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• W2023147637 abstract "Research Article| June 01, 1985 Detachment faulting and its relationship to older structural events on Saddle Island, River Mountains, Clark County, Nevada Pierre Choukroune; Pierre Choukroune 1Laboratoire de Géologie Structurale, Université de Rennes 1, Campus de Beaulieu, 35042 Rennes CEDEX France Search for other works by this author on: GSW Google Scholar Eugene I. Smith Eugene I. Smith 2Department of Geoscience, University of Nevada, Las Vegas, Nevada 89154 Search for other works by this author on: GSW Google Scholar Author and Article Information Pierre Choukroune 1Laboratoire de Géologie Structurale, Université de Rennes 1, Campus de Beaulieu, 35042 Rennes CEDEX France Eugene I. Smith 2Department of Geoscience, University of Nevada, Las Vegas, Nevada 89154 Publisher: Geological Society of America First Online: 01 Jun 2017 Online ISSN: 1943-2682 Print ISSN: 0091-7613 Geological Society of America Geology (1985) 13 (6): 421–424. https://doi.org/10.1130/0091-7613(1985)13<421:DFAIRT>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 Permissions Search Site Citation Pierre Choukroune, Eugene I. Smith; Detachment faulting and its relationship to older structural events on Saddle Island, River Mountains, Clark County, Nevada. Geology 1985;; 13 (6): 421–424. doi: https://doi.org/10.1130/0091-7613(1985)13<421:DFAIRT>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 On Saddle Island a detachment fault of Tertiary age separates two structurally different plates. In the lower plate, Precambrian amphibolite and gneiss are strongly overprinted by a subhorizontal mylonitic foliation that may have formed during east-directed overthrusting of Sevier age. The mylonitic foliation is in turn overprinted by a later brittle deformation expressed by the detachment fault and by two gently north-dipping zones of anastomosing faults that outline crude lenslike masses of unfractured rock. These fault zones are probably an expression of the brittle deformation that dominates during a detachment event and are themselves cut by north-south–trending, high-angle normal faults related to a second brittle deformation. Our field measurements of the orientation of fault planes and striae on these fault planes suggest that the orientation of the least principal stress direction (σ3) changed during the brittle faulting event from north-northwest to northwest-southeast. Neither of these directions of extension is compatible with the strain field associated with the earlier ductile shearing responsible for the development of the mylonitic foliation. 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." @default.
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• W2023147637 title "Detachment faulting and its relationship to older structural events on Saddle Island, River Mountains, Clark County, Nevada" @default.
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