Francis J. Turner

University of California, Berkeley

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D. T. Griggs

Environment Agency

W. S. Fyfe

Beth Israel Deaconess Medical Center

Lionel Weiss

University of California, Berkeley

I.Y. Borg

Lawrence Livermore National Laboratory

CHI-SHANG CH'IH

John Verhoogen

University of California, Berkeley

C. S. Venkitasubramanyan

University of California, Berkeley

ROBERTA H. DIXON

Miguel Rodríguez Orozco

Universidad Adventista de Nicaragua

C. M. Gilbert

University of California, Berkeley

Cooperative Institutions

University of California, Berkeley

Planetary Science Institute

University of California, Los Angeles

United States Geological Survey

Lawrence Livermore National Laboratory

University of California System

University of Edinburgh

Czech Academy of Sciences, Institute of Geology

Harvard University

Shell (United States)

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Plastic deformation of dolomite rock at 380 degrees C

American Journal of Science (1954)

Francis J. Turner D. T. Griggs H. C. Heard

10.2475/ajs.252.8.477

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Citations (25)

LINEATION, SYMMETRY, AND INTERNAL MOVEMENT IN MONOCLINIC TECTONITE FABRICS

Geological Society of America Bulletin (1957)

Francis J. Turner

Research Article| January 01, 1957 LINEATION, SYMMETRY, AND INTERNAL MOVEMENT IN MONOCLINIC TECTONITE FABRICS FRANCIS J TURNER FRANCIS J TURNER UNIVERSITY OF CALIFORNIA, BERKELEY, CALIFORNIA Search for other works by this author on: GSW Google Scholar Author and Article Information FRANCIS J TURNER UNIVERSITY OF CALIFORNIA, BERKELEY, CALIFORNIA Publisher: Geological Society of America Received: 31 Oct 1955 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1957, 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 (1957) 68 (1): 1–18. https://doi.org/10.1130/0016-7606(1957)68[1:LSAIMI]2.0.CO;2 Article history Received: 31 Oct 1955 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation FRANCIS J TURNER; LINEATION, SYMMETRY, AND INTERNAL MOVEMENT IN MONOCLINIC TECTONITE FABRICS. GSA Bulletin 1957;; 68 (1): 1–18. doi: https://doi.org/10.1130/0016-7606(1957)68[1:LSAIMI]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 current controversy regarding kinematic interpretation of lineation in schists hinges on the significance of symmetry in tectonite fabrics. Interpretation of such fabrics by Sander and Schmidt is based on an assumption that symmetry of fabric reflects symmetry of internal movements accompanying deformation. In identifying b lineation, which is the symmetry axis of certain monoclinic fabrics, as the principal direction of movements concerned in the evolution of those fabrics, some recent writers have neglected or rejected Sander's postulate regarding symmetry. This course seems unjustified for two reasons: (1) Those who identify regional lineation with movement direction have done so for Precambrian or Paleozoic rocks whose metamorphic and deformational history is ambiguous and often highly complex; the "direction of movement" in such rocks has not been established independently of fabric evidence. (2) Since it was proposed 30 years ago, the symmetry concept of Sander and Schmidt has become strengthened by evidence accruing from studies on fabrics of experimentally deformed metallic aggregates and ceramic bodies. Additional supporting evidence now comes from fabrics of experimentally deformed marble. In deformed marble cylinders symmetry of fabric is identical with symmetry of movement as inferred from measurable strain. The pattern of strain is controlled by the orientation of the cylinder (a mechanically anisotropic aggregate of grains) in relation to applied force. Even in highly deformed material (e.g., where elongation exceeds 500 per cent) the influence of the original anisotropy on symmetry of experimentally induced movement and strain is obvious in the final fabric. 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.

Tectonite

Lineation

10.1130/0016-7606(1957)68[1:lsaimi]2.0.co;2

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Citations (19)

Quake `06: A Campaign to Reduce Earthquake Risk in the San Francisco Bay Area

Seismological Research Letters (2005)

K. L. Knudsen Francis J. Turner

Research Article| January 01, 2005 Quake `06: A Campaign to Reduce Earthquake Risk in the San Francisco Bay Area Keith L. Knudsen; Keith L. Knudsen President and Secretary/Treasurer Northern California Chapter, Earthquake Engineering Research Institute KKnudsen@flash.net, FTurnerSE@accessbee.com Search for other works by this author on: GSW Google Scholar Fred Turner Fred Turner President and Secretary/Treasurer Northern California Chapter, Earthquake Engineering Research Institute KKnudsen@flash.net, FTurnerSE@accessbee.com Search for other works by this author on: GSW Google Scholar Author and Article Information Keith L. Knudsen President and Secretary/Treasurer Northern California Chapter, Earthquake Engineering Research Institute KKnudsen@flash.net, FTurnerSE@accessbee.com Fred Turner President and Secretary/Treasurer Northern California Chapter, Earthquake Engineering Research Institute KKnudsen@flash.net, FTurnerSE@accessbee.com Publisher: Seismological Society of America First Online: 09 Mar 2017 Online ISSN: 1938-2057 Print ISSN: 0895-0695 © 2005 by the Seismological Society of America Seismological Research Letters (2005) 76 (1): 82. https://doi.org/10.1785/gssrl.76.1.82 Article history First Online: 09 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 Keith L. Knudsen, Fred Turner; Quake `06: A Campaign to Reduce Earthquake Risk in the San Francisco Bay Area. Seismological Research Letters 2005;; 76 (1): 82. doi: https://doi.org/10.1785/gssrl.76.1.82 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 SocietySeismological Research Letters Search Advanced Search The Quake `06 Campaign is a volunteer effort capitalizing on the extraordinary earthquake risk management expertise in the San Francisco Bay area. Begun in April 2002, Quake `06 is a four-year campaign to reduce earthquake risk in the Bay Area by the hundredth anniversary of the Great San Francisco Earthquake and Fire of 1906. The campaign is a partnership between the community of earthquake professionals in the Northern California Chapter of the Earthquake Engineering Research Institute and representatives of cities, institutions, agencies, and other earthquake-risk stakeholders. Quake `06 is different from other risk-reduction efforts because our achievements depend on the... You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Quake (natural phenomenon)

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10.1785/gssrl.76.1.82

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

Geological Society of America Bulletin (1953)

DAVID GRIGGS Francis J. Turner IRIS BORG JOHN SOSOKA

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.

Asian American studies

10.1130/0016-7606(1953)64[1327:doympv]2.0.co;2

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Citations (37)

Note on the occurrence of piedmontite in quartz-muscovite-schist from Shotover valley, western Otago, New Zealand

Mineralogical Magazine and Journal of the Mineralogical Society (1933)

Francis J. Turner

Specimens of quartz-muscovite-schist obtained fro: boulders in the Shotover river, western Otago, New Zealand, ere recently examined by the writer and found to contain abundant piedmontite, a mineral not previously recorded from New Zealand. The specimens had been collected twenty years before and were labelled ' micaceous quartz schist coloured with haematite' in the geological collections of the Otago University. The following description is submitted pending further field investigations.

Muscovite

10.1180/minmag.1933.023.142.03

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Citations (5)

COUPLED REACTIONS IN METAMORPHISM: A CORRECTION

Geological Society of America Bulletin (1961)

William S. Fyfe Francis J. Turner John Verhoogen

Research Article| January 01, 1961 COUPLED REACTIONS IN METAMORPHISM: A CORRECTION W. S FYFE; W. S FYFE UNIVERSITY OF CALIFORNIA, BERKELEY, CALIF. Search for other works by this author on: GSW Google Scholar F. J TURNER; F. J TURNER UNIVERSITY OF CALIFORNIA, BERKELEY, CALIF. Search for other works by this author on: GSW Google Scholar J VERHOOGEN J VERHOOGEN UNIVERSITY OF CALIFORNIA, BERKELEY, CALIF. Search for other works by this author on: GSW Google Scholar GSA Bulletin (1961) 72 (1): 169–170. https://doi.org/10.1130/0016-7606(1961)72[169:CRIMAC]2.0.CO;2 Article history received: 21 Jun 1960 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation W. S FYFE, F. J TURNER, J VERHOOGEN; COUPLED REACTIONS IN METAMORPHISM: A CORRECTION. GSA Bulletin 1961;; 72 (1): 169–170. doi: https://doi.org/10.1130/0016-7606(1961)72[169:CRIMAC]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 No abstract available. 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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10.1130/0016-7606(1961)72[169:crimac]2.0.co;2

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Citations (1)

Introduction to petrology

Chemical Geology (1968)

Francis J. Turner

10.1016/0009-2541(68)90038-7

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Citations (7)

Preferred orientation in experimentally deformed limestone

Contributions to Mineralogy and Petrology (1973)

Hans‐Rudolf Wenk C. S. Venkitasubramanyan David W. Baker Francis J. Turner

Pole figure

Recrystallization (geology)

Deformation bands

Texture (cosmology)

Pressure solution

10.1007/bf00373875

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Citations (91)

COMPARISON OF LUNAR WITH TERRESTRIAL AND METEORITIC ROCKS

Proceedings of the National Academy of Sciences (1969)

Francis J. Turner Mabel Ulbrich

This note examines critically recent attempts to identify or closely correlate lunar surface samples-on the basis of alpha-scattering analysis-with terrestrial igneous rocks (basalts) or with eucrite meteorites. Basalts show considerable variety; but all have chemical characteristics inherited from terrestrial mantle rock melted under a limited range of terrestrial pressure-temperature conditions. What is characteristic is not so much the content of any particular element or oxide-e.g., SiO(2) 47-52 per cent-but rather a complete chemical pattern in which such ratios as Fe/Mg and Ca/(Na + K) show consistent relationships to Si content. These are the chemical criteria that might be useful in comparing terrestrial basalt with extraterrestrial rocks. Basalts also have distinctive mineralogical and textural characteristics; and if a lunar or meteoritic rock is to be identified as basalt it must possess these, too.Turkevich's analysis of alpha-scattering data for lunar samples (Surveyor V) show significant departure from basaltic composition: Very high (Ca + K)/Na associated with distinctly high Fe/Mg. In basalts relatively high (Ca + K)/Na-in no case approaching the reported lunar values-tends to be associated with Fe/Mg values lower than average. The same "lunar" pattern of high (Ca + K)/Na and Fe/Mg appears in recorded analyses of eucrite meteorites. In the lunar samples, Ti is notably higher than in basalts, and even more so than in eucrites. If eucrites are of lunar origin their Ti values are, so far, a real anomaly.

Lunar mare

10.1073/pnas.64.3.1016

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Three quartz-albite-sericite-schists from Waipori

University of Otago eBooks (1938)

Francis J. Turner

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