吉南老岭地区早白垩世铝质A型花岗岩的厘定及其构造意义

秦亚; 梁一鸿; 胡兆初; 冯坚; 李敏

doi:10.3799/dqkx.2013.068

Volume 38 Issue 4

Jul. 2013

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Article Navigation > Earth Science > 2013 > 38(4): 677-688

QIN Ya, LIANG Yi-hong, HU Zhao-chu, FENG Jian, LI Min, 2013. Confirmation of Aluminous A-Type Granite Emplacement and Its Tectonic Significance during Early Cretaceous in the Laoling Area, South of Jilin Province. Earth Science, 38(4): 677-688. doi: 10.3799/dqkx.2013.068

Citation:

QIN Ya, LIANG Yi-hong, HU Zhao-chu, FENG Jian, LI Min, 2013. Confirmation of Aluminous A-Type Granite Emplacement and Its Tectonic Significance during Early Cretaceous in the Laoling Area, South of Jilin Province. Earth Science, 38(4): 677-688. doi: 10.3799/dqkx.2013.068

Citation:

QIN Ya, LIANG Yi-hong, HU Zhao-chu, FENG Jian, LI Min, 2013. Confirmation of Aluminous A-Type Granite Emplacement and Its Tectonic Significance during Early Cretaceous in the Laoling Area, South of Jilin Province. Earth Science, 38(4): 677-688. doi: 10.3799/dqkx.2013.068

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Confirmation of Aluminous A-Type Granite Emplacement and Its Tectonic Significance during Early Cretaceous in the Laoling Area, South of Jilin Province

doi: 10.3799/dqkx.2013.068

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
State Key Laboratory of Geological Process and Mineral Resources, China University of Geosciences, Wuhan 430074, China

Received Date: 2012-12-27
Publish Date: 2013-07-01

Abstract

Abstract

Major and trace elements analysis and LA-ICP-MS zircon U-Pb ages show Toudao, Laoling, Shanglvshuiqiao and Gaotaizi plutons are Early Cretaceous aluminum A-type granites in the Laoling area, South of Jilin Province.Plutons mainly consist of k-feldspar granite, miarolitic k-feldspar granite, granite porphyry and granites.The results of LA-ICP-MS dating are (121-125) Ma.The major elements of granitoids are high in Si, alk and low in Fe, Mg, Ca, and Ti.Trace elements are enriched in incompatible elements such as K, Rb, Th and depleted in Ba, Sr, Ti, Nb, Ta, and P.The granitoids have right-wing type of chondrite-normalized REE patterns and moderate negative Eu anomalies.Geochemical features indicate that granitoids are aluminum A-type granites (A/CNK=(0.82-1.15), A/NK=(1.00-1.28)).Granitoids with relatively low incompatible element ratio values such as Ce/Nb, Y/Nb and Yb/Ta are A₁-type anorogenic granite.The formation of A₁-type granite indicates Laoling area is in the Anorogenic extensional tectonic setting during Early Cretaceous.
- geochronology,
- aluminous A-type granite,
- extensional tectonic environment,
- geochemistry,
- South of Jilin Province

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References(42)

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