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The formation and evolution of Chepaizi-Mosuowan paleo-uplift and its control on the distributions of sedimentary facies in the Junggar Basin

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Science China Earth Sciences 2010年第6期53卷 818-831页

作者： ji youliang ZHOU Yong KUANG Jun WAN Lu ZHANG Rui LU ChunHong State Key Laboratory of Petroleum Resource and Prospecting China University of PetroleumBeijing 102249China Xinjiang Oil Field Urumqi 834000China

The Chepaizi-Mosuowan paleo-uplift is a large-scale uplift stretching across the Junggar Basin formed during the Yanshanian. It has experienced four evolutionary stages: the initial forming stage (J1), the intense development stage (J2+3), the waning and burial stage (K-E), and the tilting and extinction stage (N-Q). The most intense period of activities is the Middle Jurassic. Dur-ing the Early Jurassic, the Chepaizi-Mosuowan paleo-structure was a low amplitude uplift. Because of the subsequent strong uplifting during Middle-Late Jurassic, the Middle and Upper Jurassic were eroded. With the evolution of the Chepaizi-Mosuowan paleo-uplift, the sedimentary pattern of the basin changed, and the paleo-uplift separated the northern depositional systems from those in the south side. As a result, the basin tectonics controlled the distribution and evolution of the depositional systems. During Early Jurassic, while the paleo-uplift was low, its controlling effect on depositional systems was limited and sediments coming from the northwest could reach the central and southern parts of the basin. With the strong uplifting of the Chepaizi-Mosuowan paleo-structure during Middle-Late Jurassic, sediments from the northwest provenance could only deposit in the northern graben of the paleo-uplift. The intense erosion of the Middle-Upper Jurassic also changed the former sedimentary center of the basin into a source area, supplying sediments for grabens on both sides of the paleo-uplift. In the Cretaceous, regional subsidence caused the paleo-uplift to be buried again and subsequently sediments accumulated on top of it. The depositional facies are dominated by fluvial in the Early Cretaceous and shallow lacustrine to deltaic in the Late Cretaceous. In the history of the long-lasting development of this paleo-uplift, large-scale erosions of the paleohigh not only provided sufficient sediments to the center of the Junggar Basin, but also created favorable conditions for the formation o

关键词： Chepaizi-Mosuowan paleo-uplift formation and evolution depositional systems Junggar Basin.

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The Formation Mechanism and Developmental Characteristics of Tight Oil

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Acta Geologica Sinica(English Edition) 2015年第A1期89卷 71-72页

作者： PAN Yanan ji youliang WANG Tianyun China University of Petroleum

1Introduction Unconventional oil and gas, a kind of resources of great exploration potential, has a wide application future. Tight oil, an important part of unconventional oil and gas,attracts much more attention. With the continuous improvement of technology exploration and the continuous exploitation of oil and gas, tight oil is widedly concerned in recent years.

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The Identification of an Alkaline Salt Lake:A Case Study from the Permian Fengcheng Formation in Hashan-Wuxia Area

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Acta Geologica Sinica(English Edition) 2014年第S1期88卷 233-234页

作者： MENG jinluo ji youliang ZHANG Bin jiN Li CHE Shiqi State Key Laboratory of Petroleum Resources and Prospecting College of GeosciencesChina University of Petroleum

The study area is located in the northwest of Junggar basin which was in the relaxation stage of foreland basin accompanied by momentary extend volcanic activities when the Fengcheng Formation developed in early

关键词： Alkaline salt lake Hashan-Wuxia area

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塔南凹陷白垩纪古地貌对沉积体系分布的控制作用

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石油学报 2009年第6期30卷 843-848,855页

作者：蒙启安纪友亮中国石油大学油气资源与探测国家重点实验室北京102249 中国石油大庆油田有限责任公司勘探开发研究院黑龙江大庆163000

塔南凹陷是在海拉尔—塔木查格盆地新发现的主要油气勘探和开发区。对早白垩世沉积充填特征的综合研究表明,长期活动的同沉积断裂形成的、古地貌上突变的各种断裂坡折带对盆内沉积体系的发育及分布起到重要的控制作用。根据塔南凹陷边... 详细信息

塔南凹陷是在海拉尔—塔木查格盆地新发现的主要油气勘探和开发区。对早白垩世沉积充填特征的综合研究表明,长期活动的同沉积断裂形成的、古地貌上突变的各种断裂坡折带对盆内沉积体系的发育及分布起到重要的控制作用。根据塔南凹陷边缘和盆内的古地貌结构特征,将其划分为断崖型陡坡坡折带、断阶型陡坡坡折带、断阶型缓坡坡折带和盆内坡折带4种类型,它们各自控制了不同类型沉积体系的形成和分布。断崖型陡坡坡折带控制着近岸水下扇沉积体系的形成和分布;断阶型陡坡坡折带控制着扇三角洲或近岸水下扇及前方的湖底扇体系的形成和分布;断阶型缓坡坡折带控制着扇三角洲沉积体系的形成和分布;在基准面下降阶段,盆内坡折控制着远岸湖底扇的形成和分布。

关键词：古地貌地层层序古构造坡折带沉积体系白垩纪塔南凹陷

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Pore throat characteristics of tight sandstone of Yanchang Formation in eastern Gansu,Ordos Basin

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Petroleum Research 2018年第1期3卷 33-43页

作者： Hao Wu Chunlin Zhang youliang ji Rui'e Liu Shang Cao Sheng Chen Yunzhao Zhang Ye Wang Wei Du Gang Liu College of Geosciences China University of PetroleumBeijing 102249China State Key Laboratory of Petroleum Resources and Prospecting Beijing 102249China Natural Gas Geological Department PetroChina Research Institute of Petroleum Exploration and DevelopmentHebei 065007China Research Institute of Shaanxi Yanchang Petroleum(Group)Co.Ltd. Shaanxi 710075China Institute of Marine Geology and Resource Ocean CollegeZhejiang UniversityZhejiang 310058China

An important factor to evaluate reservoir quality is the pore-throat ***,the strong heterogeneity makes it difficult to characterize the pore-throat distribution in tight *** field emission scanning electron microscope(FESEM),high pressure mercury injection and rate-controlled mercury injection are used to investigate the pore-throat size distribution in tight sandstone reservoirs of Member 7 of the Yanchang Formation in eastern Gansu,Ordos Basin,and studies of the pore throat size controlling on physical property of the tight sandstone reservoirs are also carried *** result shows that the pore type is mainly dominated by the residual intergranular pore,dissolution pore,micropore and a few micro-fractures;the high-pressure mercury injection experiment indicates that the pore-throat size ranges from 0.0148 μm to 40mm,the pore throat more than 1 mm is less;the ratecontrolled mercury injection experiment reveals that for samples with different physical properties,the pore radius mainly varies from 80 μm to 350 μm;the throat radius exhibits the strong heterogeneity,and is from 0.12 μm to 30μm;the pore-throat size can be effectively characterized by combination of high-pressure and rate-controlled mercury injections,and it varies from 0.0148 μm to 350 μ*** permeability is mainly controlled by the large pore throat(>R_(50))which accounts for a small proportion;in the tight sandstone with the permeability greater than 0.1 mD,the permeability is mainly controlled by the micropore and mesopore;in the tight sandstone with the permeability smaller than 0.1 mD,the permeability is mainly controlled by the nanopore and micropore;the proportion of small pore throat increases with reduction of permeability,it is important that the small pore throat influences the reservoir storage property though its effect on permeability are small.

关键词： Pore-throat size High-pressure and rate-controlled mercury injections Reservoir physical property Tight sandstone Member 7 of the Yanchang Formation Eastern Gansu

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Reservoir Characteristics and Control Factors of The 4th Member of Xujiahe Formation in The Middle Part of Western Sichuan Depression

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Acta Geologica Sinica(English Edition) 2015年第A1期89卷 77-78页

作者： SONG Hongyu ji youliang ZHOU Yong CHEN Xianliang ZHAO Chunni DONG Ruojing YANG Yong College of Geosciences China University of Petroleum Beijing 102249 China Xi'an University of Science and Technology Xi'an Shanxi 710054 China Exploration and Development Research Institute PetroChina Southwestern Oil and Gasfield Company ChengduSichuan 610041 China Research Institute of Petroleum Exploration andDevelopment Beijing 100083 China PetroChina Exploration and Development Company Beijing 100034 China

1 Introduction The western Sichuan depression is a foreland basin which formed since late Triassic. The middle part of it is the focus of our study, the west boundary is Longmen mountain and the east is Zhongjiang, th...

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DIAGENETIC　TRAPS　OF　EOGENE　DEEP－SEATED　CLASTIC　GAS　RESERVOIRS　IN　THE　DONGPU　DEPRESSION：A　DISCUSSION　ON　THEIR　ORIGIN

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Scientia Geologica Sinica 1995年第4期 431-438页

作者： Zhao Chenglin Liu Menghui ji youliang and Li Yumei (Petroleum University, Beijing 102200)

ＤＩＡＧＥＮＥＴＩＣＴＲＡＰＳＯＦＥＯＧＥＮＥＤＥＥＰ－ＳＥＡＴＥＤＣＬＡＳＴＩＣＧＡＳＲＥＳＥＲＶＯＩＲＳＩＮＴＨＥＤＯＮＧＰＵＤＥＰＲＥＳＳＩＯＮ：ＡＤＩＳＣＵＳＳＩＯＮＯＮＴＨＥＩＲＯＲＩＧＩＮ￥ＺｈａｏＣｈｅ... 详细信息

ＤＩＡＧＥＮＥＴＩＣＴＲＡＰＳＯＦＥＯＧＥＮＥＤＥＥＰ－ＳＥＡＴＥＤＣＬＡＳＴＩＣＧＡＳＲＥＳＥＲＶＯＩＲＳＩＮＴＨＥＤＯＮＧＰＵＤＥＰＲＥＳＳＩＯＮ：ＡＤＩＳＣＵＳＳＩＯＮＯＮＴＨＥＩＲＯＲＩＧＩＮ￥ＺｈａｏＣｈｅｎｇｌｉｎ；ＬｉｕＭｅｎｇｈｕｉ；...

关键词： GAS RESERVOIRS SEATED THE CLASTIC DEEP

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陆相前陆盆地层序结构特征研究-以准噶尔南缘晚期前陆盆地为例

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石油与天然气地质 2008年第2期29卷 237-243,251页

作者：纪友亮安爱琴朱如凯中国石油大学资源与信息学院北京102249 同济大学海洋与地球科学学院上海200092 中国石油天然气股份有限公司石油勘探开发研究院北京100083

陆相前陆盆地层序地层学是目前层序地层学的一个重要研究领域和方向。准噶尔南缘为一两期叠加的复合再生型前陆盆地,综合地震、测井、钻井、露头资料对晚期前陆层序进行了划分,共划分出1个一级层序,3个二级层序,5个三级层序以及15个四... 详细信息

陆相前陆盆地层序地层学是目前层序地层学的一个重要研究领域和方向。准噶尔南缘为一两期叠加的复合再生型前陆盆地,综合地震、测井、钻井、露头资料对晚期前陆层序进行了划分,共划分出1个一级层序,3个二级层序,5个三级层序以及15个四级层序。依据前陆盆地构造-沉积演化的旋回性及层序的内部发育特征,将各个二级层序划分出4个体系域。建立了准南前陆盆地层序地层模式,探讨了构造活动的层序地层响应。构造活动控制层序界面的形成,一次逆冲末期的回弹隆升和下一次逆冲引起的变形是形成构造层序界面的主要原因。随着造山带前缘推覆的不断向前发展,前陆盆地的沉降中心和沉积中心向斜坡带方向迁移。构造层序的发育具有旋回性和阶段性,每一层序始于沉降速率迅速加快。

关键词：层序地层格架叠置样式构造作用的沉积响应前陆盆地准噶尔盆地南缘

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高邮凹陷古近系戴南组戴一段物源分析

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同济大学学报（自然科学版） 2012年第9期40卷 1406-1413页

作者：纪友亮王勇李清山胡斌中国石油大学(北京)地球科学学院北京102249 江苏油田分公司物探研究院江苏南京210046 中国石油勘探开发研究院廊坊分院河北廊坊065000

在分析了高邮凹陷戴南组沉积期构造和沉积背景的基础上,利用重矿物组合分析法、矿物成分分析法、砂岩质量百分含量法、地震反射波组形态分析法和古地貌分析法,对戴南组戴一段的物源进行了分析.认为高邮凹陷中东部戴南组戴一段北部物源... 详细信息

在分析了高邮凹陷戴南组沉积期构造和沉积背景的基础上,利用重矿物组合分析法、矿物成分分析法、砂岩质量百分含量法、地震反射波组形态分析法和古地貌分析法,对戴南组戴一段的物源进行了分析.认为高邮凹陷中东部戴南组戴一段北部物源来自于柘垛低凸起,存在4个主要物源,南部物源主要来自通扬隆起区以及东南部的吴堡低凸起,存在5个主要物源.在此基础上,编制了戴南组戴一段的沉积体系分布图.

关键词：物源分析沉积体系古近系戴南组高邮凹陷

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SEQUENCE　STRATIGRAPHY　AND　SANDBODY　PREDICTION　IN　THE　CARBONIFEROUS　OF　TARIM　BASIN

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Scientia Geologica Sinica 1995年第4期 521-530页

作者： ji youliang Wang Yi Li Hongnan Zhang Liqiang and Zhang Shiqi (University of Petroleum, Dongying, Shangdong 257062)

ＳＥＱＵＥＮＣＥＳＴＲＡＴＩＧＲＡＰＨＹＡＮＤＳＡＮＤＢＯＤＹＰＲＥＤＩＣＴＩＯＮＩＮＴＨＥＣＡＲＢＯＮＩＦＥＲＯＵＳＯＦＴＡＲＩＭＢＡＳＩＮ￥ＪｉＹｏｕｌｉａｎｇ；ＷａｎｇＹｉ；ＬｉＨｏｎｇｎａｎ；ＺｈａｎｇＬｉｑ...

ＳＥＱＵＥＮＣＥＳＴＲＡＴＩＧＲＡＰＨＹＡＮＤＳＡＮＤＢＯＤＹＰＲＥＤＩＣＴＩＯＮＩＮＴＨＥＣＡＲＢＯＮＩＦＥＲＯＵＳＯＦＴＡＲＩＭＢＡＳＩＮ￥ＪｉＹｏｕｌｉａｎｇ；ＷａｎｇＹｉ；ＬｉＨｏｎｇｎａｎ；ＺｈａｎｇＬｉｑｉａｎｇａｎｄＺｈａｎｇＳｈｉｑｉ...

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