内蒙古拜仁达坝石炭纪岩体年代学、地球化学、Sr-Nd同位素特征及其对中亚造山带的制约

张艳飞; 周永恒; 董洋; 李琛; 王刚

doi:10.3799/dqkx.2021.059

Volume 47 Issue 4

Apr. 2022

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Zhang Yanfei, Zhou Yongheng, Dong Yang, Li Chen, Wang Gang, 2022. Geochronological, Geochemical and Sr-Nd Isotopic Characteristics of Carboniferous Rock Mass in Bayern Daba Area, Inner Mongolia and Its Constraints on Central Asian Orogenic Belt. Earth Science, 47(4): 1234-1252. doi: 10.3799/dqkx.2021.059

Citation:

Zhang Yanfei, Zhou Yongheng, Dong Yang, Li Chen, Wang Gang, 2022. Geochronological, Geochemical and Sr-Nd Isotopic Characteristics of Carboniferous Rock Mass in Bayern Daba Area, Inner Mongolia and Its Constraints on Central Asian Orogenic Belt. Earth Science, 47(4): 1234-1252. doi: 10.3799/dqkx.2021.059

Citation:

Zhang Yanfei, Zhou Yongheng, Dong Yang, Li Chen, Wang Gang, 2022. Geochronological, Geochemical and Sr-Nd Isotopic Characteristics of Carboniferous Rock Mass in Bayern Daba Area, Inner Mongolia and Its Constraints on Central Asian Orogenic Belt. Earth Science, 47(4): 1234-1252. doi: 10.3799/dqkx.2021.059

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Geochronological, Geochemical and Sr-Nd Isotopic Characteristics of Carboniferous Rock Mass in Bayern Daba Area, Inner Mongolia and Its Constraints on Central Asian Orogenic Belt

doi: 10.3799/dqkx.2021.059

Zhang Yanfei^{1
,
,},
Zhou Yongheng¹,
Dong Yang^{2
,
,},
Li Chen³,
Wang Gang³

1.
Shenyang Center of China Geological Survey, Shenyang 110034, China
2.
Liaoning Geological and Mineral Survey Institute Company Limited, Shenyang 110034, China
3.
Liaoning Chemical Geological Survey Institute Company Limited, Jinzhou 121000, China

Received Date: 2021-01-15
Available Online: 2022-04-29
Publish Date: 2022-04-25

Abstract

Abstract

In order to examine the magma origin and tectonic setting of the Bayern Daba rock mass in Inner Mongolia and thereby limit the closure of the paleo-Asian Ocean, zircon LA-ICP-MS U-Pb geochronological, geochemical and Sr-Nd isotopic measurement and analysis are presented in this paper. Zircon U-Pb dating yields a weighted mean age of 327±2 Ma(MSWD=1.4), indicating an Early Carboniferous magmatic event. The Bayern Daba rock mass is characterized by the high Si, Na, Mg, Fe and metaluminous-peraluminous features. They are relatively enriched in Rb, Th, U and K, depleted in Ba, Sr, P, Nb, Ta and Ti, and enriched in LREE over HREE with negative Eu anormaly, showing the calc-alkaline Ⅰ-type granite in island arc. Their depleted isotopic compositions with (⁸⁷Sr/⁸⁶Sr)_i from 0.705 8 to 0.709 6, negative ε_Nd(t) values from -4.93 to 0.01, and T_DM2 from 1.08 to 1.48 Ga, as well as the inherited zircon present in zircon, indicating that the magma source was derived from the partial melting of Mesoproterozoic mantle-derived basic materials. High Rb/Sr (0.70-2.63) and Zr/Hf (35.88-77.17) ratios and the positive correlation of I_Sr and ε_Nd(t) isotopic data suggest contamination by a proportion of mantle material. Combined with regional tectonic evolution, the Bayern Daba rock mass was formed in the island-arc environment of an active continental margin in Carboniferous, which further suggests that the subduction of the paleo-Asian Ocean was still ongoing at that time. The same conclusion is also reported about the Early Permian intermediate-acidic rock masses in the southern part of the Xing-Meng orogenic belt, suggesting that the paleo-Asian Ocean had been subducting northward from Late Carboniferous up to Late Permian and did not fully close until the appearance of granitoids formed in a post-orogenic extensional environment in Middle to Late Triassic.
- Bayern Daba rock mass,
- Sr-Nd isotope,
- paleo-Asian Ocean,
- active continental margin,
- petrology

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References(135)

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Geochronological, Geochemical and Sr-Nd Isotopic Characteristics of Carboniferous Rock Mass in Bayern Daba Area, Inner Mongolia and Its Constraints on Central Asian Orogenic Belt

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