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Switch from Thrusting to Normal Shearing in the Zanskar Shear Zone, NW Himalaya: Implications for Channel Flow

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F14%3A00000014" target="_blank" >RIV/00025798:_____/14:00000014 - isvavai.cz</a>

  • Result on the web

    <a href="http://gsabulletin.gsapubs.org/content/126/7-8/892.abstract" target="_blank" >http://gsabulletin.gsapubs.org/content/126/7-8/892.abstract</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1130/B30817.1" target="_blank" >10.1130/B30817.1</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Switch from Thrusting to Normal Shearing in the Zanskar Shear Zone, NW Himalaya: Implications for Channel Flow

  • Original language description

    The Zanskar Shear Zone (ZSZ) is a ductile, normal-sense shear zone that exploited the contact between the High Himalayan Crystalline series and the Tethyan Sedimentary Series. The ZSZ is an extension of the South Tibetan Detachment System and in Zanskaraccommodated 24 km of normal movement. Early thrusting is preserved in footwall and hanging wall and is overprinted by normal shearing. Thrusting and normal shearing were co-planar and co-directional, with SW-directed thrusting overprinted by NE-directednormal shearing: a simple inversion of movement sense. The telescoped isograds related to normal shearing define a broad pattern of colder rocks on top of hotter. However, we found preserved thrust-related metamorphic series, with hotter rocks on top ofcolder, severely telescoped by normal shearing. Some determinations of the amount of displacement and thinning on the ZSZ prior to the current work have assumed a steady-state crustal profile and have disregarded pre-existing perturbatio

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>x</sub> - Unclassified - Peer-reviewed scientific article (Jimp, Jsc and Jost)

  • CEP classification

    DB - Geology and mineralogy

  • OECD FORD branch

Result continuities

  • Project

    <a href="/en/project/LK11202" target="_blank" >LK11202: The role of Paleozoic accretionary and collisanal orogens on the formation and growth of continental crust</a><br>

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Others

  • Publication year

    2014

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Geological Society of America Bulletin

  • ISSN

    0016-7606

  • e-ISSN

  • Volume of the periodical

    126

  • Issue of the periodical within the volume

    7-8

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    33

  • Pages from-to

    892-924

  • UT code for WoS article

    000341193900002

  • EID of the result in the Scopus database