大兴安岭多宝山晚三叠世双峰式侵入岩年代学及地球动力学背景

刘宝山; 程招勋; 钱程; 张春鹏; 钟辉; 韩仁萍

doi:10.3799/dqkx.2020.214

Volume 46 Issue 7

Jul. 2021

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Article Navigation > Earth Science > 2021 > 46(7): 2311-2328

Liu Baoshan, Cheng Zhaoxun, Qian Cheng, Zhang Chunpeng, Zhong Hui, Han Renping, 2021. Geochronology and Geodynamic Background Study of the Late Triassic Bimodal Pattern Intrusive Rock in Da Hinggan Mountains Duobaoshan Area. Earth Science, 46(7): 2311-2328. doi: 10.3799/dqkx.2020.214

Citation:

Liu Baoshan, Cheng Zhaoxun, Qian Cheng, Zhang Chunpeng, Zhong Hui, Han Renping, 2021. Geochronology and Geodynamic Background Study of the Late Triassic Bimodal Pattern Intrusive Rock in Da Hinggan Mountains Duobaoshan Area. Earth Science, 46(7): 2311-2328. doi: 10.3799/dqkx.2020.214

Citation:

Liu Baoshan, Cheng Zhaoxun, Qian Cheng, Zhang Chunpeng, Zhong Hui, Han Renping, 2021. Geochronology and Geodynamic Background Study of the Late Triassic Bimodal Pattern Intrusive Rock in Da Hinggan Mountains Duobaoshan Area. Earth Science, 46(7): 2311-2328. doi: 10.3799/dqkx.2020.214

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Geochronology and Geodynamic Background Study of the Late Triassic Bimodal Pattern Intrusive Rock in Da Hinggan Mountains Duobaoshan Area

doi: 10.3799/dqkx.2020.214

1.
Shenyang Geological Survey Center, China Geological Survey, Shenyang 110034, China
2.
Heilongjiang Institute of Natural Resources, Harbin 150036, China

Received Date: 2020-07-20
Publish Date: 2021-07-15

Abstract

Abstract

Hornblende gabbro and tonalite which emplaced in Late Ordovician granodiorite were found in Duobaoshan mining area, possessed the characteristics of bimodal pattern intrusive rock.On the basis of detailed field geological survey, we reaserched the petrology, geochronology and geochemistry characteristics of bimodal pattern intrusive rock, and discuss their tectonic significance. The LA-ICP-MS zircon U-Pb ages of hornblende gabbro is 224.3±1.7 Ma, the LA-ICP-MS zircon U-Pb ages of tonalite is 226.3±2.3 Ma, they were both formed by the same tectonic magmatism.The SiO₂ content of intrusive rock is bimodal, their rare earth elements and microelements indicates the characteristics of island arc magma.They have the same mantle source, which influenced by the subduction metasomatic alteration of fluids. Based on analysis of the regional tectonic background, its formation is related to the Okhotsk subduction. The gabbro and tonalite which formed in the active continental margin environment, were interpreted to be formed through assimilation of OIB-type basaltic magma followed by fractional crystallization in a.double diffusive'magma chamber at the middle crust level.
- bimodal invasion rock,
- Late Triassic,
- island arc,
- Da Hinggan,
- Duobaoshan,
- tectonics

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Geochronology and Geodynamic Background Study of the Late Triassic Bimodal Pattern Intrusive Rock in Da Hinggan Mountains Duobaoshan Area

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