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DEFORMATION OF YULE MARBLE: PART V—EFFECTS AT 300°C

1953; Geological Society of America; Volume: 64; Issue: 12 Linguagem: Inglês

10.1130/0016-7606(1953)64[1327

1943-2674

DAVID GRIGGS, Francis J. Turner, IRIS BORG, JOHN SOSOKA,

Maritime and Coastal Archaeology

Research Article| December 01, 1953 DEFORMATION OF YULE MARBLE: PART V—EFFECTS AT 300°C DAVID GRIGGS; DAVID GRIGGS INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF. Search for other works by this author on: GSW Google Scholar FRANCIS J TURNER; FRANCIS J TURNER INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF. Search for other works by this author on: GSW Google Scholar IRIS BORG; IRIS BORG INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF. Search for other works by this author on: GSW Google Scholar JOHN SOSOKA JOHN SOSOKA INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF. Search for other works by this author on: GSW Google Scholar Author and Article Information DAVID GRIGGS INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF. FRANCIS J TURNER INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF. IRIS BORG INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF. JOHN SOSOKA INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; UNIVERSITY OF CALIFORNIA, BERKELEY 4, CALIF.; INSTITUTE OF GEOPHYSICS, UNIVERSITY OF CALIFORNIA, LOS ANGELES 24, CALIF. Publisher: Geological Society of America Received: 24 Feb 1953 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1953, 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 (1953) 64 (12): 1327–1342. https://doi.org/10.1130/0016-7606(1953)64[1327:DOYMPV]2.0.CO;2 Article history Received: 24 Feb 1953 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 DAVID GRIGGS, FRANCIS J TURNER, IRIS BORG, JOHN SOSOKA; DEFORMATION OF YULE MARBLE: PART V—EFFECTS AT 300°C. GSA Bulletin 1953;; 64 (12): 1327–1342. doi: https://doi.org/10.1130/0016-7606(1953)64[1327:DOYMPV]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 Yule marble has been deformed at 300°C, at 5000 atmospheres confining pressure, under conditions otherwise identical with those at room temperature and at 15O°C (Parts I-IV). The important new effects are: apparent development of intergranular flow (recrystallization1) and development of textures closely resembling those of naturally deformed marble. Fabric measurements on the deformed material show trends nearly identical with those observed in specimens deformed at lower temperature (Parts III and IV). The effect of interstitial water is negligible except for lowering of strength similar to that observed at room temperature. Slow rates of deformation seem to favor recrystallization. Granite has been deformed plastically for the first time. 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.