桂中昆仑关A型花岗岩锆石U-Pb年代学与地球化学特征

刘飞; 李堃; 黄圭成; 邱啸飞; 严乐佳; 陆世才

doi:10.3799/dqkx.2018.180

Volume 43 Issue 7

Jul. 2018

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Article Navigation > Earth Science > 2018 > 43(7): 2313-2329

Liu Fei, Li Kun, Huang Guicheng, Qiu Xiaofei, Yan Lejia, Lu Shicai, 2018. Zircon U-Pb Geochronology and Geochemical Characteristics of the Kunlunguan A-Type Granite in Central Guangxi. Earth Science, 43(7): 2313-2329. doi: 10.3799/dqkx.2018.180

Citation:

Liu Fei, Li Kun, Huang Guicheng, Qiu Xiaofei, Yan Lejia, Lu Shicai, 2018. Zircon U-Pb Geochronology and Geochemical Characteristics of the Kunlunguan A-Type Granite in Central Guangxi. Earth Science, 43(7): 2313-2329. doi: 10.3799/dqkx.2018.180

Citation:

Liu Fei, Li Kun, Huang Guicheng, Qiu Xiaofei, Yan Lejia, Lu Shicai, 2018. Zircon U-Pb Geochronology and Geochemical Characteristics of the Kunlunguan A-Type Granite in Central Guangxi. Earth Science, 43(7): 2313-2329. doi: 10.3799/dqkx.2018.180

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Zircon U-Pb Geochronology and Geochemical Characteristics of the Kunlunguan A-Type Granite in Central Guangxi

doi: 10.3799/dqkx.2018.180

Liu Fei^{1,2
,},
Li Kun^{1,2
,
,},
Huang Guicheng^1,2,
Qiu Xiaofei^1,2,
Yan Lejia³,
Lu Shicai³

1.
Wuhan Center of China Geological Survey, Wuhan 430205, China
2.
Research Center of Granitic Diagenesis and Mineralization, China Geological Survey, Wuhan 430205, China
3.
Guangxi Geological Exploration Institute of China Metallurgical Geology Bureau, Nanning 530022, China

Received Date: 2018-03-14
Publish Date: 2018-07-15

Abstract

Abstract

For studying the Late Yanshan magmatism in South China hinterland, and analyzing its petrogenesis and tectonic significance, this paper carries out systematical geochronological, geochemical and Sm-Nd isotopic investigations on the Kunlunguan granitic pluton in central Guangxi. LA-ICP-MS zircon U-Pb dating yields a weighted mean ²⁰⁶Pb/²³⁸U age of 97.7±1.3 Ma (MSWD=1.6), implying its Late Yanshan intrusion time. Geochemical compositions show that it is enriched in Si (SiO₂=69.42%-72.52%), alkali (total alkali=7.43%-8.43%), K(K₂O=4.00%-5.02%, K₂O/Na₂O=1.17-1.62), Al(Al₂O₃=13.65%-14.25%), but depleted in Ca(CaO=1.20%-2.78%). Rb, Th, U, K, Pb elements are enriched in the intrusion while Ba, Nb, Sr, P, Ti elements are depleted. REE is characterized by obvious negative Eu anomalies (δEu=0.45-0.61), and exhibits right-dipping patterns with LREE enrichment. Its aluminum saturation index value (A/CNK) ranges from 0.93 to 1.16, while redman index value (δ) ranges from 2.06 to 2.41, indicating the intrusion belongs to high-K calc-alkaline series and metaluminous to peraluminous rocks. Its ε_Nd(t) value varies between -7.68 to -10.31, and the correspondent two-stage Nd isotopic modal ages range from 1.52 to 1.73 Ga (average value is 1.58 Ga). Mineralogy and geochemical characteristics indicate that Kunlunguan pluton is A-type granite. It has formed by partial melting of the Cathaysia paleoproterozoic felsic crustal material, being mixed with some mantle drived mafic malts, under a low-pressure, high-temperature condition at an extensional tectonic setting. Taking the igneous and metallogenic events in central Guangxi and adjacent areas into consideration, this study suggests that the lithosphere of South China hinterland thinned in 100-90 Ma.
- Kunlunguan pluton,
- A-type granite,
- South China,
- Late Yanshan,
- lithosphere extension,
- geochemistry

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References(106)

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