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- W2069888915 abstract "Research Article| November 01, 2000 Stratified granular media beneath large slide blocks: Implications for mode of emplacement Mark H. Anders; Mark H. Anders 1Department of Earth and Environmental Sciences and Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA Search for other works by this author on: GSW Google Scholar Einat Aharonov; Einat Aharonov 1Department of Earth and Environmental Sciences and Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA Search for other works by this author on: GSW Google Scholar John J. Walsh John J. Walsh 1Department of Earth and Environmental Sciences and Lamont-Doherty Earth Observatory, Columbia University, Palisades, New York 10964, USA Search for other works by this author on: GSW Google Scholar Geology (2000) 28 (11): 971–974. https://doi.org/10.1130/0091-7613(2000)28<971:SGMBLS>2.0.CO;2 Article history received: 19 May 2000 rev-recd: 01 Aug 2000 accepted: 07 Aug 2000 first online: 02 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Mark H. Anders, Einat Aharonov, John J. Walsh; Stratified granular media beneath large slide blocks: Implications for mode of emplacement. Geology 2000;; 28 (11): 971–974. doi: https://doi.org/10.1130/0091-7613(2000)28<971:SGMBLS>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 SocietyGeology Search Advanced Search Abstract We have examined the bottoms of many large slide blocks and found basal layers of well-rounded, fine- to coarse-grained, granular material that typically has the appearance of stratified, stream-deposited sandstone or conglomerate. Stratification is subparallel to the basal surface (detachment) and is typically inversely graded, although normal grading and banding of material are present in some samples. The sandstone-conglomerate–like material of the basal layer can be traced continuously from the detachment surface directly into the upper plate, where it is localized within clastic dikes. Although many of the physical characteristics of these basal layers appear to be those associated with water-laid stream deposits, there is no direct evidence of fluid involvement. We interpret the sandstone-conglomerate–like material in the basal layer to be produced by mechanical sieving in a high-energy fluidized environment under a rapidly moving rock mass during a single catastrophic emplacement event. These sandstone-conglomerate layers found along detachment surfaces may prove to be important in determining whether a detached block is simply a gravity slide or the upper-plate remnant of a low-angle normal fault associated with significant crustal extension. 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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- W2069888915 title "Stratified granular media beneath large slide blocks: Implications for mode of emplacement" @default.
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