Study on the Mechanism of Siliceous Dolomite — A Case Study in a Field of Sichuan Basin

Wang Jie; Zhang Tieqiang; Sun Desheng; Li Jianhua; Zhang Sheng; Yan Zhenhua

doi:doi:10.11648/j.ogce.20231103.12

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Study on the Mechanism of Siliceous Dolomite — A Case Study in a Field of Sichuan Basin

Wang Jie, Zhang Tieqiang, Sun Desheng, Li Jianhua, Zhang Sheng, Yan Zhenhua

Published in International Journal of Oil, Gas and Coal Engineering (Volume 11, Issue 3)

Received: 6 June 2023 Accepted: 21 June 2023 Published: 8 July 2023

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Abstract

This study mainly explores the genesis of regional siliceous dolomite. Previous research was mainly based on petrological observations, conventional elemental analysis, stable isotope analysis, and elemental geochemistry, but the genesis of siliceous rocks is controversial. Based on quantitative analysis of siliceous rocks, this study investigated the source of siliceous dolomite through seismic data, curvature attributes, and paleogeography, and analyzed genetic mechanism of siliceous dolomite. The study found that siliceous dolomite gradually thickens from west to east, with a maximum thickness of 60 meters. Multiple volcanic channels are distributed in the well1 area, which spewed siliceous hot springs. Controlled by the ancient structural background, siliceous hot springs flowed from the high plateau to the low-lying area inside the plateau. Under the action of seawater, siliceous hot springs and dolomite underwent metasomatism to form siliceous dolomite. The innovation of this study lies in the use of multiple methods, such as seismic data, curvature attributes, and paleogeography, to study the genesis of siliceous dolomite. The research results provide new ideas and methods for further exploring the genesis of siliceous rocks.

Published in	International Journal of Oil, Gas and Coal Engineering (Volume 11, Issue 3)
DOI	10.11648/j.ogce.20231103.12
Page(s)	64-68
Creative Commons	This is an Open Access article, distributed under the terms of the Creative Commons Attribution 4.0 International License (http://creativecommons.org/licenses/by/4.0/), which permits unrestricted use, distribution and reproduction in any medium or format, provided the original work is properly cited.
Copyright	Copyright © The Author(s), 2024. Published by Science Publishing Group

Keywords

Siliceous Dolomite, Volcanic Hydrothermal Origin, Volcanic Channel, Curvature Attribute

References

[1]	Ma Wenxin, Liu Shugen, Huang Wenming, etc Structural characteristics and genetic mechanism of siliceous rocks in the Dengying Formation of the Sinian system in the eastern Chongqing region [J] Journal of Geology, 2014, 88 (2): 239-253.
[2]	MA Wenxin, LIU Shugen, HUANG Wenming, et al. Fabric Characteristics and Formation Mechanism of Chert in Sinian.
[3]	Dengying Formation, Eastern Chongqing [J]. Acta Geologic Sinica, 2014, 88 (2): 239-253.
[4]	Feng Caixia, Liu Jiajun The current research status and mineralization significance of siliceous rocks [J] World Geology 2001 (02): 119-123.
[5]	Yi Haisheng, Zeng Yunfu, Xia Wenjie A Study on the Sedimentary Facies and Origin of Siliceous Rocks of the Upper Sinian Series in the Hunan Guizhou Guangxi Region [J] Mineral Rock, 1989, 9 (4): 54-58.
[6]	Xiao Fan, Ban Yizhong, Zhou Yan, etc Discovery of Late Carboniferous hydrothermal siliceous rocks in Longyan area of Mount Wuyi metallogenic belt and its geological significance [J] Geology of East China.
[7]	Chen Yongquan, Jiang Shaoyong, Zhou Xinyuan, et al. 2010. Elements δ 30si, δ 18O geochemical research [J] Geochemistry, 39 (2): 159-170.
[8]	Adachi M, Yamamoto K, Sulglsk R. 1986. Hydro-thermal chert and associated siliceous rocks from the Northern Pacific: Their Geological significance as indication of ocean ridge activity [J]. Sedimentary Geology, 47 (1-2): 125-148.
[9]	Chen Xianpei, Chen Duofu. 1989. Geochemical characteristics of hydrothermal deposition of upper Devonian breast cherts in Guangxi [J] Geochemistry, 1 (2): 1-8.
[10]	Chen Qingsong, Yang Runbai, Liu Demin, et al. Origin and sedimentary environment of siliceous rocks of the Huize Dengying Formation in northeastern Yunnan - evidence from petrology and geochemistry: evidence from petrology and geochemistry. Journal of Jilin University (Geoscience Edition), 2019, 49 (5): 132-1337.
[11]	Liu Daming, Yao Hongyou, Hu Lin, et al. Genesis and sedimentary environment of Late Paleozoic siliceous rocks in Kara area, western Sichuan [J]. China Geological survey, 2020, 7 (6): 68-78.
[12]	Tang Xuesong, Tan Xiucheng, Liu Hong, et al., Characteristics and development patterns of dolomite and siliceous rock reservoirs in the Maokou Formation of the Middle Permian in the eastern Sichuan Basin. Oil and Gas Geology, 2016, 237 (5): 731-743.
[13]	Luo Wenjun, Xu Wei, Zhu Zhengping, et al., Genesis and geological significance of siliceous rocks in the fourth member of the Dengying Formation of the Sinian system in the Gaoshiti area of the Sichuan Basin, Natural Gas Exploration and Development, 2019, 42 (3): 1-9.
[14]	Jin Xiaoyan, Liu Xiaojian, Hao Yi Wei, etc. Volcanic hydrothermal fluid activity in CF oil fields and its transformation on Carbonate rock reservoirs Petroleum Geology and Oilfield Development in Daqing, 2019, 38 (1): 42-50.
[15]	He Wenyuan, Yun Jianbing, Zhong Jianhua. Reservoir-forming mechanism of carbonate dolomitization of Permian Changxing Formation in northeastern Sichuan Basin [J]. Lithologic Reservoirs, 2022, 34 (5): 1-25.

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APA Style

Wang Jie, Zhang Tieqiang, Sun Desheng, Li Jianhua, Zhang Sheng, et al. (2023). Study on the Mechanism of Siliceous Dolomite — A Case Study in a Field of Sichuan Basin. International Journal of Oil, Gas and Coal Engineering, 11(3), 64-68. https://doi.org/10.11648/j.ogce.20231103.12

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ACS Style

Wang Jie; Zhang Tieqiang; Sun Desheng; Li Jianhua; Zhang Sheng, et al. Study on the Mechanism of Siliceous Dolomite — A Case Study in a Field of Sichuan Basin. Int. J. Oil Gas Coal Eng. 2023, 11(3), 64-68. doi: 10.11648/j.ogce.20231103.12

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AMA Style

Wang Jie, Zhang Tieqiang, Sun Desheng, Li Jianhua, Zhang Sheng, et al. Study on the Mechanism of Siliceous Dolomite — A Case Study in a Field of Sichuan Basin. Int J Oil Gas Coal Eng. 2023;11(3):64-68. doi: 10.11648/j.ogce.20231103.12

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@article{10.11648/j.ogce.20231103.12,
  author = {Wang Jie and Zhang Tieqiang and Sun Desheng and Li Jianhua and Zhang Sheng and Yan Zhenhua},
  title = {Study on the Mechanism of Siliceous Dolomite — A Case Study in a Field of Sichuan Basin},
  journal = {International Journal of Oil, Gas and Coal Engineering},
  volume = {11},
  number = {3},
  pages = {64-68},
  doi = {10.11648/j.ogce.20231103.12},
  url = {https://doi.org/10.11648/j.ogce.20231103.12},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ogce.20231103.12},
  abstract = {This study mainly explores the genesis of regional siliceous dolomite. Previous research was mainly based on petrological observations, conventional elemental analysis, stable isotope analysis, and elemental geochemistry, but the genesis of siliceous rocks is controversial. Based on quantitative analysis of siliceous rocks, this study investigated the source of siliceous dolomite through seismic data, curvature attributes, and paleogeography, and analyzed genetic mechanism of siliceous dolomite. The study found that siliceous dolomite gradually thickens from west to east, with a maximum thickness of 60 meters. Multiple volcanic channels are distributed in the well1 area, which spewed siliceous hot springs. Controlled by the ancient structural background, siliceous hot springs flowed from the high plateau to the low-lying area inside the plateau. Under the action of seawater, siliceous hot springs and dolomite underwent metasomatism to form siliceous dolomite. The innovation of this study lies in the use of multiple methods, such as seismic data, curvature attributes, and paleogeography, to study the genesis of siliceous dolomite. The research results provide new ideas and methods for further exploring the genesis of siliceous rocks.},
 year = {2023}
}

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TY  - JOUR
T1  - Study on the Mechanism of Siliceous Dolomite — A Case Study in a Field of Sichuan Basin
AU  - Wang Jie
AU  - Zhang Tieqiang
AU  - Sun Desheng
AU  - Li Jianhua
AU  - Zhang Sheng
AU  - Yan Zhenhua
Y1  - 2023/07/08
PY  - 2023
N1  - https://doi.org/10.11648/j.ogce.20231103.12
DO  - 10.11648/j.ogce.20231103.12
T2  - International Journal of Oil, Gas and Coal Engineering
JF  - International Journal of Oil, Gas and Coal Engineering
JO  - International Journal of Oil, Gas and Coal Engineering
SP  - 64
EP  - 68
PB  - Science Publishing Group
SN  - 2376-7677
UR  - https://doi.org/10.11648/j.ogce.20231103.12
AB  - This study mainly explores the genesis of regional siliceous dolomite. Previous research was mainly based on petrological observations, conventional elemental analysis, stable isotope analysis, and elemental geochemistry, but the genesis of siliceous rocks is controversial. Based on quantitative analysis of siliceous rocks, this study investigated the source of siliceous dolomite through seismic data, curvature attributes, and paleogeography, and analyzed genetic mechanism of siliceous dolomite. The study found that siliceous dolomite gradually thickens from west to east, with a maximum thickness of 60 meters. Multiple volcanic channels are distributed in the well1 area, which spewed siliceous hot springs. Controlled by the ancient structural background, siliceous hot springs flowed from the high plateau to the low-lying area inside the plateau. Under the action of seawater, siliceous hot springs and dolomite underwent metasomatism to form siliceous dolomite. The innovation of this study lies in the use of multiple methods, such as seismic data, curvature attributes, and paleogeography, to study the genesis of siliceous dolomite. The research results provide new ideas and methods for further exploring the genesis of siliceous rocks.
VL  - 11
IS  - 3
ER  -

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Author Information

Wang Jie

Geological Research Center of Research Institute of BGP, Zhuozhou, China
Zhang Tieqiang

Geophysical Technology Research Center of BGP, Zhuozhou, China
Sun Desheng

Geological Research Center of Research Institute of BGP, Zhuozhou, China
Li Jianhua

Geological Research Center of Research Institute of BGP, Zhuozhou, China
Zhang Sheng

Geological Research Center of Research Institute of BGP, Zhuozhou, China
Yan Zhenhua

Geological Research Center of Research Institute of BGP, Zhuozhou, China

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Plain Text BibTeX RIS

APA Style

Wang Jie, Zhang Tieqiang, Sun Desheng, Li Jianhua, Zhang Sheng, et al. (2023). Study on the Mechanism of Siliceous Dolomite — A Case Study in a Field of Sichuan Basin. International Journal of Oil, Gas and Coal Engineering, 11(3), 64-68. https://doi.org/10.11648/j.ogce.20231103.12

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ACS Style

Wang Jie; Zhang Tieqiang; Sun Desheng; Li Jianhua; Zhang Sheng, et al. Study on the Mechanism of Siliceous Dolomite — A Case Study in a Field of Sichuan Basin. Int. J. Oil Gas Coal Eng. 2023, 11(3), 64-68. doi: 10.11648/j.ogce.20231103.12

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AMA Style

Wang Jie, Zhang Tieqiang, Sun Desheng, Li Jianhua, Zhang Sheng, et al. Study on the Mechanism of Siliceous Dolomite — A Case Study in a Field of Sichuan Basin. Int J Oil Gas Coal Eng. 2023;11(3):64-68. doi: 10.11648/j.ogce.20231103.12

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@article{10.11648/j.ogce.20231103.12,
  author = {Wang Jie and Zhang Tieqiang and Sun Desheng and Li Jianhua and Zhang Sheng and Yan Zhenhua},
  title = {Study on the Mechanism of Siliceous Dolomite — A Case Study in a Field of Sichuan Basin},
  journal = {International Journal of Oil, Gas and Coal Engineering},
  volume = {11},
  number = {3},
  pages = {64-68},
  doi = {10.11648/j.ogce.20231103.12},
  url = {https://doi.org/10.11648/j.ogce.20231103.12},
  eprint = {https://article.sciencepublishinggroup.com/pdf/10.11648.j.ogce.20231103.12},
  abstract = {This study mainly explores the genesis of regional siliceous dolomite. Previous research was mainly based on petrological observations, conventional elemental analysis, stable isotope analysis, and elemental geochemistry, but the genesis of siliceous rocks is controversial. Based on quantitative analysis of siliceous rocks, this study investigated the source of siliceous dolomite through seismic data, curvature attributes, and paleogeography, and analyzed genetic mechanism of siliceous dolomite. The study found that siliceous dolomite gradually thickens from west to east, with a maximum thickness of 60 meters. Multiple volcanic channels are distributed in the well1 area, which spewed siliceous hot springs. Controlled by the ancient structural background, siliceous hot springs flowed from the high plateau to the low-lying area inside the plateau. Under the action of seawater, siliceous hot springs and dolomite underwent metasomatism to form siliceous dolomite. The innovation of this study lies in the use of multiple methods, such as seismic data, curvature attributes, and paleogeography, to study the genesis of siliceous dolomite. The research results provide new ideas and methods for further exploring the genesis of siliceous rocks.},
 year = {2023}
}

Copy | Download

TY  - JOUR
T1  - Study on the Mechanism of Siliceous Dolomite — A Case Study in a Field of Sichuan Basin
AU  - Wang Jie
AU  - Zhang Tieqiang
AU  - Sun Desheng
AU  - Li Jianhua
AU  - Zhang Sheng
AU  - Yan Zhenhua
Y1  - 2023/07/08
PY  - 2023
N1  - https://doi.org/10.11648/j.ogce.20231103.12
DO  - 10.11648/j.ogce.20231103.12
T2  - International Journal of Oil, Gas and Coal Engineering
JF  - International Journal of Oil, Gas and Coal Engineering
JO  - International Journal of Oil, Gas and Coal Engineering
SP  - 64
EP  - 68
PB  - Science Publishing Group
SN  - 2376-7677
UR  - https://doi.org/10.11648/j.ogce.20231103.12
AB  - This study mainly explores the genesis of regional siliceous dolomite. Previous research was mainly based on petrological observations, conventional elemental analysis, stable isotope analysis, and elemental geochemistry, but the genesis of siliceous rocks is controversial. Based on quantitative analysis of siliceous rocks, this study investigated the source of siliceous dolomite through seismic data, curvature attributes, and paleogeography, and analyzed genetic mechanism of siliceous dolomite. The study found that siliceous dolomite gradually thickens from west to east, with a maximum thickness of 60 meters. Multiple volcanic channels are distributed in the well1 area, which spewed siliceous hot springs. Controlled by the ancient structural background, siliceous hot springs flowed from the high plateau to the low-lying area inside the plateau. Under the action of seawater, siliceous hot springs and dolomite underwent metasomatism to form siliceous dolomite. The innovation of this study lies in the use of multiple methods, such as seismic data, curvature attributes, and paleogeography, to study the genesis of siliceous dolomite. The research results provide new ideas and methods for further exploring the genesis of siliceous rocks.
VL  - 11
IS  - 3
ER  -

Copy | Download