Articles | Volume 14, issue 9
https://doi.org/10.5194/se-14-1031-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-14-1031-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
21 Sep 2023
Research article |
| 21 Sep 2023
| 21 Sep 2023
Mineralogical and elemental geochemical characteristics of Taodonggou Group mudstone in the Taibei Sag, Turpan–Hami Basin: implication for its formation mechanism
State Key Laboratory of Oil and Gas Resources and Exploration, Beijing
102249, China
Institute of Unconventional Oil and Gas Science and Technology, China
University of Petroleum-Beijing, Beijing 102249, China
Jianying Guo
CORRESPONDING AUTHOR
CNPC Key Laboratory of Natural Gas Accumulation and
Development, Langfang 065007,
China
Yanbin Wang
College of Geosciences and Surveying Engineering,
China University of Mining and Technology-Beijing, Beijing
100083, China
Zhenxue Jiang
State Key Laboratory of Oil and Gas Resources and Exploration, Beijing
102249, China
Institute of Unconventional Oil and Gas Science and Technology, China
University of Petroleum-Beijing, Beijing 102249, China
Chengju Zhang
State Key Laboratory of Oil and Gas Resources and Exploration, Beijing
102249, China
Institute of Unconventional Oil and Gas Science and Technology, China
University of Petroleum-Beijing, Beijing 102249, China
Chuanming Li
State Key Laboratory of Oil and Gas Resources and Exploration, Beijing
102249, China
College of Geosciences, China University of Petroleum-Beijing,
Beijing 102249, China
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Short summary
The Taodonggou Group mudstone was deposited in a warm, humid, and hot paleoclimate with strong weathering. The parent rocks of the Taodonggou Group mudstone are felsic volcanic rocks and andesites, with weak sedimentary sorting and recycling and with well-preserved source information. The Taodonggou Group mudstone was deposited in dyoxic fresh water–brackish water in intermediate-depth or deep lakes with stable inputs of terrigenous debris but at slower deposition rates.
The Taodonggou Group mudstone was deposited in a warm, humid, and hot paleoclimate with strong...
