Palaeomagnetic and structural constraints on 90 anticlockwise rotation in SW Mongolia during the Permo?Triassic: Implications for Altaid oroclinal bending. Preliminary palaeomagnetic results
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F14%3A00000083" target="_blank" >RIV/00025798:_____/14:00000083 - isvavai.cz</a>
Výsledek na webu
<a href="http://www.sciencedirect.com/science/article/pii/S1367912014003265" target="_blank" >http://www.sciencedirect.com/science/article/pii/S1367912014003265</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.jseaes.2014.07.039" target="_blank" >10.1016/j.jseaes.2014.07.039</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Palaeomagnetic and structural constraints on 90 anticlockwise rotation in SW Mongolia during the Permo?Triassic: Implications for Altaid oroclinal bending. Preliminary palaeomagnetic results
Popis výsledku v původním jazyce
New and published paleomagnetic measurements from Trans Altai and South Gobi zones in south Mongolia document large tectonic motions in between Late Carboniferous and Triassic. Magnetic inclinations confirm equatorial position of south Mongolian terranesin Late Carboniferous?Permian times. The evolution of magnetic declinations indicates 90°anticlockwise rotation in between latest Carboniferous and Early Triassic of all studied tectonic units around the Eulerian pole located close to axis of Mongolianorocline. The anticlockwise rotation continues in Triassic being accompanied by a majordrift to the north. The structural and published geochronological data suggest Carboniferous E?W shortening of the whole region resulting in N?S trend of all continental and oceanic geological units followed by orthogonal N?S shortening during Late Permian to Early Jurassic. Both paleomagnetic and geological data converge in a tectonic model of oroclinal bending of Mongolian ribbon continent, westerly
Název v anglickém jazyce
Palaeomagnetic and structural constraints on 90 anticlockwise rotation in SW Mongolia during the Permo?Triassic: Implications for Altaid oroclinal bending. Preliminary palaeomagnetic results
Popis výsledku anglicky
New and published paleomagnetic measurements from Trans Altai and South Gobi zones in south Mongolia document large tectonic motions in between Late Carboniferous and Triassic. Magnetic inclinations confirm equatorial position of south Mongolian terranesin Late Carboniferous?Permian times. The evolution of magnetic declinations indicates 90°anticlockwise rotation in between latest Carboniferous and Early Triassic of all studied tectonic units around the Eulerian pole located close to axis of Mongolianorocline. The anticlockwise rotation continues in Triassic being accompanied by a majordrift to the north. The structural and published geochronological data suggest Carboniferous E?W shortening of the whole region resulting in N?S trend of all continental and oceanic geological units followed by orthogonal N?S shortening during Late Permian to Early Jurassic. Both paleomagnetic and geological data converge in a tectonic model of oroclinal bending of Mongolian ribbon continent, westerly
Klasifikace
Druh
J<sub>x</sub> - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)
CEP obor
DB - Geologie a mineralogie
OECD FORD obor
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Návaznosti výsledku
Projekt
Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.
Návaznosti
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Journal of Asian Earth Sciences
ISSN
1367-9120
e-ISSN
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Svazek periodika
94
Číslo periodika v rámci svazku
Spec. iss
Stát vydavatele periodika
NL - Nizozemsko
Počet stran výsledku
14
Strana od-do
157-171
Kód UT WoS článku
000343351000013
EID výsledku v databázi Scopus
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