Paleozoic tectonothermal history of the amalgamation of the Tarim-North China and Mongolian collages
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F25%3A10169569" target="_blank" >RIV/00025798:_____/25:10169569 - isvavai.cz</a>
Result on the web
<a href="https://doi.org/10.1144/jgs2024-100" target="_blank" >https://doi.org/10.1144/jgs2024-100</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1144/jgs2024-100" target="_blank" >10.1144/jgs2024-100</a>
Alternative languages
Result language
angličtina
Original language name
Paleozoic tectonothermal history of the amalgamation of the Tarim-North China and Mongolian collages
Original language description
In the Mongolian Collage, metamorphic pressure-temperature (P-T) and timing reveal a one-stage evolution defined by a duality of late Neoproterozoic-Ordovician subduction-related low T/P metamorphism and suprasubduction high T/P metamorphism recorded in the Mongolia-Manchuria and Baikal-Sayan belts. This was followed by gradual prevalence of suprasubduction high T/P metamorphism towards the late Paleozoic corresponding to the Altai and South Altai cycles. In the Tarim-North China Collage, metamorphic P-T and timing reveal a two-stage evolution, from dominant intermediate T/P metamorphism possibly resulting from Ordovician-Devonian amalgamation and Andean-type evolution of the collage, to dual low and high T/P metamorphism in the Carboniferous-Permian reflecting subduction-collision processes along the South Tianshan suture in the west and a suprasubduction evolution along the Solonker suture in the east. Altogether, the Paleozoic tectonometamorphic evolution of the two collages in the Central Asian Orogenic Belt shows remarkable differences, with the Mongolian Collage displaying features typical of peripheral accretionary style reflecting recurrent tectonic switches that can be regarded as a single orogenic system, and a two-stage evolution of the Tarim-North China Collage with features of both peripheral-accretionary and interior-collisional orogenic cycles, but mostly related to recurrent subductions of interior oceans.
Czech name
—
Czech description
—
Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
—
OECD FORD branch
10505 - Geology
Result continuities
Project
<a href="/en/project/GX19-27682X" target="_blank" >GX19-27682X: Principal mechanisms of peripheral continental growth during supercontinent cycle</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2025
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Journal of the Geological Society
ISSN
0016-7649
e-ISSN
2041-479X
Volume of the periodical
182
Issue of the periodical within the volume
2
Country of publishing house
GB - UNITED KINGDOM
Number of pages
12
Pages from-to
nestránkováno
UT code for WoS article
001364136300001
EID of the result in the Scopus database
2-s2.0-85212582688