学习与工作经历
研究方向 深层油气富集机理与分布规律 主讲课程
学术兼职 1.中国地质学会石油地质专业委员会秘书长 2.第七届中国青年科技工作者协会会员 3. 《石油与天然气地质》编委 4.《地球科学》青年编委 5.国家自然科学基金优青（海外）、重点支持项目、面上项目通讯评审专家 指导研究生
承担科研课题 国家自然科学基金企业创新发展联合基金重点支持项目: 克拉通盆地内部走滑断裂体系成因及控藏机制研究-以塔里木盆地为例，执行时间2022/1-2025/12，角色：负责人 国家自然科学基金企业创新发展联合基金重点支持集成项目研究课题：克拉通盆地差异演化与深层-超深层油气地质条件形成分布，执行时间2023/01-2026/12，角色：负责人 获奖情况 1. 2020年：塔里木克拉通内高陡构造解析理论、方法、技术及应用 2. 2021年：顺北油气田勘探与关键技术 3. 2022年：顺托地区克拉通内走滑断裂解析方法、技术及应用 4. 2023年：超深走滑断控缝洞型凝析气藏高效勘探关键技术 荣誉称号
著作
论文 [1]Deng, S., Zhao R, Kong Q, et al. Two distinct strike-slip fault networks in the Shunbei area and its surroundings, Tarim Basin: Hydrocarbon accumulation, distribution and controlling factors[J/OL]. AAPG Bulletin, 2022, 106(1)，77-102.
[2]Deng, S., Li H, Zhang Z, et al. Structural characterization of intracratonic strike-slip faults in the central Tarim Basin[J]. AAPG Bulletin, 2019, 103(1): 109-137.
[3]Deng, S., Jiang, R., Karimifard, M., Aydin, A. Fluid-flow effects of compartmentalized distribution of compaction bands in an aeolian sandstone in three dimensions [J]. Petroleum Geoscience. 2017. 23, 223–230.
[4]Deng, S., Aydin, A., The strength anisotropy of localized compaction: A model for the role of the nature and orientation of cross‐beds on the orientation and distribution of compaction bands in 3‐D. [J]Journal of Geophysical Research: Solid Earth, 2015, 120.3, 1523-1542.
[5]Deng, S., Cilona, A., Morrow, C., Mapeli, C., Liu, C., Lockner, D., Prasad, M., Aydin, A., Cross–bedding related anisotropy and its interplay with various boundary conditions in the formation and orientation of joints in an aeolian sandstone [J]. Journal of. Structural Geology. 2015, 77, 175–190.
[6]Deng, S., Zuo L., Aydin A., Dvorkin, J., Mukerji, T., Permeability characterization of natural compaction bands using core flooding experiments and three-dimensional image-based analysis: comparing and contrasting the results from two different methods, AAPG Bulletin, 2015, 99(1): 27-49.
[7]Deng, S., Aydin, A., Distribution of compaction bands in 3D in an aeolian sandstone: The role of cross-bed orientation [J]. Tectonophysics, 2012, 204–218.
[8]邓尚，邱华标，刘大卫，等. 克拉通内走滑断裂成因与控藏机制研究进展——以塔里木盆地北部为例，石油与天然气地质, 2024, 45(05): 1211-1225
[9]邓尚, 刘雨晴, 刘军, 等. 克拉通盆地内部走滑断裂发育､演化特征及其石油地质意义: 以塔里木盆地顺北地区为例[J/OL]. 大地构造与成矿学, 2021, 45(6): 1111-1126
[10]邓尚,李慧莉,韩俊, 等. 塔里木盆地顺北5号走滑断裂中段活动特征及其地质意义[J]. 石油与天然气地质, 2019, 40(05): 990-999.
[11]邓尚, 李慧莉, 张仲培, 等. 塔里木盆地顺北及邻区主干走滑断裂带差异活动特征及其与油气富集的关系[J]. 石油与天然气地质, 2018, 39(5): 878-888.
[12]Wang, Z., Deng, S., Xu, Q., Zhang, Y., Wei, H., Huang, W. and Wang, B., 2025. Structural geometry and evolution of the eastern Yuqi strike-slip faults in the Tabei Uplift, Tarim Basin (NW China). Marine and Petroleum Geology, p.107430.
[13]Qiu, H., Deng, S., Zhang J., et al. The evolution of a strike-slip fault network in the Guchengxu High, Tarim Basin (NW China), Marine and Petroleum Geology. 2022, 139. https://doi.org/10.1016/j.marpetgeo.2022.105655.
[14]Bian, Q, Deng, S, Lin H, Han. J, 2022. Strike-slip salt tectonics in the Shuntuoguole Low Uplift, Tarim Basin, and the significance to petroleum exploration [J]. Marine and Petroleum Geology. 139, https://doi.org/10.1016/j.marpetgeo.2022.105600.
[15]Qiu, H., Deng, S., Cao Z., et al. The Evolution of the Complex Anticlinal Belt With Crosscutting Strike‐Slip Faults in the Central Tarim Basin, NW China[J]. Tectonics, 2019, 38(6): 2087-2113.
[16]Han X, Deng S, Tang L, et al. Geometry, kinematics and displacement characteristics of strike-slip faults in the northern slope of Tazhong uplift in Tarim Basin: A study based on 3D seismic data[J]. Marine & Petroleum Geology, 2017, 88:410-427
[17]刘雨晴，邓尚，李海英，郭康康，刘大卫，耿锋，汝智星，彭威龙，符东宇，刘爽. 深层碳酸盐岩低序级断裂体系发育特征及勘探启示：以塔里木盆地顺北油气田为例[J].地球科学,2025,50(06):1-16.
[18]彭威龙，邓尚，张继标，等. 深层海相凝析油气藏成因机制与富集主控因素——以塔里木盆地顺北4 号断裂带为例［J］. 天然气地球科学，2024，35（5）：1-13.
[19]张继标,邓尚,韩俊,等.多期构造应力控制走滑断控储层发育机理与差异性研究——以塔里木盆地顺北地区为例[J].石油实验地质,2024,46(04):775-785.
[20]刘雨晴,邓尚,张继标,邱华标,韩俊,何松高.塔里木盆地顺北及邻区走滑断裂体系差异发育特征及成因机制探讨[J/OL].地学前缘。2023
[21]李映涛,邓尚,张继标,林会喜,刘雨晴,邱华标,黄诚,刘大卫,姚怿立.深层致密碳酸盐岩走滑断裂带核带结构与断控储集体簇状发育模式:以塔里木盆地顺北4号断裂带为例[J/OL].地学前缘:1-15[2023-06-19].DOI:10.13745/j.esf.sf.2023.2.32.（通讯）
[22]何松高,邓尚,刘雨晴等.克拉通内走滑断裂空间结构及派生构造新样式：以塔里木盆地顺北12号断裂为例[J].地球科学,2023,48(06):2136-2150.
[23]刘雨晴,邓尚.板内中小滑移距走滑断裂发育演化特征精细解析——以塔里木盆地顺北4号走滑断裂为例[J].中国矿业大学学报,2022,51(01):124-136.DOI:10.13247/j.cnki.jcumt.001324.
[24]高天，邓尚，李海英，等. 盆地深部穹隆构造发育特征、成因机制及石油地质意义[J]. 地质论评, 2021.
[25]李兵, 邓尚, 李王鹏, 等. 塔里木盆地塔河地区走滑断裂体系活动特征与油气地质意义[J]. 特种油气藏, 2019.
[26]Qiu, H., Lin, W., Deng, S., Lin, H., Zhang, Z., Cao, Z., Huang, C. and Han, J., 2024. The evolution of the early Paleozoic carbonate platform in the Central uplift, Tarim Basin, northwestern China, and hydrocarbon accumulation. AAPG Bulletin, 108(5), pp.943-969.
[27]Liu, Z., Fu, X., Deng, S., et al., The critical control of arkosic sandstone porosity on deformation band formation: Insights from the Shulu across-fault borehole in the Bohai Bay Basin, China, Journal of Structural Geology, 2021, 143, 104258.
[28]Liu, C., Pollard, D.D. Deng, S. & Aydin, A. 2015a. Mechanism of formation of wiggly compaction bands in porous sandstone: 1. Observations and conceptual model[J]. Journal of Geophysical Research: Solid Earth, 120,8138–8152
[29]杨孝群,焦存礼,邓尚,等.塔里木盆地满加尔坳陷西缘鹰山组台地沉积分异及其油气地质意义[J].地质学报,2024,98(12):3703-3714. DOI:10.19762/j.cnki.dizhixuebao.
[30]张仲培,王璐瑶,邓尚,魏华动,张继标.塔里木盆地塔中Ⅰ号构造带分段变形的运动学特征与成因探讨[J].地质论评,2020,66(04):881-892.DOI:10.16509/j.georeview.2020.04.007.
[31]杨鑫,徐旭辉,邓尚,翟常博,孔强夫,王石.塔里木西南大陆边缘原特提斯洋构造演化[J].地球科学,2020,45(11):4153-4175.
专利 1.邓尚, 张仲培. 地下走滑断裂水平滑移距定量分析方法（已授权，专利号：201810211634.X） 2.邓尚, 张仲培. 一种厘定盆地地下中小尺度走滑断裂活动期次的方法（已授权，专利号：201810211645.8） 3.邓尚，李兵等. 走滑断裂体系的拓扑分析方法（已授权，专利号：201910148403 .3） 4.邓尚，林会喜等.走滑断裂控储作用的定量评价方法、装置、存储介质和计算机设备（已授权，专利号：ZL 2021 1 0326337.1） |
