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| 1 | Thick-skinned Contractional Salt Structures in the Kuqa Depression,the Northern Tarim Basin:Constraints from Physical Experiments显示文摘摘要:脸皮厚的 contractional 盐结构广泛地在西方的 Kuqa 消沉被开发,北 Tarim 盆。为了理解管理这些的发展的机制,组织,物理实验被进行,结果证明他们被地下室差错并且形成 paleo 高举和地下室斜坡的活动大部分管理。在这研究的模型材料是干燥的沙,矿脂和 plasticene (或难泡沫) ,分别地模仿 suprasalt,盐,和 subsalt 层。实验证明由于地下室差错并且形成 paleo 高举的活动,盐身体通常在被预先退出的边界差错抑制的 paleo 高举的中间的顶上显著地积累并且变厚。大规模戳差错和盐越过水坝落下的水的发展被地下室赞成与更大的剧降泼出。实验也断定因为盐层的存在,那微分结构的变丑能发生在 subsalt 和 suprasalt 层之间。他们的几何学和结构的高度的地点是不同的,尽管有高举的区域的大类似。穿透的盐挤入构造没在实验被观察,它显示弄短的 contractional 有效地不加速盐挤入构造的发展。 | YU Yixin TANG Liangjie YANG Wenjing JIN Wenzheng PENG Gengxin LEI Ganglin | 2008 | Acta Geologica Sinica(English Edition)2008，82，2： | 15 |
| 2 | Reservoir accumulation conditions and key exploration&development technologies for Keshen gas field in Tarim Basin显示文摘The Keshen gas field is located in the central part of Kuqa foreland thrust belt in Tarim Basin,and is another large gas field discovered in Kuqa depression after Kela 2 gas field.Since the breakthrough in 2008,a number of large and medium scale gas reservoirs including Keshen 2,Keshen 5 and Keshen 8 have been discovered,that are characterized by ultra depth,ultra-high pressure,ultra-low porosity,ultra-low permeability,high temperature and high pressure.With natural gas geological reserves of nearly trillion cubic meters and production capacity of nearly 5.5 billion cubic meters,the Keshen gas field is the main natural gas producing area in Tarim Oilfield.The Keshen gas field is located in a series of thrusting imbrication structures in the Kelasu structural belt of Kuqa foreland thrust belt.The salt roof structure,plastic rheology of salt beds and pre-salt faulted anticlinal structure constitute the large wedge-shaped thrust body.The thick delta sandstone of the Cretaceous Bashijike Formation is widely distributed,and it forms the superior reservoir-caprock combination with overlying Paleogene thick gypsum-salt bed.The deep Jurassic-Triassic oil and gas migrate vertically along fault system formed in Late Himalaya,break through the thick Cretaceous mudstone and move laterally along the fracture system of the pre-salt reservoirs,to form anticline and fault anticline high pressure reservoir groups.Through near ten years of studies,the three-dimensional seismic acquisition and processing technology for complex mountainous areas,extrusion salt-related structural modeling technology and fractured low-porosity sandstone reservoir evaluation technology have been established,which lay a foundation for realization of oil and gas exploration objectives.Logging acquisition and evaluation technology for high temperature,high pressure,ultra-deep and low-porosity sandstone gas reservoirs,and efficient development technology for fractured tight sandstone gas reservoirs have been developed,which provide a technical support for efficient exploration&development and rapid production of the Keshen gas field. | Haijun Yang Yong Li Yangang Tang Ganglin Lei Xiongwei Sun Peng Zhou Lu Zhou Anming Xu Jingjie Tang Wenhui Zhu Jiangwei Shang Weili Chen Mei Li | 2019 | Petroleum Research2019，4，4： | 3 |
| 3 | Structural Evolution of the Eastern Qiulitagh Fold and Thrust Belt,Northern Tarim Basin,China显示文摘东方 Qiulitagh 褶层和戳带(EQFTB ) 是活跃 Kuqa 褶层的部分和北 Tarim 盆的戳带。地震思考侧面与地质的表面和练习数据是综合的检验变丑和 EQFTB 的结构风格,特别地第纳干扰器的 deformational 历史 2 煤气的地。地震解释建议 Dongqiu 8 是双结构在被动房顶戳下面开发了的外套,它在中新世的 Jidike 形成从一根尖端线产生了,并且脚底推进从在 Kuqatawu 背斜下面向西延长的一样的 Jidike 形成 evaporite 地区被开始。Dongqiu 5 是在 EQFTB 的西方的部分的弹出式结构,也在 Jidike 形成 evaporite 下面发展了。在 EQFTB 的很轻轻的地下室剧降和陡峭的蘸的地志的斜坡建议 Jidike 形成盐提供有效去耦。在 EQFTB 的强壮的变丑向南显得发展了进一步,在 evaporite 可能正在缺乏的一个区域。自从上新世, EQFTB 在 evaporite 上向南远移动了并且到达了 Yaken 区域。恢复一张平衡剖面图建议越过 EQFTB 的最小的弄短是超过 7800 m。假设这弄短发生在 5.3 妈期间预定平底锅,弄短的率是约 1.47 公里 / 年。 | YANG Minghui JIN Zhijun LU Xiuxiang SUN Dongsheng TANG Xuan PENG Gengxin LEI Ganglin | 2009 | Acta Geologica Sinica(English Edition)2009，83，2： | 2 |
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