Citation: | CHEN Yuke. Chronology and geochemistry of the granitoids in Heri Town, Tongde County, Qinghai Province, and its tectonic significance[J]. Geological Bulletin of China, 2020, 39(7): 1015-1024. |
In this study, the author used LA-ICP-MS zircon U-Pb isotopic dating method and obtained weighted average zircon U-Pb age of 229.7±1.0 Ma from the biotite granodiorite in Heri Town, Tongde County, Qinghai Province.The geochemical characteristics show that it belongs to high-K calcium-alkali series, and resulted from partial melting of crustal components, with weak negative Eu anomalies and right-inclined chondrite-normalized REE patterns.Based on a comprehensive analysis of previous researched, the authors hold that the biotite granodiorite was formed in the Late Triassic, and belonged to I-type granite formed in the active continental margin environment before the plane collision.Its genesis was closely related to the northward subduction of the Ańyemagen-Mianlue Ocean.The results obtained by the authors provide a new age constraint for the entrance of West Qinling into the syn-collision stage in the Indosinian.
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① | 陕西地矿区研院有限公司.青海省同德县谷芒地区五幅1:5万区域地质矿产调查.2014. |
Tectonic location(a)and simplified geological map(b) of the study area
Outcrop and microscopic photos of Heri biotite granodiorite
CL images of zircons from the biotite granodiorite
Zircon age frequency histogram of biotite granodiorite
Zircon LA-ICP-MS U-Pb concordia diagram (a) and weighted mean206Pb/238U age (b) of biotite granodiorite
SiO2-(K2O+Na2O)(a) and SiO2-K2O(b) plots
Primitive mantle-normalized trace element spider diagrams (a) and chondrite-normalized REE patterns (b)
Discrimination diagrams of genetic type and tectonic environment