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Science china Earth Sciences 2004年第10期47卷 886-895页

作者： TANG Liangjie1,2, JIA Chengzao3, PI Xuejun4. CHEN Suping1,2, WANG Zhiyu5, XIE Huiwen4.1. Key Laboratory for Hydrocarbon Accumulation of Education Ministry, Beijing 10224., china 2. Basin & Reservoir Research Center, University of Petroleum, Beijing 10224., china 3. petrochina company Limited, Beijing 100011, china 4. tarim oilfield company, petrochina company ltd., kurle 841000, china 5. Department of Geology, University of Petroleum, Beijing 10224., china Key Laboratory for Hydrocarbon Accumulation of Education Ministry Beijing China Basin & Reservoir Research Center University of Petroleum Beijing China petrochina company Limited Beijing China tarim oilfield company PetroChina Company Ltd. Kurle China Department of Geology University of Petroleum Beijing China

The salt beds of Lower Tertiary developed in the mid-segment of Kuqa foreland fold belt, northern tarim basin. They considerably controlled structural deformation of the belt. Ac- cording to the field observation, seismic profile interpretation and drilling data, three different structural styles of supra-salt, intra-salt and sub-salt occurred in the Kuqa foreland fold belt. Su- pra-salt structural styles mainly include thrust faults and fault-related sags. Intra-slat structural styles essentially are salt-pillows, intra-salt faults and folds, and salt weld structures. Sub-salt structural styles mainly consist of imbricated thrust faults, duplex structures, pop-up and fault-related folds. It is indicated that great differences exist among supra-salt, intra-salt and sub-salt structures of Kuqa foreland fold belt. The salt-related structures were formed in the same structural stress field. The dynamic mechanism of the salt-related structures is mainly associated with gravitation, compression and plastic flow of salt beds.

关键词： salt-related structural style, supra-salt structure, intra-salt structure, sub-salt structure, Kuga foreland fold belt.

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Abnormal high pressure in Kuqa foreland thrust belt of tarim basin: Origin and impacts on hydrocarbon accumulation

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Progress in Natural Science:Materials International 2006年第12期16卷 1307-1314页

作者： ZENG Lianbo~1** and LIU Benming~ 1,2 (1. Key Laboratory of Hydrocarbon Accumulation in china Petroleum University, Ministry of Education, Beijing 10224., china 2. The Institute of Oil and Gas Exploration and Development, tarim oilfield {4., petrochina {4. Limited, Korla 841000, china) Key Laboratory of Hydrocarbon Accumulation in china Petroleum University Ministry of Education Beijing 102249 China The Institute of Oil and Gas Exploration and Development Tarim Oilfield Company PetroChina Company Limited Korla 841000 China

Following analyses of the abnormal high pressure distribution characteristics, based on the geological characteristics, tectonic stress field and physical simulation, we investigated the formation mechanisms of abnormal high pressure and its impacts on hydrocarbon accumulation in the Kuqa foreland thrust belt. The abnormal high pressure appears at the bottom of the Paleogene and obviously exists in the Triassic and Jurassic. However, the pressure coefficient in the Triassic and Jurassic is lower than that in the Cretaceous and at the bottom of the Paleogene. Horizontally, the abnormal high pressure distribution is characterized by E-W orientation zoning. The maximum pressure coefficient lies in the Kelasu-Dongqiu-Dina tectonic zones in the center of the Kuqa foreland thrust belt and decreases away from the tectonic zones. The formation of abnormal high pressure was mainly related with the intense tectonic compression in the Early Pleistocene time, and tectonic uplifting, undercompaction and hydrocarbon generation were secondary factors contributing to abnormal high pressure. Under the rapid and intense tectonic compression in the Early Pleistocene, the rock framework firstly undertook 1/4.of the compression stress and the other was borne by the pore fluids. Due to the presence of great seal of gypsum-salt or gypsum-mudstone beds in the Paleogene, the pressure of pore fluids increased rapidly and led to the abnormal high pressure in the Kuqa foreland thrust belt. The abnormal high pressure has important impacts on hydrocarbon accumulation. It is one of the necessary conditions for formation of large oil and gas fields in the Kuqa foreland thrust belt.

关键词： abnormal high pressure formation mechanism oil and gas reservoir Kuqa foreland thrust belt tarim basin.

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Characteristics,genesis and accumulation history of natural gas in Hetianhe gasfield,tarim Basin,china

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Science china Earth Sciences 2008年第S1期51卷 84-95页

作者： WANG ZhaoMing 1 ,WANG QingHua 1 ,ZHAO MengJun 2 ,LI Yong 1 &XU ZhiMing 3 1 tarim oilfield company,petrochina,Kuerle {4.,china 2 Research Institute of Petroleum Exploration&Development,petrochina,Beijing 100083,china 3 Southwest Petroleum Institute,Nanchong 637001,china tarim oilfield company PetroChina Kuerle China Research Institute of Petroleum Exploration & Development PetroChina Beijing China Southwest Petroleum Institute Nanchong China

Hetianhe gasfield in Bachu region of the tarim Basin is mainly composed of three reservoir-caprock assembly,namely regional caprock of upper mudstone,middle mudstone and lower mudstone of the Carboniferous and reservoir of Bachu bioclastic limestone,glutenite and the Ordovician carbonate buried *** gas in Hetianhe gasfield sourced from the Cambrian source *** is thought that gases in Ma4.well block in the east of Hetianhe gasfield are mainly crude-oil cracked gases,while those in Ma3 and Ma8 well blocks in the west are the mixture gases of kerogen cracked gases and crude-oil cracked *** gas is rich in H2S and accumulated in multiply stages as the result of *** accumulation history is divided into three stages,namely accumulation and breakage in the late Caledonian-early Hercynian,migration and dissipation in the late Hercynian and accumulation in Himalayan. The main accumulation of reformed gas reservoir is in Himalayan.

关键词： gas characteristics gas genesis accumulation history Hetianhe gasfield tarim Basin

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Kinetics of hydrocarbon generation for Well Yingnan 2 gas reservoir,tarim Basin,china

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Science china Earth Sciences 2008年第S1期51卷 107-114页

作者： XIAO ZhongYao 1,2 ,XIAO XianMing 3 ,MA DeMing 4.,LU YuHong 2 &YANG ChaoShi 2 1 china University of Mining&Technology,Beijing 100083,china 2 Research Institutes of Exploration and Development,tarim oilfield {4.,petrochina,Korla 841000,china 3 Guangzhou Institutes of Geochemistry,Chinese Academy of Sciences,Guangzhou 51064.,china 4.Department of Synthetic Physical-Chemical Prospecting,BGP,Zhuozhou 072656,china china University of Mining & Technology Beijing China Research Institutes of Exploration and Development Tarim Oilfield Company PetroChina Korla China Guangzhou Institutes of Geochemistry Chinese Academy of Sciences Guangzhou China Department of Synthetic Physical-Chemical Prospecting BGP Zhuozhou China

Well Yingnan 2,an important exploratory well in the east of tarim Basin,yields high commercial oil and gas flow in *** gas components and carbon isotopic composition indicate that it belongs to sapropel type *** this region presents many suits of hydrocarbon source rocks,there are some controversies that natural gases were generated from kerogen gas or crude oil cracking gas at *** using the kinetics of hydrocarbon generation and carbon isotope,natural gas of Well Yingnan 2 is composed mainly of crude oil cracking gas,about 72%,it is generated from secondary kerogen gas of Cambrian-Lower Ordovician source rock and crude oil cracking gas of Mid-Upper Ordovician oil *** main oil and gas filling time is 65 Ma later in the Jurassic gas reservoir of Well Yingnan 2,so the gas reservoir belongs to late accumulation and continuous filling type.

关键词： kinetic migration and accumulation process crude oil cracking gas Well Yingnan 2 tarim Basin

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Poly-phase salt tectonics and hydrocarbon accumulation in tarim superimposed basin,northwest china

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Science china Earth Sciences 2004年第Z2期47卷 104-113页

作者： TANG Liangjie1,2, JIN Zhijun1’3, JIAChengzao1’4. Pl Xuejun5 & CHEN Suping1,2 1. Key Laboratory for Hydrocarbon Accumulation of Education Ministry, Beijing 10224., china 2. Basin & Reservoir Research Center, University of Petroleum, Beijing 10224., china 3. Institute of Petroleum Exploration and Development, SINOPEC, Beijing 100083, china 4. petrochina {4. Limited, Beijing 100011, china 5. tarim oilfield {4., petrochina company ltd., Korla 841000, china Key Laboratory for Hydrocarbon Accumulation of Education Ministry Beijing 102249 China Basin & Reservoir Research Center University of Petroleum Beijing 102249 China Key Laboratory for Hydrocarbon Accumulation of Education Ministry Beijing 102249 China Institute of Petroleum Exploration and Development SINOPEC Beijing 100083 China Key Laboratory for Hydrocarbon Accumulation of Education Ministry Beijing 102249 China petrochina company Limited Beijing 100011 China tarim oilfield company PetroChina Company Ltd. Korla 841000 China

The purpose of this paper is to discuss the poly-phase salt tectonics and its relation to the hydrocarbon accumulation of the tarim superimposed basin. Several salt sequences are developed in the tarim basin, they are: (1) the Mid-Early Cambrian salt sequence, mainly distributed in the west part of the north tarim uplift and Keping uplift; (2) the Early Carboniferous salt sequence, mainly distributed in the south slope of the north tarim uplift; (3) the Paleogene salt sequence, mainly distributed in the mid-west part of the Kuqa foreland fold belt and north tarim uplift; and (4. the Miocene salt sequence, mainly distributed in the east part of the Kuqa foreland fold belt. The salt sequences deposited in the tectonically calm scenario, while the salt layers deformed during the period of intense tectonism. Although the salt sequences are characteristic of plastic flow, the differences of salt deformation styles exist in the different salt sequences be-cause of the different deformation mechanism. It is attractive that the distribution of the large oil-gas fields or pools has a bearing upon the salt sequences and salt structures, such as the Tahe oilfield related to the Lower Carboniferous salt sequence and laterally facies changed mudstone, the Kela No.2 gas field to the Paleogene salt structures, and the Dina gas field to the Miocene salt structures. It is indicated that the large-scale hydrocarbon accumulation is con-trolled by the poly-phase salt sequences and structures. The deep analysis of the poly-phase salt tectonics is helpful to understanding the characteristics of the structural deformation and oil-gas accumulation of the tarim basin.

关键词： superimposed basin, salt tectonics, hydrocarbon accumulation, tarim basin.

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Control of neotectonic movement on hydrocarbon accumulation in the Kuqa Foreland Basin,west china

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Petroleum Science 2010年第1期7卷 49-58页

作者： Jiang Zhenxue Li Lianxia Song Yan Tian Fenghua Zhao Mengjun Wang Haijiang Zhao Zhenxing State Key Laboratory of Petroleum Resources and Prospecting China University of Petroleum Beijing 102249 China Basin and Reservoir Research Center China University of Petroleum Beijing 102249 China Exploration and Development Research Institute PetroChina Beijing 100083 China Department of Exploration ＆ Development PetroChina CBM Limited Company Beijing 100013 China Exploration Department Tarim Oilfield Company PetroChina Kuerle Xinjiang 841000 China No.8 Oil Production Plant Changqing Oilfield Company PetroChina Xi＇an Shaanxi 710018 China

Neotectonic movement refers to the tectonic movement that has happened since the Cenozoic, which is the latest movement. It has the most important influence on the basins in west china, especially on the hydrocarbon accumulation in the western foreland basins. We determined the time of neotectonic movement in the Kuqa Foreland Basin, which began from the Neogene, and analyzed the patterns of movement, which were continuous and fast subsidence in the vertical direction and intense lateral compression. The structure styles are that the faulting is weakened and the folding is strengthened gradually from north to south. We studied the control of neotectonic movement on the hydrocarbon accumulation process and model in the Kuqa Foreland Basin with basin simulation technique. The largest subsidence rate of the Kuqa Foreland Basin reached 1,200 m/Ma during the neotectonic movement, leading to rapid maturing of source rock within 5 Ma and a large quantity of hydrocarbon being generated and expelled. The thick neotectonic strata can form high quality reservoirs with the proved gas and oil reserves accounting for 5% and 27% of the total reserves, respectively. 86% of the structural traps were formed in the neotectonic movement period. The faults formed during the neotectonic movement serve as important migration pathways and they exist in the region where the hydrocarbon reservoirs are distributed. Abnormally high pressure caused by the intense lateral compression, thick neotectonic strata deposition and rapid hydrocarbon generation provide driving force for hydrocarbon migration. The accumulation elements match each other well over a short period, leading to many large gas fields formed later in the Kuqa Foreland Basin.

关键词： Kuqa Foreland Basin neotectonic movement accumulation element accumulation process accumulation model

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基于序贯模块法的天然气处理全流程模拟软件

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天然气工业 2009年第1期29卷 100-102页

作者：梁平陶宏伟李志铭唐柯彭志伟重庆科技学院中国石油西南油气田公司输气管理处中国石油塔里木油田公司中国航油重庆分公司中国石油大港油田公司

天然气处理系统是一个统一、密闭的水动力系统,仅通过单独改变某一个或多个设备的运行参数很难达到全流程最优处理效果。针对这种情况,在完成各单体设备处理流程模拟的基础上,提出了运用序贯模块法完成各单体设备之间输入输出的连接,实... 详细信息

天然气处理系统是一个统一、密闭的水动力系统,仅通过单独改变某一个或多个设备的运行参数很难达到全流程最优处理效果。针对这种情况,在完成各单体设备处理流程模拟的基础上,提出了运用序贯模块法完成各单体设备之间输入输出的连接,实现了天然气处理全流程模拟,可达到全流程操作参数优化的目的。应用该方法开发出的牙哈凝析气田集中处理站全流程模拟软件能够有效地实现全流程模拟,并就此提出了全流程优化方案。实践证明该优化方案可有效指导生产。

关键词：天然气处理序贯模块法全流程模拟软件优化设计

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库车坳陷西段盐构造及其与油气的关系

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石油学报 2004年第1期25卷 30-34,39页

作者：陈书平汤良杰贾承造皮学军谢会文石油大学石油天然气成藏机理教育部重点实验室中国地震局地质研究所北京100029 中国石油天然气股份有限公司塔里木油田分公司

根据断层相关褶皱理论和盐构造理论 ,结合地面地质调查和地震剖面的精细解释 ,厘定了库车坳陷西段下第三系库姆格列木群的膏盐岩层系的盐上、盐下和盐间构造样式、分布及形成机理。其中典型盐构造样式有盐核背斜、外来盐、盐枕、盐焊接... 详细信息

根据断层相关褶皱理论和盐构造理论 ,结合地面地质调查和地震剖面的精细解释 ,厘定了库车坳陷西段下第三系库姆格列木群的膏盐岩层系的盐上、盐下和盐间构造样式、分布及形成机理。其中典型盐构造样式有盐核背斜、外来盐、盐枕、盐焊接和断层焊接、盐缩颈、盐成凹陷和“鱼尾”构造。盐构造的形成分两个阶段 ,即早期初始形成阶段 ( 65～ 1 64.a)和晚期挤压构造定型阶段( 1 64.a前后 )。变形早期盐上层的重力滑动和顺层挤压决定了克拉苏构造带盐上、盐下不同的构造组合 ,秋立塔克构造带受滑脱传力作用 ,构造样式与盐层厚度和断层交切方式等有关。结合石油地质资料 ,讨论了盐构造的油气分布规律 ,并预测了有利勘探区带。

关键词：库车坳陷盐构造构造样式形成机理油气分布

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Quantitative studies of hydrocarbon loss of the Silurian bitumen sandstone in the tarim Basin

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Science china Earth Sciences 2008年第S2期51卷 101-107页

作者： JIANG ZhenXue1,2,PANG XiongQi1,2,LIU LuoFu1,2,WANG XianDong3,ZHANG Jun4.& LI HongYi1,2 1 Basin and Reservoir Research Center,china University of Petroleum,Beijing 10224.,china 2 State Key Laboratory of Petroleum Resource and Prospecting,china University of Petroleum,Beijing 10224.,china 3 Research Institute of Exploration and Development,Daqing {4. company ltd.Daqing 163712,china 4.Petroleum Exploration and Production Institute of SINOPEC,Beijing 100083,china Basin and Reservoir Research Center China University of Petroleum Beijing China State Key Laboratory of Petroleum Resource and Prospecting China University of Petroleum Beijing China Research Institute of Exploration and Development Daqing Oilfield Company Ltd Daqing China Petroleum Exploration and Production Institute of SINOPEC Beijing China

The evolution of tarim Basin experienced several tectonic movements,of which Caledonian movement caused a serious damage to reservoirs of Silurian. The earlier reservoirs size and the later hydrocarbon loss are two key factors to exploration prospect of Silurian. On the basis of net thickness of bituminous sandstone and recovery coefficient of crude oil converting to bitumen,the scale of the hydrocarbon loss of palaeo-accumulation in bitumen sandstone of Silurian was calculated (86.30×108t). The deter-mination of net thickness of bitumen sandstone was completed mainly by several methods,such as physical property demarcation,observing lithology,grains with oil inclusion (GOI) technology,and quantitative grains fluorescence (QGF) technology. The samples of black sandstone and white sand-stone were collected and compared by means of the methods mentioned above. The results showed that there was little hydrocarbon,or none,in the white sandstone. The recovery coefficient was ob-tained by the analyses of plentiful physical parameters of crude oil and bitumen sandstone,based on the hypothesis that nonhydrocarbon compounds and bitumen were invariable in the process of bitu-men forming. The calculated result,which is more scientific and actual,indicates the exploration pros-pect is more promising in Silurian of the tarim Basin.

关键词： tarim Basin Silurian bitumen sandstone hydrocarbon loss quantitative research recovery coefficient

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塔里木盆地塔中地区古生界油气成藏体系

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新疆石油地质 2004年第6期25卷 599-602页

作者：刘克奇刘玉魁敬兵杨喜峰石油大学盆地与油藏研究中心中国石油塔里木油田分公司勘探开发研究院新疆库尔勒841000 中国石油吉林油田分公司新木采油厂地质所吉林松原138000

油气成藏体系是地表以下含油气的自然系统,它包括了形成油气藏的一切必要元素以及这些元素之间有效的配置结构,其中的元素是烃源岩、输导体系和圈闭。塔中早古生代和晚古生代成藏体系的烃源岩、输导体系和圈闭均为分离状,都属于三位成... 详细信息

油气成藏体系是地表以下含油气的自然系统,它包括了形成油气藏的一切必要元素以及这些元素之间有效的配置结构,其中的元素是烃源岩、输导体系和圈闭。塔中早古生代和晚古生代成藏体系的烃源岩、输导体系和圈闭均为分离状,都属于三位成藏体系,但前者的油气来源单一(单源),后者的油气来源多样(多源),故两者分别被称之为塔中早古生代单源三位成藏体系和塔中晚古生代多源三位成藏体系。烃类流体主要来源于塔中北斜坡烃源岩,烃类流体沿不整合面和志留系砂岩层侧向运移,再沿断裂向上运移,分别为早古生代和晚古生代成藏体系提供油气。

关键词：晚古生代早古生代烃源岩圈闭塔中地区油气成藏古生界成藏体系输导体系烃类

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