the other... You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2093738971 title "Metallogenesis and Mineralization of Intraoceanic Arcs II: The Aeolian, Izu-Bonin, Mariana, and Kermadec Arcs, and the Manus Backarc Basin--Introduction" @default.
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