Izu-Bonin-Mariana Forearc Crust as a Modern Ophiolite Analogue

• DOI: 10.2113/gselements.10.2.115
• Publication Date: 2014-04-29T14:41:10Z
• Authors: O. Ishizuka; K. Tani; M. K. Reagan
• Keywords: Geological survey

Research Article| April 01, 2014 Izu-Bonin-Mariana Forearc Crust as a Modern Ophiolite Analogue Osamu Ishizuka; Ishizuka 1Institute of Geology and Geoinformation, Geological Survey Japan/AIST, Central 7, 1-1-1, Higashi, Tsukuba, Ibaraki, 305-8567, JapanE-mail: [e-mail]2IFREE, JAMSTEC, 2-15 Natsushima, Yokosuka, Kanagawa, 237-0061, Japan Search for other works by this author on: GSW Google Scholar Kenichiro Tani; Tani 2IFREE, Mark K. Reagan 3Department Geoscience, 121 Trowbridge Hall, University Iowa, Iowa City, IA 52242, USA Author Article Information Publisher: Mineralogical Society America First Online: 09 Mar 2017 Online ISSN: 1811-5217 Print 1811-5209 © the Elements (2014) 10 (2): 115–120. https://doi.org/10.2113/gselements.10.2.115 history Cite View This Citation Add to Manager Share Icon Facebook Twitter LinkedIn Email Permissions Site Ishizuka, Tani, Reagan; Analogue. 2014;; doi: Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Dropdown Menu input auto suggest filter your All ContentBy SocietyElements Advanced Abstract Recent geological geophysical surveys in forearc have revealed occurrence on seafloor oceanic crust generated initial stages subduction earliest stage island arc formation. The magmatism after initiation basalts, subsequently, boninitic tholeiitic calc-alkaline lavas were produced. Collectively, these rocks make up extrusive sequence crust. volcanic stratigraphy its time-progressive development are analogous those documented from many suprasubduction zone ophiolites. Most ophiolites may be on-land fragments crust, produced during early development. You do not access content, please speak institutional administrator if you feel should access.