4.7 Article

Geochronology and geochemistry of gneiss and migmatite from the Korla Complex in the Quruqtagh block, NW China: Implications for Proterozoic crustal evolution of the northeastern Tarim Craton

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Late Paleoproterozoic orogenic evolution of the northern Tarim Craton, NW China: Insights from phase equilibrium modeling and zircon U-Pb geochronology of metapelitic granulite in the Kuluketage area

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Summary: The global paleoproterozoic orogenic evolution plays an important role in understanding the assembly of the Columbia supercontinent. This study focuses on the northern Tarim region and reveals a paleoproterozoic tectono-thermal event related to the Columbia supercontinent assembly. However, the limited metamorphic investigations hindered the recognition of paleoproterozoic orogenic evolution in the northern Tarim, impacting the understanding of the relationship between Tarim Craton and the Columbia supercontinent. The study conducted petrography, zircon U-Pb geochronology, and phase equilibria modeling to analyze metapelitic granulite samples from the Xingditage Group. The results provide insights into the paleoproterozoic orogenic evolution in the northern Tarim Craton and propose a tectonic evolution scenario involving a collision with an unknown block prior to approximately 1.85 Ga.

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