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Fault-related rocks: Suggestions for terminology
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1984
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EngineeringFault GeologyEarth ScienceRegional GeologyGeological DataFault-related RocksRegional TectonicsNeotectonicsSeismic CycleGeographyGeologyTectonicsFault GeometryStructural GeologyCivil EngineeringNew OrleansEconomic GeologyRock BurstEarth SciencesPetrology
Research Article| July 01, 1984 Fault-related rocks: Suggestions for terminology D. U. Wise; D. U. Wise 1Department of Geology and Geography, University of Massachusetts, Amherst, Massachusetts 01003 Search for other works by this author on: GSW Google Scholar D. E. Dunn; D. E. Dunn 2Department of Earth Sciences, University of New Orleans, New Orleans, Louisiana 70148 Search for other works by this author on: GSW Google Scholar J. T. Engelder; J. T. Engelder 3Lamont-Doherty Geological Observatory, Palisades, New York 10946 Search for other works by this author on: GSW Google Scholar P. A. Geiser; P. A. Geiser 4Department of Geology, University of Connecticut, Storrs, Connecticut 06268 Search for other works by this author on: GSW Google Scholar R. D. Hatcher; R. D. Hatcher 5Department of Geology, University of South Carolina, Columbia, South Carolina 29208 Search for other works by this author on: GSW Google Scholar S. A. Kish; S. A. Kish 6Department of Geology, Florida State University, Tallahassee, Florida 32306 Search for other works by this author on: GSW Google Scholar A. L. Odom; A. L. Odom 7Department of Geology, Florida State University, Tallahassee, Florida 32306 Search for other works by this author on: GSW Google Scholar S. Schamel S. Schamel 8Earth Sciences and Resources Institute, University of South Carolina, Columbia, South Carolina 29208 Search for other works by this author on: GSW Google Scholar Author and Article Information D. U. Wise 1Department of Geology and Geography, University of Massachusetts, Amherst, Massachusetts 01003 D. E. Dunn 2Department of Earth Sciences, University of New Orleans, New Orleans, Louisiana 70148 J. T. Engelder 3Lamont-Doherty Geological Observatory, Palisades, New York 10946 P. A. Geiser 4Department of Geology, University of Connecticut, Storrs, Connecticut 06268 R. D. Hatcher 5Department of Geology, University of South Carolina, Columbia, South Carolina 29208 S. A. Kish 6Department of Geology, Florida State University, Tallahassee, Florida 32306 A. L. Odom 7Department of Geology, Florida State University, Tallahassee, Florida 32306 S. Schamel 8Earth Sciences and Resources Institute, University of South Carolina, Columbia, South Carolina 29208 Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1984) 12 (7): 391–394. https://doi.org/10.1130/0091-7613(1984)12<391:FRSFT>2.0.CO;2 Article history First Online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Tools Icon Tools Get Permissions Search Site Citation D. U. Wise, D. E. Dunn, J. T. Engelder, P. A. Geiser, R. D. Hatcher, S. A. Kish, A. L. Odom, S. Schamel; Fault-related rocks: Suggestions for terminology. Geology 1984;; 12 (7): 391–394. doi: https://doi.org/10.1130/0091-7613(1984)12<391:FRSFT>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 Many traditional terms for fault-related rocks have undergone recent dynamic metamorphism under high-pressure discussions by various groups of specialists. A generally acceptable simplified framework encompassing these and associated structural terms is now needed for many geologic, engineering, and legal purposes. Such a framework is proposed here, focusing on a rate-of-strain versus rate-of-recovery diagram and relating this framework to the products of brittle and ductile deformation along faults. 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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