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• W2004109993 abstract "Research Article| December 01, 1981 Structure and stratigraphy of the Luning allochthon and the kinematics of allochthon emplacement, Pilot Mountains, west-central Nevada JOHN S. OLDOW JOHN S. OLDOW 1Department of Geology, Rice University, Houston, Texas 77001 Search for other works by this author on: GSW Google Scholar GSA Bulletin (1981) 92 (12): 888–911. https://doi.org/10.1130/0016-7606(1981)92<888:SASOTL>2.0.CO;2 Article history first online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation JOHN S. OLDOW; Structure and stratigraphy of the Luning allochthon and the kinematics of allochthon emplacement, Pilot Mountains, west-central Nevada. GSA Bulletin 1981;; 92 (12): 888–911. doi: https://doi.org/10.1130/0016-7606(1981)92<888:SASOTL>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 northern Pilot Mountains of west-central Nevada consist of a complexly deformed terrane of imbricate thrust sheets composed of rocks of Mesozoic and possible late Paleozoic ages. Thrust nappes within the allochthonous terrane, named the Luning allochthon, are principally constituted by the Upper Triassic Luning Formation. Locally, the nappes contain numerous imbricate thrust slices, some of which are composed of undifferentiated Sunrise-Gabbs Formation (Triassic and Jurassic) and unnamed volcanic-carbonate assemblages of probable Permian or Triassic age.Three episodes of folding and thrusting are recognized on the basis of folded thrusts and thrusted folds, and deformation and emplacement of the allochthon is constrained as late Mesozoic. Folds apparently formed coevally with thrust faults and fold geometry is used to determine approximate directions of thrust transport. Thrust displacements are responsible for 35 to 40 km of an estimated 70 km of intra-allochthon contraction which is inferred from lithofacies analysis of rocks juxtaposed by thrust nappes and from the structural overlap of imbricate thrusts.The history of thrust displacement is complex and involves three directions of motion on a regionally extensive detachment surface, the Luning thrust. First motion, from northwest to southeast, resulted in the major component of stratal contraction and is the probable result of northwest-southeast regional compression. The final two episodes of motion are northeast to southwest followed by east to west; they resulted in small displacements and are possibly the product of gravity sliding of the thrust sheets into a depression formed beneath part of the allochthon within the autochthon. The site of downwarp in the autochthon may have formed by either load-induced subsidence or regional compression. 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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• W2004109993 title "Structure and stratigraphy of the Luning allochthon and the kinematics of allochthon emplacement, Pilot Mountains, west-central Nevada" @default.
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