塔里木地块东南缘新太古代安南坝石英闪长片麻岩的成因及其对地壳演化的启示

辜平阳; 计文化; 陈锐明; 庄玉军; 彭璇; 查显锋; 郭亚鹏

doi:10.3799/dqkx.2020.140

Volume 45 Issue 9

Sep. 2020

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Article Navigation > Earth Science > 2020 > 45(9): 3268-3281

Gu Pingyang, Ji Wenhua, Chen Ruiming, Zhuang Yujun, Peng Xuan, Zha Xianfeng, Guo Yapeng, 2020. Petrogenesis of Neoarchean Ananba Quartz Diorite Gneiss in Southeastern Margin of Tarim: Implications for Crustal Evolution. Earth Science, 45(9): 3268-3281. doi: 10.3799/dqkx.2020.140

Citation:

Gu Pingyang, Ji Wenhua, Chen Ruiming, Zhuang Yujun, Peng Xuan, Zha Xianfeng, Guo Yapeng, 2020. Petrogenesis of Neoarchean Ananba Quartz Diorite Gneiss in Southeastern Margin of Tarim: Implications for Crustal Evolution. Earth Science, 45(9): 3268-3281. doi: 10.3799/dqkx.2020.140

Citation:

Gu Pingyang, Ji Wenhua, Chen Ruiming, Zhuang Yujun, Peng Xuan, Zha Xianfeng, Guo Yapeng, 2020. Petrogenesis of Neoarchean Ananba Quartz Diorite Gneiss in Southeastern Margin of Tarim: Implications for Crustal Evolution. Earth Science, 45(9): 3268-3281. doi: 10.3799/dqkx.2020.140

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Petrogenesis of Neoarchean Ananba Quartz Diorite Gneiss in Southeastern Margin of Tarim: Implications for Crustal Evolution

doi: 10.3799/dqkx.2020.140

Gu Pingyang^{1, 2
,
,},
Ji Wenhua^{1, 2},
Chen Ruiming^{1, 2},
Zhuang Yujun^{1, 2},
Peng Xuan^{1, 2},
Zha Xianfeng^{1, 2},
Guo Yapeng^{1, 2}

1.
Center for Orogenic Belt Geology, CGS, Xi'an Geological Survey Center, Xi'an 710054, China
2.
Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, MNR, Xi'an Geological Survey Center, Xi'an 710054, China

Received Date: 2020-03-31
Publish Date: 2020-09-15

Abstract

Abstract

The study on the formation age and petrogenetic mechanism of early Precambrian rocks in the southeast margin of Tarim block is relatively weak, which restricts the understanding of the formation and early evolution of continental crust. These geochemistry and zircon Hf isotope compositions show that primary magma of the quartz diorite gneiss was formed by partial melting of the lower crust meta-basalt with minor addition of mantle-derived materials. LA-ICP-MS zircon U-Pb dating results reveal that the diagenetic ages of the quartz diorite gneiss are 2 662±12 Ma and 2 676±15 Ma, indicating the Archean rock formation ages in the southeastern margin of Tarim were mainly concentrated in 2.55－2.70 Ga; corresponding metamorphic ages are 1 980±30 Ma and 1 828±20 Ma－2 087±29 Ma respectively, representing the geological record of magmatic-matamorphic events related to orogenic processes in the middle and late period of Paleoproterozoic in the southeastern margin of Tarim. Additionally, two-stage model ages(T_DM2)of zircon for the quartz diorite gneiss in this study vary from 2 954 to 3 742 Ma, with peak ages clustering at ~3.24 Ga. Thus, combined with the available data, it is suggested that the ~3.2 Ga age represents the main period of continental crustal growth in the southeastern margin of Tarim, and subsequently crustal reconstruction occurred in 2.55－2.70 Ga. It is concluded that ancient crustal material recycling could be an important way of continental crustal evolution in the middle and late period of Neoarchean in this area.
- quartz diorite gneiss,
- petrology,
- geochemistry,
- zircon U-Pb age,
- Hf isotope,
- southeastern margin of Tarim

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References(70)

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