黑龙江黑河地区早侏罗世岩浆弧的火成岩记录及其成因

刘继旭; 刘翠; 邓晋福; 罗照华; 张昱; 贺国奇; 刘庆; 岳洪举

doi:10.3799/dqkx.2020.057

Volume 45 Issue 7

Jul. 2020

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Article Navigation > Earth Science > 2020 > 45(7): 2538-2554

Liu Jixu, Liu Cui, Deng Jinfu, Luo Zhaohua, Zhang Yu, He Guoqi, Liu Qing, Yue Hongju, 2020. Igneous Rock Records and Genesis of the Early Jurassic Magmatic Arc in Heihe Area of Heilongjiang Province. Earth Science, 45(7): 2538-2554. doi: 10.3799/dqkx.2020.057

Citation:

Liu Jixu, Liu Cui, Deng Jinfu, Luo Zhaohua, Zhang Yu, He Guoqi, Liu Qing, Yue Hongju, 2020. Igneous Rock Records and Genesis of the Early Jurassic Magmatic Arc in Heihe Area of Heilongjiang Province. Earth Science, 45(7): 2538-2554. doi: 10.3799/dqkx.2020.057

Citation:

Liu Jixu, Liu Cui, Deng Jinfu, Luo Zhaohua, Zhang Yu, He Guoqi, Liu Qing, Yue Hongju, 2020. Igneous Rock Records and Genesis of the Early Jurassic Magmatic Arc in Heihe Area of Heilongjiang Province. Earth Science, 45(7): 2538-2554. doi: 10.3799/dqkx.2020.057

PDF( 9573 KB)

Igneous Rock Records and Genesis of the Early Jurassic Magmatic Arc in Heihe Area of Heilongjiang Province

doi: 10.3799/dqkx.2020.057

Liu Jixu^{1
,
,},
Liu Cui^{1
,
,
,},
Deng Jinfu¹,
Luo Zhaohua¹,
Zhang Yu²,
He Guoqi¹,
Liu Qing¹,
Yue Hongju³

1.
School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China
2.
Bureau of Geology and Mineral Resoures of Heilongjiang Province, Harbin 150036, China
3.
701 Team of Heilongjiang Nonferrous Metal Geological Exploration, Harbin 150028, China

Received Date: 2020-03-22
Publish Date: 2020-07-15

Abstract

Abstract

Mesozoic igneous rocks are widely developed in Heihe area, but the age of formation, igneous rock assemblages at different stages, petrogenesis, and the geotectonic background of the formation are still controversial. This article conducts detailed field, petrology, geochemistry, and chronology studies on intrusive rocks around the Woniu Lake in Heihe area to reveal the age and genesis of the rocks. LA-ICP-MS zircon dating of diorite and monzogranite shows that they formed at 175.53±0.53 Ma and 177.25±0.45 Ma.Igneous rocks in this area during this period were mainly intrusive rocks and some dike rocks, intrusive rocks are mainly granite, granodiorite, and a small amount of monzonite, dike rocks are mainly granitic dikes and dioritic dikes.Plutonic facies rocks were T₁T₂G₁G₂ rock assemblage contained some Tonalite(T₁)-Trondhjemite(T₂) rocks and more Granodiorite(G₁)-Granite(G₂) rocks.The rock assemblage were mainly subalkaline series on SiO₂-(Na₂O+K₂O) diagram and on SiO₂-K₂O diagram were mainly high-potassium calcium-alkali series, were calcium alkali or alkali calcium series on SiO₂-(Na₂O+K₂O-CaO)diagram.They were metaluminums-peraluminous series rocks. Most of the rocks in SiO₂-MgO diagram were similar to magnesium andesite(MA) series.Trace elements spider diagrams were generally enriched in LILE, such as Rb, K, Pb, depleted in Nb, Ta, La, Ce, Ti. The REE patterns were right-inclined, LREE were steeper and HREE were gentler. The rock assemblages and their characteristics all indicated the characteristics of island arc magmatic rocks. Based on the discrimination of the tectonic environment, it is considered that the rock assemblages were formed in the environment related to ocean subduction. Magma may have formed in the local melting of the subducting basaltic crust reacted with the overlying mantle wedge and the local melting of the crust under the Xing'an arc.It is considered to be related to the evolution of the northern Mongolia-Okhotsk Ocean.
- Woniu Lake in Heihe area,
- ocean subduction,
- magmatic arc,
- T₁T₂G₁G₂ rock assemblage,
- chronology

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