张广才岭地块早-中二叠世镁铁质侵入岩体的年代学、地球化学及岩石成因

冯光英; 刘燊; 牛晓露; 杨经绥

doi:10.3799/dqkx.2018.721

Volume 43 Issue 4

Apr. 2018

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Article Navigation > Earth Science > 2018 > 43(4): 1293-1306

Feng Guangying, Liu Shen, Niu Xiaolu, Yang Jingsui, 2018. Geochronology, Geochemistry and Petrogenesis of Early-Middle Permian Mafic Intrusion in Zhangguangcai Range, China. Earth Science, 43(4): 1293-1306. doi: 10.3799/dqkx.2018.721

Citation:

Feng Guangying, Liu Shen, Niu Xiaolu, Yang Jingsui, 2018. Geochronology, Geochemistry and Petrogenesis of Early-Middle Permian Mafic Intrusion in Zhangguangcai Range, China. Earth Science, 43(4): 1293-1306. doi: 10.3799/dqkx.2018.721

Citation:

Feng Guangying, Liu Shen, Niu Xiaolu, Yang Jingsui, 2018. Geochronology, Geochemistry and Petrogenesis of Early-Middle Permian Mafic Intrusion in Zhangguangcai Range, China. Earth Science, 43(4): 1293-1306. doi: 10.3799/dqkx.2018.721

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Geochronology, Geochemistry and Petrogenesis of Early-Middle Permian Mafic Intrusion in Zhangguangcai Range, China

doi: 10.3799/dqkx.2018.721

1.
Center for Advanced Research on Mantle(CARMA), Key Laboratory of Deep-Earth Dynamics of Ministry of Land and Resources, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2.
State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China

Received Date: 2017-12-20
Publish Date: 2018-04-15

Abstract

Abstract

The Shuangfengshan mafic intrusion crops out in the southern margin of the Songnen-Zhangguangcai range. It is predominantly made of olivine gabbro, which yielded a crystallization age of 279±4 Ma (Early-Middle Permian). These rocks consist mainly of olivine, pyroxene, high-An (80.1-87.9) plagioclase and hornblende as reaction rim. The features of these minerals indicate a high-H₂O or water-saturated parental magma which experienced fluid metasomatism in the mantle source. Major and trace elements studies suggest that the mafic magma was derived from partial melting (~20%) of depleted garnet-lherzolite mantle source. Variable degrees of plagioclase accumulation and orthopyroxene crystal fractionation occurred in the process of magma evolution. They are also characterized by relatively low Sr isotopic ratio (0.705 2-0.706 1), positive ε_Nd(t) (0.9-1.3) and ε_Hf(t) (0-10.2) values, confirming that the Shuangfengshan mafic magma was derived from depleted mantle source and apparent crustal contamination was not found during magma upwelling. Combining trace elemental and isotopic results suggest that the parental magmas were likely derived from mantle wedge metasomatized by sedimentary melt and fluid from the subducted Paleo-Asian slab. Moreover, these rocks display transitional properties of MORB and arc basalt, conforming that the studied olivine gabbros were probably formed in back-arc extensional environment. And the mantle heterogeneity beneath the studied area was probably reduced by the multi-stage Paleozoic subduction of the Paleo-Asian Ocean.
- Early-Middle Permian,
- Songnen-Zhangguangcai range,
- mafic intrusion,
- petrogenesis,
- geochemistry

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References(85)

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