闽西南龙岩地区印支期天宫山花岗岩体成因

康丛轩; 周延; 宗雯; 范飞鹏; 李凤春; 孙建东; 吕劲松

doi:10.3799/dqkx.2017.602

Volume 43 Issue 12

Dec. 2018

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Kang Congxuan, Zhou Yan, Zong Wen, Fan Feipeng, Li Fengchun, Sun Jiandong, Lü Jinsong, 2018. Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian. Earth Science, 43(12): 4621-4637. doi: 10.3799/dqkx.2017.602

Citation:

Kang Congxuan, Zhou Yan, Zong Wen, Fan Feipeng, Li Fengchun, Sun Jiandong, Lü Jinsong, 2018. Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian. Earth Science, 43(12): 4621-4637. doi: 10.3799/dqkx.2017.602

Citation:

Kang Congxuan, Zhou Yan, Zong Wen, Fan Feipeng, Li Fengchun, Sun Jiandong, Lü Jinsong, 2018. Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian. Earth Science, 43(12): 4621-4637. doi: 10.3799/dqkx.2017.602

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Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian

doi: 10.3799/dqkx.2017.602

1.
Nanjing Center of Geological Survey, China Geological Survey, Nanjing 210016, China
2.
School of Earth Sciences and Engineering, Hohai University, Nanjing 210016, China
3.
Geological Survey of Jiangsu Province, Nanjing 210018, China
4.
Testing Center of Shandong Bureau, China Metallurgy and Geology Bureau, Jinan 250014, China

Received Date: 2017-12-19
Publish Date: 2018-12-15

Abstract

Abstract

The research of petrogenesis about Tiangongshan Indosinian granites have great significance on the magmatic evolution and dynamic process in Southwest Fujian. The Tiangongshan pluton is dominated by syenogranite. Previous studies obtained the K-Ar age of 146-149 Ma from its granites, while U-Pb zircon analyses yielded consistent age of 233±2.0 Ma and 230±2.8 Ma by LA-ICP-MS in our study, indicating that the pluton was formed in Late Triassic and Indosinian tectonic movement. The granites are characterized by high silicon and alkali (σ=1.21-2.55, A/CNK=0.97-1.73), belonging to quasi aluminum to peraluminous calc-alkaline series. The granites have high ΣREE and relative accumulation of LREE, and are deficient in Al₂O₃ and Sr, and rich in Y and Yb, showing obvious micrographic texture with relatively high negative Eu anomaly and moderately negative to weak positive Ce anomaly; the granites are depleted in LILE and enriched in HFSE.The Tiangongshan pluton has the characteristics of A-type granite with high Ga/Al value. Its w (P₂O₅) averages on 0.02%, lower than that of highly fractionated S-type granite, w (Na₂O) on average of 2.93%, higher than that of highly fractionated S-type granite, and w (TFeO) on average of 1.15%, higher than that of highly fractionated I-type granite.The average saturation temperature of zircon is 729.8℃.The ε_Hf(t) all is negative (-5.29 to -10.69), suggesting possible material sources from the lower crustal material of Paleoproterozoic. The magma of the diagenetic stage, derived from partial melting of the crustal material, is crust-derived aluminous A-type granite formed in the syn-collisional settings. Through the stage of Indosinian collisional-compressional orogeny, the Paleoproterozoic lower crustal material of the pluton initially melted. Stretched by Indosinian tectonic movements, part of the mantle material was involved in the underplating.
- Tiangongshan granite,
- Indosinian,
- U-Pb age of zircon,
- rock formation cause,
- Lu-Hf isotope,
- geochemistry

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References(92)

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Petrogenesis of Tiangongshan Indosinian Granites in Longyan Area, Southwest Fujian

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