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Climate: A Primary Control of Sedimentation in the Peru-Chile Trench

1969; Geological Society of America; Volume: 80; Issue: 9 Linguagem: Inglês

10.1130/0016-7606(1969)80[1849

1943-2674

CARLOS GALLI-OLIVIER,

Geological and Tectonic Studies in Latin America

Research Article| September 01, 1969 Climate: A Primary Control of Sedimentation in the Peru-Chile Trench CARLOS GALLI-OLIVIER CARLOS GALLI-OLIVIER Department of Geology, Wayne State University, Detroit, Michigan Search for other works by this author on: GSW Google Scholar Author and Article Information CARLOS GALLI-OLIVIER Department of Geology, Wayne State University, Detroit, Michigan Publisher: Geological Society of America Received: 15 Jan 1969 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1969, 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 (1969) 80 (9): 1849–1852. https://doi.org/10.1130/0016-7606(1969)80[1849:CAPCOS]2.0.CO;2 Article history Received: 15 Jan 1969 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation CARLOS GALLI-OLIVIER; Climate: A Primary Control of Sedimentation in the Peru-Chile Trench. GSA Bulletin 1969;; 80 (9): 1849–1852. doi: https://doi.org/10.1130/0016-7606(1969)80[1849:CAPCOS]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 The Peru-Chile Trench and the Andes present perhaps the greatest relief known on earth. It seems, however, that climate, rather than continental relief, rate of uplift, or structure, was the major control over the rate of sedimentation. The climate factor should be given greater consideration in interpreting the sediments of geosynclines. 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.