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

Kód výsledku v 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>

Nalezeny alternativní kódy

RIV/00025798:_____/14:00000018

Výsledek na webu

<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>

Jazyk výsledku

angličtina

Název v původním jazyce

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

Popis výsledku v původním jazyce

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,

Název v anglickém jazyce

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

Popis výsledku anglicky

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,

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

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

Název periodika

Gondwana Research

ISSN

1342-937X

e-ISSN

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Svazek periodika

25

Číslo periodika v rámci svazku

1

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

29

Strana od-do

309-337

Kód UT WoS článku

000328099900018

EID výsledku v databázi Scopus

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