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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 {2. 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 1,2.0 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 2.% 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

Volcanic Facies and Their Reservoirs Characteristics in Eastern china Basins

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地学前缘 2009年第S1期16卷 152-153页

作者： Chunshuang Jin~(1,2.,Dewu Qiao~2.Wenli Pan~3 1.institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 10002.,china. 2.Strategic {2. Center of Oil & Gas Resources,Ministry of Land & Resources,Beijing 100034,china 3.Geophysical exploration {2. institute of Huabei oilfield company,Renqiu 062.52.china

In these years,the Upper Jurassic andesitic volcanic reservoirs in Erlian basin,the Lower Cretaceous rhyolitic volcanic reservoirs in Songliao Basin,the Cretaceous rhyolitic,and the Paleogene basaltic and trachytic volcanic reservoirs in Bohai Bay Basin,and the basaltic volcanic reservoirs in Subei basin were *** more and more volcanic oil and gas fields being discovered and developed,the volcanic rocks demonstrate a great petroleum potential in eastern basins of *** volcanic facies were identified in these basins,including volcanic conduit facies,explosive facies,effusive facies。

关键词： volcanic rocks volcanic facies reservoirs porosity types

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限定井眼方向待钻轨道设计的代数法

西南石油大学学报（自然科学版） 2009年第5期31卷 158-162页

作者：鲁港中国石油辽河油田公司勘探开发研究院辽宁盘锦124010

限定了井眼方向的待钻井眼轨道设计问题需要求解一个7元非线性方程组,通常使用的数值迭代方法有许多固有的缺点,提出了一个新方法──代数法:将原始非线性方程组化简成一个三元多项式方程组,再进一步归结为求一个10次多项式方程全部正... 详细信息

限定了井眼方向的待钻井眼轨道设计问题需要求解一个7元非线性方程组,通常使用的数值迭代方法有许多固有的缺点,提出了一个新方法──代数法:将原始非线性方程组化简成一个三元多项式方程组,再进一步归结为求一个10次多项式方程全部正实数解问题和一个二元线性代数方程组问题。给出了代数法的计算机实现方法,具有计算速度快、数值稳定性好、存储需求小等特点。代数法具有与解析法相近的良好数学性质,能够对问题是否有解做出事前判断;在问题存在多个解的情况下,能够正确求出全部的解。所使用的数学化简技巧能够推广应用到求解定向井、水平井的井眼轨道设计问题中,有重要的理论价值和应用前景。

关键词：圆弧井眼轨道钻井设计代数方程数学机械化

research on the dynamics of the South china Sea opening:Evidence from analogue modeling

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Science china Earth Sciences 2006年第10期49卷 1053-1069页

作者： SUN Zhen1,2. ZHOU Di1, ZHONG Zhihong3, XIA Bin2. QIU Xuelin1, ZENG Zuoxun4 & JIANG Jianqun5 1. CAS Key Laboratory of Marginal Sea Geology, South china Sea institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, china 2. CAS Key Laboratory of Marginal Sea Geology, Guangzhou institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, china 3. Department of Technology, Shenzhen Branch of CNOOC, Guangzhou 5102.0, china 4. Faculty of Earth Sciences, china University of Geosciences, Wuhan 430074, china 5. Hainan Oil & Gas exploration company, Liaohe oilfield Petrochina, Panjin 12.010, china CAS Key Laboratory of Marginal Sea Geology South China Sea Institute of Oceanology Chinese Academy of Sciences Guangzhou China CAS Key Laboratory of Marginal Sea Geology Guangzhou Institute of Geochemistry Chinese Academy of Sciences Guangzhou China Department of Technology Shenzhen Branch of CNOOC Guangzhou China Faculty of Earth Sciences China University of Geosciences Wuhan China Hainan Oil & Gas exploration company Liaohe Oilfield PetroChina Panjin China

Independent of Indochina extrusion, the South china Sea experienced a process from passive continental rifting to marginal sea drifting. According to the fault patterns in the Beibu Gulf basin and the Pearl River Mouth basin, the continental rifting and early spreading stage from 32.to 2. Ma were controlled by extensional stress field, which shifted clockwise from southeastward to south southeastward. From 2. Ma on, the sea spread in NW-SE direction and ceased spreading at around 15.5 Ma. Integrated geological information with the assumption that the South china Sea developed along a pre-Cenozoic weakness zone, we did analogue experiments on the South china Sea evolu- tion. Experiments revealed that the pre-existing weakness zone goes roughly along the uplift zone between the present Zhu-1 and Zhu-2.depression. The pre-existing weakness zone is composed of three segments trending NNE, roughly EW and NEE, respectively. The early opening of the South china Sea is accompanied with roughly 15° clockwise rotation, while the SE sub-sea basin opened with SE extension. Tinjar fault was the western boundary of the Nansha block (Dangerous Ground), while Lupar fault was the eastern boundary of the Indochina, NW-trending rift belt known as Zengmu basin developed between above two faults due to block divergent of Indochina from Nansha. In the experiment, transtensional flower structures along NW-trending faults are seen, and slight inversion occurs along some NE-dipping faults. The existence of rigid massifs changed the orientations of some faults and rift belt, and also led to deformation concentrate around the massifs. The rifting and drifting of the South china Sea might be caused by slab pull from the proto South china Sea subducting toward Borneo and/or mantle flow caused by India-Asia collision.

关键词： South china Sea, rifting and drifting, clockwise rotation, analogue modeling, rigid massifs.

Two accumulation modes of marine-origin natural gas in the tarim Basin

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Science Bulletin 2007年第S1期 215-223页

作者： WANG HongJun1, ZHAO WenZhi1, HU GuoYi1 & HU JianFeng2.1 research institute of Petro{2. exploration and development, Beijing 100083, china 2.research institute of the tarim oilfield Corporation, Petro{2., Korla 841.00, china

Hetianhe gas field, Lungudong gas field and Tazhong gas field are marine marine-origin natural gas reservoirs in the craton area in the tarim Basin. The natural gas is generated from Cambrian source rocks. The simulation experiment indicated that the cracking of the dispersedly dissoluble organic matter remaining in the source rocks is the main origin of marine natural gas. There are two modes to form gas reservoirs, one is the dry gas reservoir such as Hetianhe gas field, in which gas accumulated on the fault belt with violent tectonic movement, the other is condensate gas reservoir formed on the inheriting uplift such as Lunnan and Tazhong gas fields. The hybrid simulation experiment of cracking gas and crude oil indicated that crude oil accumulated on a large scale in those uplift belts at the early stage, and natural gas filled the ancient oil reservoir at the late stage, and the gas reservoirs were formed after the gas mixed with the crude oil.

关键词： tarim Basin marine natural gas origin cracking accumulation

Geochemical Characteristics and Origin of Natural Gases in the Qaidam Basin,china

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Acta Geologica Sinica(English Edition) 2003年第1期77卷 103-115页

作者： ZHANG Xiaobao, HU Yong, DUAN Yi, MA Liyuan, MENG Zifang, HE Peng,ZHOU Shixin and PENG DehuaState Key Laboratory of Gas Geochemistry, Lanzhou institute of Geology, Chinese Academy ofSciences, Lanzhou, Gansu 730000 research institute of Petroleum exploration and development, Qinghai Petroleum company,CNPC, Dunhuang, Gansu 7362.0 Chinese Acad Sci Lanzhou Inst Geol State Key Lab Gas Geochem Lanzhou 730000 Gansu Peoples R China Qinghai Petr Co Res Inst Petr Explorat & Dev CNPC Dunhuang 736200 Gansu Peoples R China

Sixty-five natural gas samples were collected from 19 oil-gasfields in theQaidam basin, china. The chemical composition and carbon isotope values of the samples weremeasured, and the geochemical characteristics and origin of the natural gases were studied. Thegases can be divided into biogenic gases, sapropelic oil-type gases, mixed type oil-type gases,coal-type gases and mixed gas. The delta^(13)C_1 values of the biogenic gases are very small and theC_2.+ contents of them are very low, ranging from -68.2.per thousand to -61 .8 per thousand and0.06 percent to 0.2. percent respectively. They have heavy delta D and delta^(13)C_(CO_2., showing aCO_2.reduction pathway. They ,are distributed in the East depression region and derived from theQuaternary source rocks. The sapropelic oil-type gases have small delta^(13)C_2.values and highC_2.+ ranging from -36.6 per thousand to -2..6 per thousand and from 33.01 percent to 47.15 percentrespectively. The mixed type oil-type gases have delta^(13)C_2.values and C_2.+ contents varyingfrom -2..6 per thousand to -2..8 per thousand and from 4.81 percent to 2..06 percent *** sapropelic oil-type gases and mixed type oil-type gases are associated with oil-type oils,distributed in the West depression region and derived from the Tertiary saltwater lacustrinesapropelic source rocks and humic source rocks respectively. The delta^(13)C_2.values of thecoal-type gases are extremely high and the C_2.+ contents are very low, changing from -2..3 perthousand to -12.5 per thousand and from 0.06 percent to 18.07 percent respectively. The coal-typegases in the Nanbaxian gasfield and the Lenghu oil-gasfields in the North fault block belt arederived from the Middle Jurassic coal-measures source rocks, whereas those in the West depressionregion are derived from the Tertiary saltwater lacustrine humic source rocks. Compared with someother basins in china, the natural gases there have obviously heavier delta^(13)C due to the heavierdelta^(1

关键词： natural gas geochemical characteristics origin Qaidam basin

Hydrocarbon enrichment characteristics and difference analysis in the TZ1-TZ4 well block of the tarim Basin

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Petroleum Science 2010年第2期7卷 201-210页

作者： Jiang Zhenxue Pang Xiongqi Yang Haijun Li Zhuo Xiang Caifu Gu Qiaoyuan State Key Laboratory of Petroleum Resources and Prospecting Beijing 102249 China Basin and Reservoirresearch Center China University＂ of Petroleum Beijing 102249 China exploration and development {2. of the tarim oilfield company PetroChina Korla Xinjiang 841000 China

The reservoirs in the TZ1-TZ4 well block of the tarim Basin are complex, and the hydrocarbon enrichment shows differences. The three Carboniferous oil layers are characterized by ＂oil in the upper and lower layers and gas in the middle＂ in profile and ＂oil in the west and gas in the east＂ in plane view. In order to discuss the complex reservoir accumulation mechanisms, based on the petroleum geology and reservoir distribution, we studied the generation history of source rocks, the fault evolution and sealing, the accumulation periods and gas washing, and reconstructed the accumulation process of the TZ1-TZ4 well block. It is concluded that the hydrocarbon enrichment differences of oil layers CIII, CII and CI were caused by multiple sources and multi-period hydrocarbon charging and adjustment. The CII was closely related to CIII, but CI was formed by reservoir adjustment during the Yanshan period and was not affected by gas washing after it was formed. During the Himalayan period, different degrees of gas washing in the east and west led to hydrocarbon enrichment differences on the plane. The Carboniferous accumulation process of two-stage charging and one-stage adjustment is summarized： oil charging during the late Hercynian period is the first accumulation period of CIII and CII; oil reservoirs were adjusted into CI in the Yanshan period; finally gas washing in the Himalayan period is the second accumulation period of CIII and CII, but CI was not affected by gas washing. This complex accumulation process leads to the hydrocarbon enrichment differences in the TZ1-TZ4 well block.

关键词： tarim Basin enrichment difference multi-source and multi-period charging accumulation process

Sequence stratigraphic framework and distribution of depositional systems for the Paleogene in Liaodong Bay area

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Science china Earth Sciences 2008年第S2期51卷 1-10页

作者： ZHU XiaoMin1,DONG YanLei1,YANG JunSheng1,ZHANG Qin1,LI DeJiang2.XU ChangGui3 & YU Shui3 1 National Key Laboratory of Petroleum Resources and Prospecting,china University of Petroleum,Beijing 102.49,china 2.{2. institute of Petroleum exploration and development——Langfang,Petrochina,Langfang 065007,china 3 Technology Department of CNOOC Tianjin company,Tianjin 300452.china National Key Laboratory of Petroleum Resources and Prospecting China University of Petroleum Beijing China research institute of Petroleum {2. and development—Langfang PetroChina Langfang China Technology Department of CNOOC Tianjin company Tianjin China

With a comprehensive geological and geophysical data base,the Paleogene in the Liaodong Bay area,which consists of the Kongdian,Shahejie and Donghying Formations from the base to top,was divided into 4 second-order sequences and 8 third-order sequences based on the characteristics of the se-quence boundaries. Each third-order sequence is subdivided into the lowstand,lake transgressive and highstand systems tracts. The Lowstand systems tract (LST) is mainly composed of progradational parasequence sets,while the lake transgressive systems tract (TST) largely consists of the retrograda-tional parasequence sets and the highstand systems tract (HST) is dominated by the progradational parasequence sets. The main types of depositional systems include the shallow lake,semi-deep lake,deep lake,delta,fan delta,braided fluvial delta and nearshore subaqueous fan. The braided fluvial delta and fan delta depositional systems are mainly confined to the sequences of the lower SEs4-Ek,SEs3 and SEs1+2.while the sequences of SEd3,SEd2.and SEd1 are dominated by the delta and nearshore subaqueous fan depositional systems with the latter being developed at the downthrown side of the basin-bounding fault in each sequence. The evolution of the depositional systems is always con-trolled by the paleo-tectonic setting and the ancient landform in the space and geological time. It is concluded that the most favorable reservoirs are distributed in the Liaoxi low uplift and the central Liaozhong sag.

关键词： Liaodong Bay area Paleogene sequence stratigraphy sequence boundary depositional system

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松辽盆地岩性油藏形成条件与分布规律

石油与天然气地质 2004年第4期25卷 393-399页

作者：杨玉峰中国石油石油勘探开发研究院

松辽盆地中浅层大型坳陷湖盆河流-三角洲、湖泊沉积体系形成的砂泥岩薄互层决定了其具有形成大面积岩性油藏的地质条件。纵向上,由于各时期基准面升降造成可容空间在不同时期差别较大,因此发育的砂体类型也有一定的差别。由于储层埋藏... 详细信息

松辽盆地中浅层大型坳陷湖盆河流-三角洲、湖泊沉积体系形成的砂泥岩薄互层决定了其具有形成大面积岩性油藏的地质条件。纵向上,由于各时期基准面升降造成可容空间在不同时期差别较大,因此发育的砂体类型也有一定的差别。由于储层埋藏深度以及与烃源岩的相对位置不同,各含油组合岩性油藏成藏条件与分布规律也存在一定的差异。断层在岩性油藏成藏过程中起很重要的作用,它一方面是形成断层-岩性复合圈闭的主要要素,同时又是油气进入岩性圈闭成藏的主要运移通道。平面上,岩性油藏的类型受构造部位和砂岩的发育程度控制。凹陷中三角洲外前缘相带主要形成岩性油藏,凹陷周边是各种隐蔽油气藏发育的主要地区。

关键词：中、浅层岩性油藏主控因素分布规律松辽盆地