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Polymetamorphic evolution of the granulite-facies Paleoproterozoic basement of the Kabul Block, Afghanistan

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F15%3A10312141" target="_blank" >RIV/00216208:11310/15:10312141 - isvavai.cz</a>

  • Result on the web

    <a href="http://dx.doi.org/10.1007/s00710-015-0371-9" target="_blank" >http://dx.doi.org/10.1007/s00710-015-0371-9</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1007/s00710-015-0371-9" target="_blank" >10.1007/s00710-015-0371-9</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Polymetamorphic evolution of the granulite-facies Paleoproterozoic basement of the Kabul Block, Afghanistan

  • Original language description

    The Kabul Block is an elongate crustal fragment which cuts across the Afghan Central Blocks, adjoining the Indian and Eurasian continents. Bounded by major strike slip faults and ophiolitic material thrust onto either side, the block contains a stronglymetamorphosed basement consisting of some of the only quantifiably Proterozoic rocks south of the Herat-Panjshir Suture Zone. The basement rocks crop-out extensively in the vicinity of Kabul City and consist predominantly of migmatites, gneisses, schistsand small amounts of higher-grade granulite-facies rocks. Granulite-facies assemblages were identified in felsic and mafic siliceous rocks as well as impure carbonates. Granulite-facies conditions are recorded by the presence of orthopyroxene overgrowing biotite in felsic rocks; by orthopyroxene overgrowing amphibole in mafic rocks and by the presence of olivine and clinohumite in the marbles. The granulite-facies assemblages are overprinted by a younger amphibolite-facies event that is

  • 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/GA13-06958S" target="_blank" >GA13-06958S: Mineral and textural signatures recording pre-exhumation and pre-collision history of the HP/UHPM rocks in orogenic zone</a><br>

  • Continuities

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

Others

  • Publication year

    2015

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Mineralogy and Petrology

  • ISSN

    0930-0708

  • e-ISSN

  • Volume of the periodical

    109

  • Issue of the periodical within the volume

    4

  • Country of publishing house

    AT - AUSTRIA

  • Number of pages

    22

  • Pages from-to

    463-484

  • UT code for WoS article

    000358253300008

  • EID of the result in the Scopus database

    2-s2.0-84937968291