东昆仑中泥盆世A型花岗岩的确定及其构造意义

刘彬; 马昌前; 郭盼; 张金阳; 熊富浩; 黄坚; 蒋红安

doi:10.3799/dqkx.2013.093

Volume 38 Issue 5

Sep. 2013

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Article Navigation > Earth Science > 2013 > 38(5): 947-962

LIU Bin, MA Chang-qian, GUO Pan, ZHANG Jin-yang, XIONG Fu-hao, HUANG Jian, JIANG Hong-an, 2013. Discovery of the Middle Devonian A-type Granite from the Eastern Kunlun Orogen and Its Tectonic Implications. Earth Science, 38(5): 947-962. doi: 10.3799/dqkx.2013.093

Citation:

LIU Bin, MA Chang-qian, GUO Pan, ZHANG Jin-yang, XIONG Fu-hao, HUANG Jian, JIANG Hong-an, 2013. Discovery of the Middle Devonian A-type Granite from the Eastern Kunlun Orogen and Its Tectonic Implications. Earth Science, 38(5): 947-962. doi: 10.3799/dqkx.2013.093

Citation:

LIU Bin, MA Chang-qian, GUO Pan, ZHANG Jin-yang, XIONG Fu-hao, HUANG Jian, JIANG Hong-an, 2013. Discovery of the Middle Devonian A-type Granite from the Eastern Kunlun Orogen and Its Tectonic Implications. Earth Science, 38(5): 947-962. doi: 10.3799/dqkx.2013.093

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Discovery of the Middle Devonian A-type Granite from the Eastern Kunlun Orogen and Its Tectonic Implications

doi: 10.3799/dqkx.2013.093

LIU Bin^{1, 2
,},
MA Chang-qian^{1, 2
,
,},
GUO Pan²,
ZHANG Jin-yang³,
XIONG Fu-hao^{1, 2},
HUANG Jian²,
JIANG Hong-an²

1.
State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China
2.
Faulty of Earth Sciences, China University of Geosciences, Wuhan 430074, China
3.
Faulty of Earth Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2012-08-14
Publish Date: 2013-09-15

Abstract

Abstract

Middle Devonian Binggou granites from the eastern Kunlun orogen, are characterized by relatively high silicon (SiO₂=71.85%-72.77%), total alkali (K₂O+Na₂O=8.39-8.58), aluminum(A/CNK=0.93-1.03), FeO_t/MgO (6.24-7.86) and 10⁴Ga/Al values (3.04-3.60), high LREE, obvious negative Eu anomalies, and notable enrichment of HFSE (Zr, Ga, Y, Hf, etc.), strong depletion of Ba, Sr, P and Ti relative to the primitive mantle, similar to the geochemical features of A-type granites. The LA-ICP-MS Zircon U-Pb analyses yield a weighted mean ²⁰⁶Pb/²³⁸U age of 391±3 Ma (MSWD=2.36), considered to be the formation age of the Binggou granites. With a comprehensive consideration on many different indexes, such as whole rock Sr-Nd isotopes, geochemistry, experimental petrology and so on, we conclude that the Binggou granites formed by partial melting of crust materials (meta-greywacke) on the conditions of low pressure and high temperature at the stage of postorogenic stretch. The Binggou granites are younger than the other Paleozoic A-type granites reported in the eastern Kunlun orogen, suggesting the ending proto-tethys and the beginning paleo-tethys.
- A-type,
- granite,
- postorogenic,
- Middle Devonian,
- eastern Kunlun orogen,
- tectonics,
- petrology

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References(96)

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