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
—