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Dacite and Related Sediment from the West Mariana Ridge, Philippine Sea

1970; Geological Society of America; Volume: 81; Issue: 7 Linguagem: Inglês

10.1130/0016-7606(1970)81[2143

1943-2674

Daniel E. Karig, William E. Glassley,

Geological and Geophysical Studies

Research Article| July 01, 1970 Dacite and Related Sediment from the West Mariana Ridge, Philippine Sea DANIEL E KARIG; DANIEL E KARIG Scripps Institution of Oceanography, University of California at San Diego, La Jolla, California 92037 Search for other works by this author on: GSW Google Scholar WILLIAM E GLASSLEY WILLIAM E GLASSLEY Scripps Institution of Oceanography, University of California at San Diego, La Jolla, California 92037 Search for other works by this author on: GSW Google Scholar Author and Article Information DANIEL E KARIG Scripps Institution of Oceanography, University of California at San Diego, La Jolla, California 92037 WILLIAM E GLASSLEY Scripps Institution of Oceanography, University of California at San Diego, La Jolla, California 92037 Publisher: Geological Society of America Received: 02 Feb 1970 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1970, The Geological Society of America, Inc. Copyright is not claimed on any material prepared by U.S. government employees within the scope of their employment. GSA Bulletin (1970) 81 (7): 2143–2146. https://doi.org/10.1130/0016-7606(1970)81[2143:DARSFT]2.0.CO;2 Article history Received: 02 Feb 1970 First Online: 02 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 DANIEL E KARIG, WILLIAM E GLASSLEY; Dacite and Related Sediment from the West Mariana Ridge, Philippine Sea. GSA Bulletin 1970;; 81 (7): 2143–2146. doi: https://doi.org/10.1130/0016-7606(1970)81[2143:DARSFT]2.0.CO;2 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 SocietyGSA Bulletin Search Advanced Search Abstract Dredge hauls from the West Mariana Ridge recovered vesicular dacitic lava and late Pliocene sandstone from depths between 3000 and 4000 m. The sandstone, consisting of glass shards identical to the dacitic glass and pelagic foram tests, appears to have been deposited contemporaneously with the lavas. The very high vesicularity of the dacite suggests that it was erupted near sea level, implying Quaternary subsidence of the West Mariana Ridge. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.