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- W2393879382 abstract "SHRIMP U-Pb dating of zircons from biotite granite of the Sidingheishan super-unit on the eastern margin of the Tuha basin yields an apparent 206Pb/238U age of 386±5 Ma (MSWD=1.01). According to the petrological characteristics and related zircon CL images, this age is explained as the intrusion age of the granite. According to this dating result and similar metamorphism and deformation of the granite to those of its county rocks (which are classified by local geologists as the Paleoproterozoic Xingxingxia Group), combined with the available chronological, geochemical and related geological data, the authors come to the following preliminary conclusions: ① the eastern and southern margins of the Tuha basin are different parts of the same Paleozoic active continental margin, whose formation and evolution is related to the subduction of the paleo-oceanic lithospheric plate, represented by fragments of oceanic crust in the Kanggurtag collisional belt, northward under the Siberian paleoplate, and ② the event of deformation and metamorphism on the eastern margin of the basin, which is characterized by nearly E-W-trending and steeply south-dipping schistosity or gneissosity, took place later than 386 Ma." @default.
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- W2393879382 date "2006-01-01" @default.
- W2393879382 modified "2023-09-28" @default.
- W2393879382 title "Devonian granite on the eastern margin of the Tuha basin in the East Tianshan, Xinjiang, China and its tectonic implication" @default.
- W2393879382 hasPublicationYear "2006" @default.
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