准噶尔盆地克拉美丽气田滴西14井区石炭系蚀变凝灰岩储层热液作用过程及时限

刘小洪; 王委委; 冯明友; 卓宜茜; 岳怀海

doi:10.3799/dqkx.2021.188

Volume 47 Issue 5

May 2022

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Liu Xiaohong, Wang Weiwei, Feng Mingyou, Zhuo Yiqian, Yue Huaihai, 2022. Hydrothermal Process and Duration of Carboniferous Altered Tuff Reservoir in Well Dixi 14 Area of Kelameili Gas Field (Junggar Basin), NW China. Earth Science, 47(5): 1694-1710. doi: 10.3799/dqkx.2021.188

Citation:

Liu Xiaohong, Wang Weiwei, Feng Mingyou, Zhuo Yiqian, Yue Huaihai, 2022. Hydrothermal Process and Duration of Carboniferous Altered Tuff Reservoir in Well Dixi 14 Area of Kelameili Gas Field (Junggar Basin), NW China. Earth Science, 47(5): 1694-1710. doi: 10.3799/dqkx.2021.188

Citation:

Liu Xiaohong, Wang Weiwei, Feng Mingyou, Zhuo Yiqian, Yue Huaihai, 2022. Hydrothermal Process and Duration of Carboniferous Altered Tuff Reservoir in Well Dixi 14 Area of Kelameili Gas Field (Junggar Basin), NW China. Earth Science, 47(5): 1694-1710. doi: 10.3799/dqkx.2021.188

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Hydrothermal Process and Duration of Carboniferous Altered Tuff Reservoir in Well Dixi 14 Area of Kelameili Gas Field (Junggar Basin), NW China

doi: 10.3799/dqkx.2021.188

Liu Xiaohong^{1, 2
,
,},
Wang Weiwei¹,
Feng Mingyou^{1, 2
,
,},
Zhuo Yiqian¹,
Yue Huaihai¹

1.
School of Geosciences and Technology, Southwest Petroleum University, Chengdu 610500, China
2.
Natural Gas Geology Key Laboratory of Sichuan Province, Southwest Petroleum University, Chengdu 610500, China

Received Date: 2021-07-26
Publish Date: 2022-05-25

Abstract

Abstract

To decipher the fluid action and pore evolution in the Carboniferous altered tuff reservoir in Kelameili gas field (Junggar basin, Northwest China), the petrography and geochemistry were studied by core and thin section observation, scanning electron microscopy, electron probe, cathodoluminescence, fluorescence, rare elements and U-Pb isotope dating, etc.. The results show that the pore filling minerals of reservoir in the well Dixi 14 area mainly include kaolinite, albite, quartz, chlorite, pyrite, apatite, and the pore types are mainly residual pores of feldspar (K-feldspar and plagioclase) by dissolution-infilling and intergranular pores of various authigenic minerals. Firstly, the dissolution of pyroclastic materials and the transformation of diagenetic materials were fundamental for the formation of authigenic mineral. A large number of mold pores in crystal pyroclast were formed by acid fluid dissolution and kaolinite and quartz were precipitated from pores. More importantly, diagenetic environment changes caused by burial, hydrocarbon generation, hydrothermal charging and other activities are significant for pore formation and evolution. Albite and calcite were precipitated in dissolved pores by the fluid transformation from acid to alkaline, and resulted in the rapidly decrease of pores. During Middle Yanshanian (135±27 Ma), the thermal events were critical for the formation and evolution of the reservoir. (1) The illite of matrix was transformed into K-feldspar by the recharge of high temperature and rich-silicon hydrothermal fluid. (2) Simultaneously, fluoapatite and titanite were precipitated by combination of P, Ti, F ions with Ca²⁺ ion that derived by secondary dissolution, and filled the pores. Quartz was precipitated in the pore by the oversaturation of SiO₂ fluid. Thereafter, arsenopyrite and chlorite were formed by the transformation of alkaline and redox condition in the process of burial diagenesis. Thus, devitrification caused by temperature elevation, mineral transformation from clay to zeolite, recrystallization and dissolution partly increased the secondary reservoir space, which is beneficial to the enrichment of hydrocarbon.
- Kelameili gas field,
- Carboniferous,
- tuff reservoir,
- hydrothermal titanite,
- hydrothermal duration,
- petroleum geology

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Hydrothermal Process and Duration of Carboniferous Altered Tuff Reservoir in Well Dixi 14 Area of Kelameili Gas Field (Junggar Basin), NW China

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