甘肃红石泉地区基性岩脉特征及Ar-Ar定年

蓝德初; 张树明; 秦雨; 杨春四; 王利玲; 戚佳伟

doi:10.3799/dqkx.2018.272

Volume 44 Issue 10

Nov. 2019

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Article Navigation > Earth Science > 2019 > 44(10): 3469-3483

Lan Dechu, Zhang Shuming, Qin Yu, Yang Chunsi, Wang Liling, Qi Jiawei, 2019. Characteristics and Ar-Ar Dating of Mafic Dykes in Hongshiquan Area, Gansu Province. Earth Science, 44(10): 3469-3483. doi: 10.3799/dqkx.2018.272

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Lan Dechu, Zhang Shuming, Qin Yu, Yang Chunsi, Wang Liling, Qi Jiawei, 2019. Characteristics and Ar-Ar Dating of Mafic Dykes in Hongshiquan Area, Gansu Province. Earth Science, 44(10): 3469-3483. doi: 10.3799/dqkx.2018.272

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Characteristics and Ar-Ar Dating of Mafic Dykes in Hongshiquan Area, Gansu Province

doi: 10.3799/dqkx.2018.272

1.
State Key Laboratory Breeding Base of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, China
2.
National Defense Key Laboratory of Radioactive Geology and Exploration Technology, East China University of Technology, Nanchang 330013, China
3.
Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China

Received Date: 2018-12-12
Publish Date: 2019-11-11

Abstract

Abstract

The basic vein is a "window" for studying mantle and its evolution, and has important relationship with gold, uranium, diamond deposits and the others. The most typical alaskite type uranium deposit in China occurs in Hongshiquan area of Gansu Province among which there are a number of basic veins. The fresh surface of the basic rocks in the study area is gray-green, with typical lamprophyre structure, and massive structure. The porphyry minerals are mainly hornblende, the matrix mainly is composed of plagioclase and biotite, and accessory minerals are mainly magnetite, apatite, zircon etc.. Based on this characteristics, it is determined that the basic rock is diorite lamprophyre. The characteristics of elemental geochemistry ascertain that the lamprophyres are rich in alkali, high in potassium, poor in iron, and enriched in LREE and LILE, indicating that they belong to potash calc-alkaline lamprophyres. The whole-rock ⁴⁰Ar-³⁹Ar dating yields a lamprophyre diagenetic age of 237.2±2.6 Ma. The magma of the lamprophyre originated from EMII-enriched mantle and formed in the intraplate extensional environment. The magma was contaminated with crustal materials during the process of rising emplacement, which was the product of the extension following closure of the Late Asian Paleozoic Paleo-Asian Ocean and continental collision. There is no direct genetic relationship between the uranium metallogenesis of the Hongshiquan lamprophyre and the uranium deposit, but only late-stage transformation of uranium deposits.
- lamprophyre,
- petrography,
- geochemistry,
- Ar-Ar whole-rock dating,
- Hongshiquan,
- petrology

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Characteristics and Ar-Ar Dating of Mafic Dykes in Hongshiquan Area, Gansu Province

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