Bayanhaote Basin
| Bayanhaote Basin | |
|---|---|
| Geography | |
| Location | Inner Mongolia[1] |
| Country | China |
The Bayanhaote Basin[2] (simplified Chinese: 巴彦浩特盆地; traditional Chinese: 巴彥浩特盆地; pinyin: Bāyànhàotè Péndì), also known as Bayanhot Basin,[3] is a geographic region located in the west-central part of Inner Mongolia Autonomous Region.[4] It is a superimposed basin that underwent a long-term sedimentary evolution process from transgression to retrogression during the Carboniferous to Late Permian.[5]
The Bayanhot Basin is a composite and superimposed basin developed in the crossing zone of the Qinlin-Qilian-Helan trifurcate rift system (秦、祁、贺三叉裂谷系) during the beginning of Early Palaeozoic Era (早古生代早期) of crossover zone.[6]
It has been a self-flowing tectonic basin since the Mesozoic.[7] In the early 1950s, oil and gas exploration in this area began.[8]
References
[edit]- ^ 邓荣来; 李庆浩; 宋桂桥; 刘天佑 (2002). "重磁联合反演及重磁与MT综合解释巴彦浩特盆地火成岩" [Investigation on distribution of igneous rock in Bayabhaote Basin with joint inversion and integrated interpretation of gravity, magnetic and MT data]. 石油物探 [Geophysical Prospecting for Petroleum] (in Chinese). 41 (2): 222–225.
- ^ Li, A; Huang, WH; Yan, DN; Gong, YY (2013). "Accumulation conditions of the Carboniferous shale gas in Bayanhaote Basin and its southern periphery". Journal of Xi'an Shiyou University (Natural Science Edition). 28: 34–41.
- ^ 卢辉楠; 袁效奇 (1991). "巴彦浩特盆地及其边缘地区侏罗纪和早白垩世轮藻类" [Jurassic and Early Cretaceous charophytes from the Bayanhot Basin and its neighbourhood]. 微体古生物学报 [Acta Micropalaeontologica Sinica]. 8 (4): 373–394, 489–492.
- ^ 卫平生; 李天顺; 李安春; 王建功 (2005). "巴彦浩特盆地石炭系沉积相及沉积演化" [Carboniferous Sedimentary Evolution and Reservoir Estimation in Bayanhot Basin]. 沉积学报 [Acta Sedimentologica Sinica] (in Chinese). 23 (2): 240–247.
- ^ Zhao, Junfeng; Zhou, Yijun; Wang, Ke; Li, Xuan; Ma, Zhanrong; Ruan, Zhengzhong; Wang, Dong; Xue, Rui (May 2021). "Provenance and paleogeography of Carboniferous–Permian strata in the Bayanhot Basin: Constraints from sedimentary records and detrital zircon geochronology". Geoscience Frontiers. 12 (3): 101088. Bibcode:2021GeoFr..1201088Z. doi:10.1016/j.gsf.2020.09.017.
- ^ 宋桂桥; 马玉春; 刘传川; 孙潜茹; 于明德; 韩玉戟 (1999). "巴彦浩特盆地构造样式分析及其意义" [Structural Pattern Analysis of Bayanhaote Basin and Its Significance]. 石油地质与工程 [Petroleum Geology and Engineering] (in Chinese). 13 (4): 8–11.
- ^ 崔天秀 (1996). 据高灵敏度航空伽玛能谱资料探讨内蒙巴彦浩特盆地（腾格里沙漠）第四系成钾远景 [A Preliminary Study of Potash Potential Resources in the Bayinhaote Basin (the Tenygeli Desert) Based on Aerial Gamma (RAY) Spectrometric Data] (Report) (in Chinese). S2CID 223682146.
- ^ Mingwang, X. U. E.; Tan, Zhang; Wenlong, Ding; Baocheng, Jiao; Zhicheng, Zhou; Xiaoyu, D. U. (28 February 2020). "巴彦浩特盆地东部坳陷石炭系流体势特征及油气运聚单元划分" [Fluid potential characteristics of Carboniferous and the division of hydrocarbon migration and accumulation units in the eastern depression of the Bayanhaote Basin]. 地质力学学报 [Journal of Geomechanics] (in Chinese). 26 (1): 65–73. doi:10.12090/j.issn.1006-6616.2020.26.01.007.
Further reading
[edit]- Zhao, Hongge; Liu, Chiyang; Zhou, Yijun; Shao, Xiaozhou; Wang, Jianqiang; Peng, Zhichao; Huang, Lei; Ruan, Zhengzhong; Guo, Hui; Fu, Xinhui; Li, Ya'nan (October 2022). "Characteristics of late reformation and petroleum prospect of Carboniferous strata in the Bayanhot Basin, N. China". Geological Journal. 57 (10): 4183–4193. Bibcode:2022GeolJ..57.4183Z. doi:10.1002/gj.4537.
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