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Late Paleozoic-Mesozoic tectonic evolution of the Trans-Altai and South Gobi Zones in southern Mongolia based on structural and geochronological data

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F14%3A10173685" target="_blank" >RIV/00216208:11310/14:10173685 - isvavai.cz</a>

  • Alternative codes found

    RIV/00025798:_____/14:00000018

  • Result on the web

    <a href="http://dx.doi.org/10.1016/j.gr.2013.03.014" target="_blank" >http://dx.doi.org/10.1016/j.gr.2013.03.014</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.gr.2013.03.014" target="_blank" >10.1016/j.gr.2013.03.014</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Late Paleozoic-Mesozoic tectonic evolution of the Trans-Altai and South Gobi Zones in southern Mongolia based on structural and geochronological data

  • Original language description

    The Trans-Altai Zone in southern Mongolia is characterized by thrusting of greenschist-facies Silurian oceanic rocks over Devonian and Lower Carboniferous volcano-sedimentary sequences, by E-W directed folding affecting the early Carboniferous volcanic rocks, and by the development of N-S trending magmatic fabrics in the Devonian-Carboniferous arc plutons. This structural pattern is interpreted as the result of early Carboniferous thick-skinned E-W directed nappe stacking of oceanic crust associated with syn-compressional emplacement of a magmatic arc. The southernmost South Gobi Zone represents a Proterozoic continental domain affected by shallow crustal greenschist-facies detachments of Ordovician and Devonian cover sequences from the Proterozoic substratum, whereas supracrustal Carboniferous volcanic rocks and Permian sediments were folded into N-S upright folds. This structural pattern implies E-W directed thin-skinned tectonics operating from the late Carboniferous to the Permian,

  • 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

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

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

    Gondwana Research

  • ISSN

    1342-937X

  • e-ISSN

  • Volume of the periodical

    25

  • Issue of the periodical within the volume

    1

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    29

  • Pages from-to

    309-337

  • UT code for WoS article

    000328099900018

  • EID of the result in the Scopus database