南海北部中央峡谷水道的岩相-地球化学特征及其源区性质

尤丽; 钟佳; 张迎朝; 李才; 吴仕玖; 代龙; 蔡玉蔓

doi:10.3799/dqkx.2017.588

Volume 43 Issue 2

Feb. 2018

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Article Navigation > Earth Science > 2018 > 43(2): 514-524

You Li, Zhong Jia, Zhang Yingzhao, Li Cai, Wu Shijiu, Dai Long, Cai Yuman, 2018. Petrography-Geochemistry and Source Significance of Western Canyon Channel of Northern South China Sea. Earth Science, 43(2): 514-524. doi: 10.3799/dqkx.2017.588

Citation:

You Li, Zhong Jia, Zhang Yingzhao, Li Cai, Wu Shijiu, Dai Long, Cai Yuman, 2018. Petrography-Geochemistry and Source Significance of Western Canyon Channel of Northern South China Sea. Earth Science, 43(2): 514-524. doi: 10.3799/dqkx.2017.588

Citation:

You Li, Zhong Jia, Zhang Yingzhao, Li Cai, Wu Shijiu, Dai Long, Cai Yuman, 2018. Petrography-Geochemistry and Source Significance of Western Canyon Channel of Northern South China Sea. Earth Science, 43(2): 514-524. doi: 10.3799/dqkx.2017.588

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Petrography-Geochemistry and Source Significance of Western Canyon Channel of Northern South China Sea

doi: 10.3799/dqkx.2017.588

1.
College of Earth Sciences, Jilin University, Changchun 130061, China
2.
The Zhanjiang Branch of CNOOC Ltd., Zhanjiang 524057, China
3.
The Geological Survey Institute of Jiangsu Province, Nanjing 210018, China

Received Date: 2017-09-26
Publish Date: 2018-02-15

Abstract

Abstract

Canyon channel is the main reservoir of the deepwater area in Qiongdongnan basin in the northern South China Sea. Reservoir stones have good physical properties since they are dominated by powder and fine sandstones. However, there are few studies on the main provenance supply, nature of the parent rock area in different periods of channel formation, and paleo-weathering degree. In this study, it is found that the rock types are mainly debris-quartz sandstone and feldspar-debris sandstone.The heavy mineral assemblages show that they are dominated by magnetite, ilmenite, zircon and tourmaline in Yacheng area, whereas they are dominated by ilmenite, garnet, tourmaline and zircon in Lingshui area. Geochemical characteristics of mudstone show significantly lower SiO₂ content, but higher Fe₂O₃, MgO, K₂O and the total amount of rare earth contents relating to high clay minerals than sandstone. Al₂O₃/TiO₂, K₂O/Al₂O₃ and K₂O/Na₂O ratios in mudstone and sandstone indicate that the source area is enriched in quartz and depleted in potassium feldspar, and is of quartz sediment source, and neutral igneous rock source respectively. The sandstone is characterized with higher SiO₂/Al₂O₃ ratio, lower ICV, CIA and CIW values compared to mudstone, indicating that the source regions have experienced low to moderate weathering, and they are the deposition of recirculation in the stable tectonic environment, whereas the formation environment of mudstone is more active.
- canyon channel,
- petrography,
- geochemistry,
- source significance,
- Huangliu Formation,
- deepwater area,
- Qiongdongnan basin

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References(58)

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