湘桂边界越城岭岩基北部印支期花岗岩锆石U-Pb年代学和地球化学特征

程顺波; 付建明; 崔森; 卢友月; 马丽艳; 刘阿睢

doi:10.3799/dqkx.2018.178

Volume 43 Issue 7

Jul. 2018

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Article Navigation > Earth Science > 2018 > 43(7): 2330-2349

Cheng Shunbo, Fu Jianming, Cui Sen, Lu Youyue, Ma Liyan, Liu A'sui, 2018. Zircon U-Pb Chronology, Geochemistry of the Indonesian Granitic Rocks from Northern Yuechengling Batholith in Guangxi-Hunan Junction. Earth Science, 43(7): 2330-2349. doi: 10.3799/dqkx.2018.178

Citation:

Cheng Shunbo, Fu Jianming, Cui Sen, Lu Youyue, Ma Liyan, Liu A'sui, 2018. Zircon U-Pb Chronology, Geochemistry of the Indonesian Granitic Rocks from Northern Yuechengling Batholith in Guangxi-Hunan Junction. Earth Science, 43(7): 2330-2349. doi: 10.3799/dqkx.2018.178

Citation:

Cheng Shunbo, Fu Jianming, Cui Sen, Lu Youyue, Ma Liyan, Liu A'sui, 2018. Zircon U-Pb Chronology, Geochemistry of the Indonesian Granitic Rocks from Northern Yuechengling Batholith in Guangxi-Hunan Junction. Earth Science, 43(7): 2330-2349. doi: 10.3799/dqkx.2018.178

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Zircon U-Pb Chronology, Geochemistry of the Indonesian Granitic Rocks from Northern Yuechengling Batholith in Guangxi-Hunan Junction

doi: 10.3799/dqkx.2018.178

Cheng Shunbo^{1,2
,},
Fu Jianming^1,2,
Cui Sen^{1,2
,
,},
Lu Youyue^1,2,
Ma Liyan^1,2,
Liu A'sui^1,2

1.
Wuhan Center of Chinese Geological Survey, Wuhan 430205, China
2.
Research Center of Granitic Diagenesis and Mineralization, Chinese Geological Survey, Wuhan 430205, China

Received Date: 2018-03-15
Publish Date: 2018-07-15

Abstract

Abstract

The temporal and spatial distribution of Indonesian granitoid in northern Yuechengling batholith is still uncertained. In this paper, a compilation of petrology, zircon U-Pb chronology, geochemistry and Nd-Hf isotopes was used on the granitoid to solve this uncertainty. The result shows Indonesian granitoid spreads in north area of the border with the age of 236-222 Ma, and mainly consists of medium to fine grained tourmaline-bearing monzogranites, with accessory minerals assemblage of zircon, zoisite (and/or clinozoisite), apatite and garnet. The granitic samples have characteristics of high SiO₂, alkaline, low CaO, MgO, P₂O₅ contents, and weak to strong peraluminous (A/CNK=1.07-1.17), with enrichment of Rb, Th, U and strong depletion of Ba, Sr, Eu, Nb, Ti elements. Source of early stage of Indonesian granitic rocks mainly consisting of metagreywackes, with small amount of new crustal component. Those of late stage are inhomogeneous mixing of metagreywackes and metapelites. Granitic rocks of both stage have stable high negative ε_Nd(t)(-9.3——10.6) and ε_Hf(t) (-5.4——11.9) ratios with source's average crustal residence age of ca 1.8 Ga. Integrated with Indonesian tectonic involvement of South China, formation of granitic magma is perhaps due to dehydration melting of mica-riched metasediments during post-orogenic thickened crust environment, migration and emplacement of the magma is controlled by relaxation of deep fault adjacent to the batholith.
- zircon U-Pb chronology,
- geochemistry,
- Nd-Hf isotope,
- Indosinian,
- Guangxi-Hunan junction

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References(121)

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Zircon U-Pb Chronology, Geochemistry of the Indonesian Granitic Rocks from Northern Yuechengling Batholith in Guangxi-Hunan Junction

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