PROPOSED CLASSIFICATION OF VOLCANICLASTIC SEDIMENTS AND ROCKS
1961; Geological Society of America; Volume: 72; Issue: 9 Linguagem: Inglês
10.1130/0016-7606(1961)72[1409
ISSN1943-2674
Autores Tópico(s)Hydrocarbon exploration and reservoir analysis
ResumoResearch Article| September 01, 1961 PROPOSED CLASSIFICATION OF VOLCANICLASTIC SEDIMENTS AND ROCKS RICHARD V FISHER RICHARD V FISHER UNIVERSITY OF CALIFORNIA AT SANTA BARBARA, GOLETA, CALIF. Search for other works by this author on: GSW Google Scholar Author and Article Information RICHARD V FISHER UNIVERSITY OF CALIFORNIA AT SANTA BARBARA, GOLETA, CALIF. Publisher: Geological Society of America Received: 27 Dec 1960 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1961, 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 (1961) 72 (9): 1409–1414. https://doi.org/10.1130/0016-7606(1961)72[1409:PCOVSA]2.0.CO;2 Article history Received: 27 Dec 1960 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 RICHARD V FISHER; PROPOSED CLASSIFICATION OF VOLCANICLASTIC SEDIMENTS AND ROCKS. GSA Bulletin 1961;; 72 (9): 1409–1414. doi: https://doi.org/10.1130/0016-7606(1961)72[1409:PCOVSA]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 Volcaniclastic sediments and rocks are divided here into autoclastic, pyroclastic, and epiclastic types with grain-size limits the same as non-volcanic epiclastic rocks. Autoclastic rocks contain fragments that are produced within (but not usually extruded from) volcanic vents, during movement of lava flows, or by gas explosions within flows that have ceased to flow. Pyroclastic rocks contain fragments produced by volcanic explosion and extruded as discrete particles from volcanic vents. Epiclastic volcanic rocks contain fragments produced by weathering and erosion of solidified or lithified volcanic rocks of any type. Volcaniclastic types may be mixed in all proportions with each other or with nonvolcanic fragments, although these mixtures are not designated within this classification. A non-genetic category, based only upon particle size and the presence of volcanic material, is included for rocks with clasts of unknown origin. 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.
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