珠江口盆地珠江组混积岩中有孔虫的矿化特征与机制

刘娜; 吴克强; 刘立; 于雷; 徐思萌; 彭晓蕾

doi:10.3799/dqkx.2020.079

Volume 45 Issue 10

Nov. 2020

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Liu Na, Wu Keqiang, Liu Li, Yu Lei, Xu Simeng, Peng Xiaolei, 2020. Mineralization Characteristics and Mechanism of Foraminifera in Mixed Siliciclastic-Carbonate Sediments in Zhujiang Formation of Pearl River Mouth Basin. Earth Science, 45(10): 3746-3758. doi: 10.3799/dqkx.2020.079

Citation:

Liu Na, Wu Keqiang, Liu Li, Yu Lei, Xu Simeng, Peng Xiaolei, 2020. Mineralization Characteristics and Mechanism of Foraminifera in Mixed Siliciclastic-Carbonate Sediments in Zhujiang Formation of Pearl River Mouth Basin. Earth Science, 45(10): 3746-3758. doi: 10.3799/dqkx.2020.079

Citation:

Liu Na, Wu Keqiang, Liu Li, Yu Lei, Xu Simeng, Peng Xiaolei, 2020. Mineralization Characteristics and Mechanism of Foraminifera in Mixed Siliciclastic-Carbonate Sediments in Zhujiang Formation of Pearl River Mouth Basin. Earth Science, 45(10): 3746-3758. doi: 10.3799/dqkx.2020.079

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Mineralization Characteristics and Mechanism of Foraminifera in Mixed Siliciclastic-Carbonate Sediments in Zhujiang Formation of Pearl River Mouth Basin

doi: 10.3799/dqkx.2020.079

Liu Na^{1
,
,},
Wu Keqiang²,
Liu Li^{1
,
,},
Yu Lei¹,
Xu Simeng¹,
Peng Xiaolei¹

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
Research Institute of China National Offshore Oil Corporation Limited, Beijing 100028, China

Received Date: 2019-12-30
Publish Date: 2020-11-17

Abstract

Abstract

The Pearl River Mouth basin is an important area for deep water petroleum exploration in China,within which,the Liwan X structure is mainly composed of mixed siliciclastic-carbonate sediments at the depths between 3 000 m and 3 281 m. Petrologic and isotopic geochemical characteristics were investigated by polarizing microscope and carbon-oxygen isotopic analysis. The host rock type of foraminifera and the petrographic characteristics of foraminifera mineralization were determined,and the mineralization mechanism of foraminifera was discussed,and finally the mineralization model of foraminifera was established. The bioclast of Zhujiang Formation is mainly composed of foraminiferal clasts,while the foraminiferal shell is composed of blade-,equal diameter calcite or ferrocalcite. There are mainly three filling patterns for the foraminifera's chamber:unfilled,half-filled and full-filled pattern. According to the types and the occurrences of the main authigenic minerals,the foraminiferal mineralization can be divided into four types,including pyritization,ferrocalcitization,dawsonitization and ankeritization,among which the formation of pyritization may be related to the biodegradation of foraminiferal soft tissue,and the ferrocalcitization may be related to the thermal decarboxylation of organic matter,while the magmatic CO₂ provided the carbon sources for the precipitation of dawsonite and ankerite.
- mineralization mechanism,
- mixed siliciclastic-carbonate sediment,
- foraminifera,
- dawsonite,
- mantle CO₂,
- Pearl River Mouth basin,
- sedimentation,
- hydrocarbon

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Mineralization Characteristics and Mechanism of Foraminifera in Mixed Siliciclastic-Carbonate Sediments in Zhujiang Formation of Pearl River Mouth Basin

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