23 June 2014, Volume 41 Issue 3
    

  • Select all
    |
    油气勘探
  • Zhao Wenzhi; Shen Anjiang; Zhou Jin’gao; Wang Xiaofang and Lu Junming
    , 2014, 41(3): 257-267.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    Taking reef-shoal bodies developed in multiple formations in the Tarim Basin and Sichuan Basin as examples, this paper examines the origin of pores and heterogeneity of types of reef-shoal reservoirs, and tries to find out the distribution rules of various reef-shoal reservoirs. Reef-shoal reservoirs can be classified into two main types, i.e. biohermal reservoirs and grain shoal reservoirs. The former, related to reef framework, in the form of frilled platform margin, can be subdivided into interior platform reef complex and margin reef complex (sedimentary or tectonic origin). The latter, not related to reef framework, is controlled by the fluctuation of sea level on gentle slope carbonate platform, is widely developed on carbonate ramp due to the migration of shoal, and can be subdivided into interior platform shoal and platform-margin shoal on steep slopes. Reservoir space of reef-shoal carbonates was primarily formed during syngenetic and burial stages. Syngenetic porosity is controlled by original rock fabric and dissolution related to the exposure of sequence boundaries, while porosity development and distribution in burial stage is closely related to that in syngenetic stage, showing inherited features. Reef-shoal reservoirs are strongly heterogeneous, and complicated in effective reservoir distribution. Platform margin reef and biohermal shoal coexisting with reef on the top of shallowing upward sequence are main reservoirs rich in pores, the grain shoal deposited on top of shallowing upward cycle of isolated reef is also the main zone rich in pores, which usually interbeds with tight reservoir. Overall, grain shoal reservoirs are bigger in scale and better in physical properties than biohermal reservoirs.
  • Du Jinhu; Zou Caineng; Xu Chunchun; He Haiqing; Shen Ping; Yang Yueming; Li Yalin; Wei Guoqi; Wang Zecheng and Yang Yu
    , 2014, 41(3): 268-277.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    Since 2011, a giant gas field has been discovered in the Sinian and Cambrian strata in Moxi–Gaoshiti region, central Sichuan paleo-uplift, with the geological reserves reaching more than one trillion cubic meters. The main gas-bearing layers include Deng 2 Member, Deng 4 Member of Sinian Dengying Formation and Cambrian Longwangmiao Formation. Based on brief review of the exploration history of large gas province in central Sichuan paleo-uplift, the paper systematically describes the formation conditions and petroleum accumulation patterns of the giant gas field, and points out the large ancient uplift background, huge net of hydrocarbon supply system, large-scale particle shoal reservoirs and regional reservoir-cap combinations are important material conditions for the formation of the giant gas field. In view of the huge depth, high temperature, high pressure and some other complex formation conditions, a lot of efforts have been put into the research on logging, seismic, drilling, reservoir stimulation etc, and a series of accomplishments have been achieved, which work well in the exploration and development of gas in Sichuan Basin. The Sinian and Cambrian strata in the Sichuan Basin have a great potential for petroleum exploration.
  • Zou Caineng; Du Jinhu; Xu Chunchun; Wang Zecheng; Zhang Baomin; Wei Guoqi; Wang Tongshan; Yao Genshun; Deng Shenghui; Liu Jingjiang; Zhou Hui; Xu Anna; Yang Zhi; Jiang Hua and Gu Zhidong
    , 2014, 41(3): 278-293.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    The Anyue Sinian-Cambrian giant gas field was discovered in central paleo-uplift in the Sichuan Basin in 2013, which is a structural-lithological gas reservoir, with 779.9 km2 proven gas-bearing area and 4 403.8×108 m3 proven geological reserves in the Cambrian Longwangmiao Formation in Moxi Block, and the discovery implies it possesses trillion-cubic-meter reserves in the Sinian-Cambrian Formations in Sichuan Basin. The main understandings achieved are as follows: (1) Sinian-Cambrian sedimentary filling sequences and division evidence are redetermined; (2) During Late Sinian and Early Cambrian, “Deyang-Anyue” paleo-taphrogenic trough was successively developed and controlled the distribution of source rocks in the Lower-Cambrian, characterized by 20-160 m source rock thickness, TOC 1.7%-3.6% and Ro 2.0%-3.5%; (3) Carbonate edge platform occurred in the Sinian Dengying Formation, and carbonate gentle slope platform occurred in the Longwangmiao Formation, with large-scale grain beach near the synsedimentary paleo-uplift; (4) Two types of gas-bearing reservoir, i.e. carbonate fracture-vug type in the Sinian Dengying Formation and dolomite pore type in the Cambrian Longwangmiao Formation, and superposition transformation of penecontemporaneous dolomitization and supergene karst formed high porosity-permeability reservoirs, with 3%-4% porosity and (1-6)×10-3 μm2 permeability in the Sinian Dengying Formation, and 4%-5% porosity and (1-5)×10-3 μm2 permeability in the Cambrian Longwangmiao Formation; (5) Giant paleo-oil pool occurred in the core of the paleo-uplift during late Hercynian—Indosinian, with over 5 000 km2 and (48-63)×108 t oil resources, and then in the Yanshanian period, in-situ crude oil cracked to generate gas and dispersive liquid hydrocarbons in deep slope cracked to generate gas, both of which provide sufficient gas for the giant gas field; (6) The formation and retention of the giant gas field is mainly controlled by paleo-taphrogenic trough, paleo-platform, paleo-oil pool cracking gas and paleo-uplift jointly; (7) Total gas resources of the Sinian-Cambrian giant gas field are preliminarily predicted to be about 5×1012 m3, and the paleo-uplift and its slope, southern Sichuan Basin depression and deep formations of the high and steep structure belt in east Sichuan, are key exploration plays. The discovery of deep Anyue Sinian-Cambrian giant primay oil-cracking gas field in the Sichuan Basin, is the first in global ancient strata exploration, which is of great inspiration for extension of oil & gas discoveries for global middle-deep formations from Lower Paleozoic to Middle-Upper Proterozoic strata.
  • Wang Xiangzeng; Gao Shengli and Gao Chao
    , 2014, 41(3): 294-304.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    The geological characteristics of Mesozoic continental shale gas are summarized from the following aspects: shale distribution, geochemistry of shale gas, characteristics of shale reservoir, enrichment form of shale gas etc, based on the continental shale gas exploration research and practices in southeast of the Ordos Basin. The geochemical characteristics and thermal evolution degree of shale gas source rocks are controlled by the evolution of lacustrine basin in the early and middle stages of late Triassic Period, and the main hydrocarbon-generation rocks are shale from the Chang 7 and Chang 9 members of the Triassic Yanchang Formation, with high abundance of organic matter and in the mature to wet gas stage. The most mineral compositions are quartz, feldspar and clay mineral in shale gas reservoir, and the primary intergranular pores and secondary dissolution pores are the main pore types. The shale gas in the study area is oil-type gas, dominantly wet gas. The shale gas occurs mostly in the adsorption state, the free state and the dissolved state. Estimated by the volumetric method, the total shale gas resources of Chang 7 is 5 318.27×108 m3, and the total shale gas resources of Chang 9 is 3 067.29×108 m3.
  • Wang Zecheng; Jiang Hua; Wang Tongshan; Lu Weihua; Gu Zhidong; Xu Anna; Yang Yu and Xu Zhaohui
    , 2014, 41(3): 305-312.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    Through analyzing the nature and periods of Tongwan tectonization, by using seismic data, drilling data and outcrop data, the pre-Qiongzhusi Formation eroded paleo-geomorphology was described with remaining thickness and moldic methods, and the hydrocarbon accumulation conditions were analyzed. The Sichuan Basin and its adjacent areas experienced Tongwan tectonization from late Sinian to early Cambrian which include three episodes that all manifested as regional uplift and erosion, forming three disconformities. Affected by that movement, a large scale Deyang-Luzhou eroded valley in N-S direction was formed in Central-Southern Sichuan Basin. In the valley, thick Maidiping Formation and Qiongzhusi Formation are important Cambrian source kitchens; they form good source-reservoir combinations with two sets of weathering karst reservoirs in Deng 2 and Deng 4 Member in Sinian Dengying Formation, favorable for the formation of large gas field with huge resource potential. The analysis of forming mechanism and evolution history of the eroded valley shows the thrusting-fold uplifting and erosion in the second episode of Tongwan tectonization in late Sinian period, and the extensional movement in the background of rapid marine transgression in early Cambrian are key to the formation of the eroded valley.
  • Yang Ping; Xie Yuan; Wang Zhengjiang; Li Qiyan; Liu Jiahong; Zhang Di; Yang Zhi and Yin Feng
    , 2014, 41(3): 313-322.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    By taken the Sinian Dengying Formation in Northern Guizhou as an example, based on the data from homogenization temperature, salinity and density of fluid inclusions, and combined with the restoration of burial history and thermal history, this paper investigates hydrocarbonaceous fluid activity periods and restores the process of hydrocarbon accumulation and destruction. Four periods of hydrocarbonaceous fluid activity periods occurred in the research region, and they correspond to the homogenization temperature of fluid inclusions of 87.1–111.4 ℃, 126.1–163.0 ℃, 166.9–225.1 ℃ and 95.3–116.4 ℃ respectively, reflecting two stages of hydrocarbon charge, one stage of gas accumulation and gas reservoir destruction activity in Dengying Formation reservoir. Comprehensive analysis on observation of thin sections, cathodoluminescence and oxygen isotope show that, Dengying Formation reservoir developed six generations of cements, four stages of dolomite, and had four stages of dissolution, the organic acids from fluid activities in different buried environment produced multiphase dissolution on residual pores and fillings of the ancient karst. Dengying Formation in Northern Guizhou occurred three periods of petroleum accumulation which are, in order, Middle-Late Caledonian (470–428 Ma), Indo-Chinese epoch (252–228 Ma), Early Yanshanian period (177–145 Ma), and the ideal depth for the preservation of natural gas accumulation in Dengying Formationn in Northern Guizhou is about 3 600 m.
  • Feng Congjun; Bao Zhidong; Yang Ling; Si Xiong; Xu Guibin and Han Xiong
    , 2014, 41(3): 323-329.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    Taking the J19 dense well network area in the Fuyu Oilfield as a case, combined with field outcrop and modern shallow water delta sedimentary model and using coring and logging data, this paper puts forward a comprehensive analysis method for reservoir architecture of deltaic front underwater distributary channel single sand body. The causes and sedimentary evolution mechanisms for foresets of retained type, destructive type and the mixed type and for foreset sand bodies of prograding type, retrograding type and aggrading type are summarized. The calibration of rock and logging, fitting formula, dense spacing wells and pair wells data are used to ascertain the foresets and foreset sand bodies. The models of three-dimensional reservoir architecture are set up. The analysis of remaining oil shows that foreset controls the vertical distribution of the remaining oil, while in the internal of the foreset sand bodies, the remaining oil is enriched in the updip direction.
  • 油气田开发
  • Deng Shiguan; Lü Weifeng; Liu Qingjie; Leng Zhenpeng; Li Tong; Liu Hongxian; Gu Hongjun; Xu Changfu; Zhang Xuhui and Lu Xiaobing
    , 2014, 41(3): 330-335.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    Taking the conglomerate from Xinjiang Oilfield as study object, the porosity distribution characteristics of the conglomerate were analyzed with CT scanning; through the online monitoring of the water and polymer flooding process in a conglomerate core using an CT scanning system, the saturation profile along the core and the CT reconstructed images of core section during the displacing process were obtained; oil displacement mechanism was analyzed according to a new characterization parameter, “oil saturation frequency distribution”. The results show that the conglomerate has strong heterogeneity, resulting in “preferential channels”, and in turn ineffective water circulation and low water flooding oil recovery, moreover, the oil in high oil saturation area is produced first. In polymer flooding, the oil in high and medium oil saturation areas can be produced but the oil in low oil saturation areas still cannot be produced. Oil produced in the subsequent water flooding is still mainly from the high oil saturation areas. For conglomerate reservoirs, previous water flooding should reach as high water cut as possible so as to strengthen the slug effect of the polymer. Meanwhile the injection volume of polymer should be reduced, and a subsequent water flooding should be used to push the polymer slug to produce oil.
  • Cheng Wan; Jin Yan; Chen Mian; Xu Tong; Zhang Yakun and Diao Ce
    , 2014, 41(3): 336-340.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    Based on the analysis of the stress fields near the hydraulic fracture tip and on the natural fracture surface, a criterion for identifying hydraulic fractures crossing natural fractures was proposed. A series of hydraulic fracturing tests were conducted to investigate the influences of natural fractures occurrence and horizontal stress contrast on hydraulic fracture propagation using large scale tri-axial fracturing system. The experiment results showed that the crossing happens in the region with high approaching angle and strike angle, large horizontal stresses and horizontal stress difference coefficient. Horizontal stress contrast has a critical value, only when it is above the critical value, may the hydraulic fracture cross the natural fracture. These experimental results agree with the predictions of this criterion well. It is predicted by this criterion that the hydraulic fracture of a test well in the Longmaxi shale formation, Sichuan Basin, can’t cross the natural fracture, which agrees with the micro-seismic monitoring results.
  • Yuan Zixue; Wang Jingyun; Li Shuxun; Ren Jihong and Zhou Mingqing
    , 2014, 41(3): 341-348.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    The methods of estimating recovery factor of newly added measured reserves in existing petroleum reserves standardization of China are unsuitable for sandstone oil reservoirs of extra-low permeability with water flooding, so new empirical formula method and analogous method for estimating recovery factor of the reservoirs are studied. The key parameters influencing recovery factor are permeability, formation oil viscosity, porosity, mobility and well spacing density. Based on the requirements such as longer development time, reliable reserves and available reservoir parameters, 37 sandstone oil reservoirs of extra-low permeability were selected, and 19 recovery factor models were summarized. With consideration of high multiple regression coefficient and low standard error, 4 empirical formulae suitable for reservoir of water-flood development with vertical well were established. Comparison of calculated results from the empirical formulae and calibrated recovery factors of PetroChina recently shows that the formulae match well. It is important to choose reservoir with successful pilots and/or developed in large scale as benchmark reservoirs in the analogy estimation. Based on the principle of keeping consistent of analogous method with production performance, a practical example of Chang 8 reservoir, Triassic, FX oilfield was given to illustrate the determination of recovery factor of extra-low permeability reservoir. Empirical formula method and analogous method have their advantages and disadvantages, reserves estimators should pay great attention to the reliability of data, to application condition for empirical formulae method and to the avoidance of single reservoirs in analogous method.
  • 石油工程
  • He Mingfang; Ma Xu; Zhang Yanming; Lai Xuan’ang; Xiao Yuanxiang and Hao Ruifen
    , 2014, 41(3): 349-353.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    Sulige gas field is a typical low-permeability reservoir in China. According to desert landform features along with the regional hydrologic feature and the existing fracturing technology and operational conditions, a factory-like fracturing method suitable for Sulige gas field is established to improve techniques and production organization. This method includes five key parts: (1) centralized water supply mode (water source well supply+artificial lake storage); (2) highly efficient fracturing process (two mature multi-stage fracturing technologies, sliding sleeve fracturing for vertical wells and open-hole packer fracturing for horizontal wells); (3) pipeline operation mode with seven procedures, including well drift and flushing perforation etc; (4) high efficiency operation equipment; (5) recovery of fracturing flow-back fluid. This method shortens the preparation and operation period of fracturing treatment and also relieves the pressure on environment. Pilot tests were carried out in 11 well groups in total. Sixty-seven stages of fracturing in 14 wells were successfully completed within 42 days, representing a reduction of fracturing operation cycle of more than 50%, and an encouraging improvement in efficiency.
  • Liu Xiushan and Su Yi’nao
    , 2014, 41(3): 354-358.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    The well deviation equation of circular-arc trajectory in space was established, the solution methods to determine the posture of the inclined plane that the circular-arc trajectory lies on and the extreme value of inclination angle of the circular-arc trajectory were presented, and the evolution pattern and control mode of well deviation for circular-arc trajectories in space was revealed. Some parameters can be calculated by the forward model and inverse model respectively, including the inclination angle and azimuth angle at any point along a circular-arc trajectory, the inclined angle and inclined azimuth angle of the inclined plane that the circular-arc trajectory lies on and the various parameters at the point with extreme inclination angle, and the calculated results from the forward model are the same as those from the inverse model. There are two points with extreme inclination angles along a circular-arc trajectory or its trendline, and the tangent lines of wellbore trajectory at the points with minimum and maximum inclination angles point to downdip and updip directions of the inclined plane respectively, the bending angle and azimuth angle differences between the two points are both 180°. The posture of inclined plane and parameters at extreme inclination points relate to the inclination angle and tool face angle at the beginning point of well interval, but have nothing to do with the interval length. The inclined angle mode for controlling a circular-arc trajectory is ambiguous, so the tool-face angle or directional azimuth angle modes should be used.
  • Yin Bangtang; Li Xiangfang; Sun Baojiang and Zhang Hongquan
    , 2014, 41(3): 359-366.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    Based on the classification and flow behaviors of two phase flow in wellbore annuli, the hydraulic models for slug flow and annular flow in annuli for vertical or inclined wells were established, and the flow regime transition criteria were also obtained. Based on the flow behavior research of multiphase flow in wellbore annuli, the liquid film zone was used as the control volume, and the effect of the tubing liquid film, casing liquid film and the droplets in gas core area on the mass and momentum transfers were considered. The mass and momentum conservation equations of slug and annular flows were obtained. Then the evaluation criterion of flow pattern transitions were established, including dispersed flow to slug flow, bubble flow to slug flow and slug flow to annular flow. The model prediction results were compared under the experimental conditions from the previous literatures. The predictions of flow pattern, liquid holdup and pressure gradient were compared between the new model and the pipe flow model modified by using the hydraulic diameter. The results show that the flow pattern, liquid holdup and pressure gradient can be predicted by the new model more accurately, and the prediction of liquid holdup and pressure gradient are better.
  • 综合研究
  • Zhang Hong; Zhang Shuichang; Liu Shaobo; Hao Jiaqing; Zhao Mengjun; Tian Hua and Jiang Lin
    , 2014, 41(3): 367-374.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    By analyzing the relationship between throat threshold and fluid forces of oil charge in tight reservoirs and according to the oil-charging mechanical conditions, the lower limits of throat at the interface between source and reservoir rocks and in the middle of reservoirs were determined theoretically. On the basis of Young-Laplace formula and the equilibrium between driving forces and capillary resistance, the threshold models were set up by using the maximum driving forces near the source-and-reservoir interface and inside reservoirs respectively. They were applied to the Yanchang Formation in the Ordos Basin, the middle-lower Jurassic in the Sichuan Basin and the Bakken Formation in the Williston Basin in America. The corresponding results near the interface are 15.74 nm, 29.06 nm, and 14.22 nm, and the ones in the middle of reservoirs are 39.45 nm, 37.20 nm, and 52.32 nm respectively. Accordingly, the threshold permeabilities of the three typical tight oil reservoirs calculated are 0.002 1×10-3 μm2, 0.006 1×10-3 μm2, 0.001 8×10-3 μm2 near the interface and 0.010 0×10-3 μm2, 0.009 4×10-3 μm2, 0.016 9×10-3 μm2 at the inner reservoirs. The rocks near the interface are complex, so there is a poor correlation between porosity and permeability, while inside reservoirs, homogeneous lithology results in good correlation between porosity and permeability. The porosity thresholds were determined as 2.16%, 2.00% and 3.50% respectively.
  • 学术讨论
  • He Xunyun; Shou Jianfeng; Shen Anjiang; Wu Xingning; Wang Yongsheng; Hu Yuanyuan; Zhu Yin and Wei Dongxiao
    , 2014, 41(3): 375-384.
    Abstract ( ) Download PDF ( ) Knowledge map Save
    The trace elements, rare earth elements (REE), carbon and oxygen isotopic compositions and strontium isotopes were analyzed to study systematically the geochemical characteristics and origin of the middle assemblage dolomites from the Ordovician Majiagou Formation Member 5 in the Jingxi area (the west of Jingbian Gas Field). The analytical results of samples demonstrate that the MgO and CaO contents of the middle assemblage dolomite are negatively correlated, and the Mg/Ca values are high; the dolomites are characterized by high Fe content, relatively high Mn content and low Sr and Na content, while part dolomites have low Fe and Mn content but high Na content; the dolomites have very low REE content and similar REE distribution patterns, which are generally characterized by enrichment of light REE, losses of heavy REE, obviously negative anomaly of Eu and weak negative anomaly of Ce; The δ13C values of dolomites are consistent with those of the coeval seawater, while most of the δ18O values of dolomites are more negative than those of the coeval seawater; most of the 87Sr/86Sr values of dolomites are significantly higher than those of the coeval seawater while only a few are close to those of the coeval seawater. Combined with the geological setting and geochemical characteristics of the middle assemblage dolomites, the middle assemblage dolomites of the Majiagou Member 5 are probably the origin of seepage reflux dolomitization, and were superimposed by burial dolomitization during the burial period. The eastern part of the Jingxi area is favorable reservoir development area, the favorable area can extend eastward.