银额盆地哈日凹陷下白垩统热水沉积岩特征及成因

陈志鹏; 任战利; 于春勇; 祁凯; 任文波; 杨燕; 马骞

doi:10.3799/dqkx.2018.527

Volume 43 Issue 6

Jun. 2018

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Article Navigation > Earth Science > 2018 > 43(6): 1941-1956

Chen Zhipeng, Ren Zhanli, Yu Chunyong, Qi Kai, Ren Wenbo, Yang Yan, Ma Qian, 2018. Characteristics and Genetic Analysis of Hydrothermal Sediment of Lower Cretaceous in Hari Depression, Yin'e Basin. Earth Science, 43(6): 1941-1956. doi: 10.3799/dqkx.2018.527

Citation:

Chen Zhipeng, Ren Zhanli, Yu Chunyong, Qi Kai, Ren Wenbo, Yang Yan, Ma Qian, 2018. Characteristics and Genetic Analysis of Hydrothermal Sediment of Lower Cretaceous in Hari Depression, Yin'e Basin. Earth Science, 43(6): 1941-1956. doi: 10.3799/dqkx.2018.527

Citation:

Chen Zhipeng, Ren Zhanli, Yu Chunyong, Qi Kai, Ren Wenbo, Yang Yan, Ma Qian, 2018. Characteristics and Genetic Analysis of Hydrothermal Sediment of Lower Cretaceous in Hari Depression, Yin'e Basin. Earth Science, 43(6): 1941-1956. doi: 10.3799/dqkx.2018.527

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Characteristics and Genetic Analysis of Hydrothermal Sediment of Lower Cretaceous in Hari Depression, Yin'e Basin

doi: 10.3799/dqkx.2018.527

State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China

Received Date: 2018-02-01
Publish Date: 2018-06-15

Abstract

Abstract

The Lower Cretaceous of the Hari sag in the Yin'e basin has a unique sedimentary structure and mineral composition. The cause, sedimentary environment and formation pattern of the hydrothermal sediment of Lower Cretaceous in Hari depression, Yin'e basin are discussed in this study, based on its mineralogy, petrology and geochemistry. The Lower Cretaceous in Hari depression with lots of minerals including ganalcites, siderite and dolomite, is rich in Fe, Mn and Ba, characterized by high content of ∑REE, enrichment of LREE, and the negative Eu anomaly. Combined with Fe vs. Mn vs. (Cu+Co+Ni)×10 and Ni vs. Co vs. Zn ternary diagrams, it is proved that the Lower Cretaceous received long-term hydrothermal input during deposition. Analyses of trace elements, carbon and oxygen isotopes indicate the anoxic, closed, salty and lacustrine depositional environment. The formation temperatures of carbonate calculated by oxygen isotopes range from 43.94 ℃ to 86.08 ℃. It is concluded that complex faulting system provides the access to the lake water infiltrating down and the hydrothermal fluids upwelling. Moreover, convection activities between the hydrothermal fluids and the lake water continually offer heat and mineral elements to the lake. This type of hydrothermal sedimentation is long enduring and wide ranging, controlled by both terrigenous detrital materials supply and hydrothermal fluid property, which represents a special sedimentary model.
- lacustrine hydrothermal sediment,
- geochemical characteristics,
- formation temperature,
- hydrothermal fluid eruption,
- Yin'e basin,
- Lower Cretaceous,
- petroleum geology

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References(73)

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沈阳化工大学材料科学与工程学院沈阳 110142

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Characteristics and Genetic Analysis of Hydrothermal Sediment of Lower Cretaceous in Hari Depression, Yin'e Basin

doi: 10.3799/dqkx.2018.527

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