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- W2359487669 abstract "According to the index fossil of Late Devonian, the age of the epimetamorphic rocks on the southwestern margin of the Tarim Basin is interpreted as Late Devonian, contradictory to previous assertion that they are Proterozoic, Silurian—Middle Devonian, or Late Cambrian—Middle Ordovician in age. The lithological components, spatial distribution and regional geological features of these epimetamorphic rocks show that their protolith experienced low-temperature dynamic metamorphism soon after they were deposited. The metamorphism is related to the collisional orogeny of the North Kunlun Orogen during the Silurian—Devonain. The Upper Devonian epimetamorphic rocks provide new age constraint on the North Kunlun Collisional Orogeny." @default.
- W2359487669 created "2016-06-24" @default.
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- W2359487669 date "2007-01-01" @default.
- W2359487669 modified "2023-09-26" @default.
- W2359487669 title "AGE DETERMINATION AND ITS GEOLOGICAL SIGNIFICANCE OF THE EPIMETAMORPHIC ROCKS ON THE SOUTHWESTERN MARGIN OF THE TARIM BASIN" @default.
- W2359487669 hasPublicationYear "2007" @default.
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