河北围场朝阳地中泥盆世高Sr/Y花岗岩成因及对兴蒙造山带演化的约束

王树庆; 胡晓佳; 赵华雷; 刘文刚; 杨泽黎

doi:10.3799/dqkx.2018.350

Volume 44 Issue 1

Jan. 2019

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Wang Shuqing, Hu Xiaojia, Zhao Hualei, Liu Wengang, Yang Zeli, 2019. Petrogenesis of Middle Devonian Chaoyangdi High Sr/Y Granite and Constraints on the Evolution of Xing-Meng Orogeny. Earth Science, 44(1): 145-160. doi: 10.3799/dqkx.2018.350

Citation:

Wang Shuqing, Hu Xiaojia, Zhao Hualei, Liu Wengang, Yang Zeli, 2019. Petrogenesis of Middle Devonian Chaoyangdi High Sr/Y Granite and Constraints on the Evolution of Xing-Meng Orogeny. Earth Science, 44(1): 145-160. doi: 10.3799/dqkx.2018.350

Citation:

Wang Shuqing, Hu Xiaojia, Zhao Hualei, Liu Wengang, Yang Zeli, 2019. Petrogenesis of Middle Devonian Chaoyangdi High Sr/Y Granite and Constraints on the Evolution of Xing-Meng Orogeny. Earth Science, 44(1): 145-160. doi: 10.3799/dqkx.2018.350

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Petrogenesis of Middle Devonian Chaoyangdi High Sr/Y Granite and Constraints on the Evolution of Xing-Meng Orogeny

doi: 10.3799/dqkx.2018.350

Tianjin Center of China Geological Survey, Tianjin 300170, China

Received Date: 2018-07-06
Publish Date: 2019-01-15

Abstract

Abstract

Xing-Meng orogeny is the accretionary orogeny between Siberia and North China plates with complex multi-stage subduction and accretion, and its tectonic evolution. has remained controversial for a long time. To reveal the arc-continent collision in the end of Early Paleozoic, this paper presents a study on Chaoyangdi Middle Devonian high Sr/Y granite in southern part of Xing-Meng orogeny zircon U-Pb dating results yield a formation age of 386.8±2.9 Ma, with the corresponding age of Middle Devonian (D2). Geochemical data shows that these rocks have high SiO₂, Al₂O₃ and Na₂O, moderate CaO and K₂O, but low FeO_t and MgO contents with the Na₂O/K₂O>1 and calc-alkaline series signature. The A/CNK ratios range from 1.02 to 1.08, indicating these samples are weak peraluminous series. Trace element analysis results display enrichment of LILEs, such as Rb, Ba, K and Sr, but depletion of HFSE, i.e., Nb, Ta, P and Ti, with high Sr/Y ratios (103-146), similar with adakitic-affinity. These rocks have strong fractionation between LREE and HREE ((La/Yb)_N=9.9-14.6), no obvious HREE fractionation ((Gd/Yb)_N=1.45-1.97) and weak positive Eu anomalies (δEu=1.31-1.80). All these geochemical characteristics suggest that high Sr/Y signature is inherited from magma source. Sr-Nd-Hf analyses show enriched isotopic signatures-both ε_Hf(t) and ε_Nd(t) are negative(-38.30 to -23.59 and -18.6 to -17.9) with old two-stage model age (2 825 to 3 745 Ma for Hf, 2 584 to 2 642 Ma for Nd), indicating an old enriched crustal source. Based on petrology, geochemistry and Hf-Sr-Nd isotopic characteristics, we conclude that the Chaoyangdi Middle Devonian intrusive rocks were formed by partial melting of ancient basic lower crust with high Sr/Y ratios and formed by post-collisional extension and heating of asthenosphere upwelling, indicating the regional extension after collision between the Bainaimiao arc and the North China Block.
- Middle Devonian,
- high Sr/Y granite,
- arc-continent collision,
- lower continental crust source,
- northern part of North China Craton,
- Xing-Meng orogeny,
- geochemistry

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References(106)

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Petrogenesis of Middle Devonian Chaoyangdi High Sr/Y Granite and Constraints on the Evolution of Xing-Meng Orogeny

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