柴北缘西段晚古生代牛鼻子梁高镁闪长岩成因机制及地球动力学过程

钱兵; 张照伟; 吕鹏瑞; 王亚磊

doi:10.3799/dqkx.2018.176

Volume 43 Issue 12

Dec. 2018

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Article Navigation > Earth Science > 2018 > 43(12): 4375-4389

Qian Bing, Zhang Zhaowei, Lü Pengrui, Wang Yalei, 2018. Petrogenesis and Geodynamics Processes of Early Paleozoic Niubiziliang High-Mg Diorites in West Segment of North Qaidam, Qinghai. Earth Science, 43(12): 4375-4389. doi: 10.3799/dqkx.2018.176

Citation:

Qian Bing, Zhang Zhaowei, Lü Pengrui, Wang Yalei, 2018. Petrogenesis and Geodynamics Processes of Early Paleozoic Niubiziliang High-Mg Diorites in West Segment of North Qaidam, Qinghai. Earth Science, 43(12): 4375-4389. doi: 10.3799/dqkx.2018.176

Citation:

Qian Bing, Zhang Zhaowei, Lü Pengrui, Wang Yalei, 2018. Petrogenesis and Geodynamics Processes of Early Paleozoic Niubiziliang High-Mg Diorites in West Segment of North Qaidam, Qinghai. Earth Science, 43(12): 4375-4389. doi: 10.3799/dqkx.2018.176

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Petrogenesis and Geodynamics Processes of Early Paleozoic Niubiziliang High-Mg Diorites in West Segment of North Qaidam, Qinghai

doi: 10.3799/dqkx.2018.176

Qian Bing^{1,2
,},
Zhang Zhaowei^1,2,
Lü Pengrui^1,2,
Wang Yalei^1,2

1.
Key Laboratory for the Study of Focused Magmatism and Giant Ore Deposits, Ministry of Natural Resources, Xi'an 710054, China
2.
Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China

Received Date: 2018-03-20
Publish Date: 2018-12-15

Abstract

Abstract

The high-Mg diorites, newly discovered in Niubiziliang area, are important for discussing the evolution history of lithospheric mantle in North Qaidam, Qinghai Province. To determine the petrogenesis and geodynamic processes of these rocks, the major and trace element analysis, zircon U-Pb dating and Hf isotopic analysis have been carried out in this paper. The petrogeochemistry shows that the rocks are calc-alkaline rocks, and enriched in Mg (Mg^#=62-72), Cr, Ni and LREE (LREE/HREE=2.84-4.61) elements, with low FeO^T/MgO (0.70-1.12) ratios.They belong to high-magnesium diorite. All the rocks are enriched in large iron lithiphile elements (Rb, Ba, Th, U, K and LREE) and depleted in high strength field elements (Nb, Ta, Ti, P and HREE).Additionally, the diorite rocks have the same characteristics of geochemistry as typical sanukitoids. The mean U-Pb age of the zircons in these high-Mg diorites is 388 Ma, suggesting that the rocks were formed in Middle Triassic. The zircon Hf isotopes show that all the ε_Hf(t)(4.4-11.6) are positive, indicating the magma was originated from the depleted mantle.Combined with the regional tectonic evolution process, it is suggested that the mantle source of the Niubiziliang high-Mg diorite was formed by the reaction of the slab-derived fluids with the overlying mantle peridotite in Early Paleozoic (540-520 Ma). In Late Paleozoic (400-388 Ma), partial melting of the enriched mantle might generate the studied high-Mg diorites due to lithospheric extension.
- high-Mg diorite,
- petrogenesis,
- lithospheric mantle,
- Niubiziliang area,
- north Qaidam orogenic belt,
- geochemistry

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References(99)

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Petrogenesis and Geodynamics Processes of Early Paleozoic Niubiziliang High-Mg Diorites in West Segment of North Qaidam, Qinghai

doi: 10.3799/dqkx.2018.176

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