广东惠州燕山期以来地质构造演化：对华南构造的新启示

张敏; 旷健; 肖志才; 王帅; 祁士华; 陈孝雄; 李立峰; 唐灵

doi:10.3799/dqkx.2020.016

Volume 46 Issue 1

Jan. 2021

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Article Navigation > Earth Science > 2021 > 46(1): 242-258

Zhang Min, Kuang Jian, Xiao Zhicai, Wang Shuai, Qi Shihua, Chen Xiaoxiong, Li Lifeng, Tang Ling, 2021. Geological Evolution since the Yanshanian in Huizhou, Guangdong Province: New Implications for the Tectonics of South China. Earth Science, 46(1): 242-258. doi: 10.3799/dqkx.2020.016

Citation:

Zhang Min, Kuang Jian, Xiao Zhicai, Wang Shuai, Qi Shihua, Chen Xiaoxiong, Li Lifeng, Tang Ling, 2021. Geological Evolution since the Yanshanian in Huizhou, Guangdong Province: New Implications for the Tectonics of South China. Earth Science, 46(1): 242-258. doi: 10.3799/dqkx.2020.016

Citation:

Zhang Min, Kuang Jian, Xiao Zhicai, Wang Shuai, Qi Shihua, Chen Xiaoxiong, Li Lifeng, Tang Ling, 2021. Geological Evolution since the Yanshanian in Huizhou, Guangdong Province: New Implications for the Tectonics of South China. Earth Science, 46(1): 242-258. doi: 10.3799/dqkx.2020.016

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Geological Evolution since the Yanshanian in Huizhou, Guangdong Province: New Implications for the Tectonics of South China

doi: 10.3799/dqkx.2020.016

Zhang Min^{1
,
,},
Kuang Jian²,
Xiao Zhicai²,
Wang Shuai³,
Qi Shihua^{2, 3},
Chen Xiaoxiong⁴,
Li Lifeng¹,
Tang Ling^{1
,
,
,}

1.
Team 935 of Guangdong Nonferrous Metals Geological Bureau, Huizhou 516001, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
3.
School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
4.
Petroleum Engineering and Geophysics Co., Ltd., SINOPEC, Wuhan 430223, China

Received Date: 2020-02-10
Publish Date: 2021-01-15

Abstract

Abstract

Based on synthesizes basic Geological Survey, magnetotellurics, lithogeochemistry, and chronology, a case study of the Shiba-Huangshadong area in Huizhou was settled to reveal the evolution of geological tectonics since the Yanshanian (Jurassic and Cretaceous era) in Huizhou, Guangdong. The magnetotelluric data display that there are present the subterrane an bedrock of Yanshanian granite intrusions with a thickness of more than 5 km, and the graniteis sliced by the Cenozoic faults. The basal conglomerate minerals in the Danxia Formation have edges and corners, which show near-source sedimentary characteristics.The harmonic age and age spectrum show that the age of basal conglomerate is about 160 Ma.The REE pattern and spider diagram of granites in the study area with age more than 150 Ma indicate that the basal conglomerate is the product of denudation of Yanshanian granite. Based on the tectonic evolution of South China and its adjacent areas, we have established a conceptual model of geological evolution of the study area since the Yanshanian. The emplacement of the voluminous Yanshanian granite resulted in the uplift of the crust.The previously deposited strata suffered from long-term denudation, which caused the expose and denudation of granite that in the Paleozoic and Mesozoic strata. Combined with the Cenozoic large-scale Yue-Gui shearing caused by the collision of India-Eurasia plate and the northward drift of Philippine Plate, forming a series of deep-seated faults, for example, the Heyuan fault, the Zijin-Boluo fault, and the Lianhuashan fault.These faults are all cutting through the Yanshanian granite body. The current topography of the study area has been shaped by multiple activities.
- tectonic evolution,
- shearing,
- Yanshanian,
- Cenozoic,
- Huizhou, Guangdong Province

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Geological Evolution since the Yanshanian in Huizhou, Guangdong Province: New Implications for the Tectonics of South China

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