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Table of Content

    25 March 1998, Volume 19 Issue 1
    A NEW METHOD FOR QUANTITATIVE PREDICTION OF TECTONIC FRACTURES—TWO-FACTOR METHOD
    Ding Zhongyi, Qian Xianglin, Huo Hong, Yang Youqing
    1998, 19(1):  1-7,14.  doi:10.11743/ogg19980101
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    The quantitative prediction technique of tectonic fractures is an urgent subject in the exploration and development of fractured reservoirs.In the present paper,rock fracture method and energy method are used to simulate tectonic fracture development in Qiuling Oilfield of Turpan Hami Basin.The results from both the rock fracture method and the energy method are complementary each other.Thus,a new method—two factor method is proposed to simulate the development of tectonic fractures by means of fracturs value and energy value together.According to this method,a fitting formular predicting the fracture density through calculating fracture value and strain energy is given.A comparison of the predicted fracture densities with the corresponding observed ones of 16 wells was made,the results show that the relative errors of 12 wells are less than 25%.On this basis,the predicted diagrams showing the density distribution of tectonic fractures within the producing formations of the Qiuling Oilfield are presented.

    DEVELOPMENTS IN PETROLEUM GEOLOGY: REVIEW AND LOOK AHEAD
    Zhao Zhongyuan
    1998, 19(1):  8-14.  doi:10.11743/ogg19980102
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    Long ago’ people had known that oil and gas are fluid and organic minerals.The organic nature of oil and gas hints us where they might be,and the fluidity tells us how to search for them.The petroleum geology which records the human knowledge on the role of oil and gas distribution,however,had not developed around these two properties but along another way which was in keeping with the process of human cognition.People primarily knew the oil and gas starting from where they are now,for example,the earliest wells for oil or gas always drilled close by oil or gas seepage,and then,people found that oil and gas always distributed along a certain linear structure,or especially occurred in anticline structures as the anticlinal theory of petroleum accumulation was proposed;or within a tectoic province,known as petroliferous province.Aferwards there was a great leap in the process of human cognition when pepole differentiated the sedimentary basin from other tectonic unit in the petroliferous province,thus knowing that the basin is the only place suiting the formation of hydrocarbon.But the problems that what role would the fluidity of oil and gas play in pool formation,and what kind of principle would they follow,and how to utilize it for exploration still remain unsolved.Therefore,turning oil and gas exploration to basin merely shows that people have found the place where the oil and gas are being,but how to discover them is still remains discussing.

    FRACTAL GEOMETRY DESCRIPTION OF RESERVOIR PORE STRUCTURE
    He Chengzu, Hua Mingqi
    1998, 19(1):  15-23.  doi:10.11743/ogg19980103
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    That the grain sizes are between 0.2~50 μm have fractal property.Acoording to the principle of the fractal geometry,the expressions of pore size distribution curve,capillary pressure curve,J function curve,relative permeability curve and equilibrium contact angle of the reservoir rocks could be derived.Leverett.et.al show that the reservoir rocks with the similar properties have unique J fanction curve.The expression derived for J function curve indicates that the reservoir rocks of this kind have the similar fractal dimension and pore tortuosity.The expression of the capillary pressure and J function curve could be used to calculate the fractal dimension of the reservoir rock pore structure and its change after the water sensitivity or acidizing.This method is simpler than scanning electron microscopy.

    SIMULATION EXPERIMENTS OF EXPULSION EFFICIENCY FROM COAL-FORMED OIL
    Dai Qinglin, Hao Shisheng, Lu Shuangfang
    1998, 19(1):  24-28.  doi:10.11743/ogg19980104
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    Simulation experiments of primary or oil-added source rocks(some oil was added into source rock)have been conducted.The oil expulsion efficiency and mechanism of coal at different oil saturations,temperatures,pressures,time and water saturations have been systematically studied and compared in detail with those of mudstone.The results indicate that coal-formed oil could expel its mother souree,and its expulsion efficiencies are about 5%~25%,which is 10% lower than those of mudstone at the same conditions.

    DEGRADATION OF ANAEROBIC BACTERIA IN CRUDE OIL AND ITS PRODUCT PROPERTY
    Li Zanhao, Li Ji, Xiang Longbin, Xia Zunyi, Zhang Yuancheng
    1998, 19(1):  29-34.  doi:10.11743/ogg19980105
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    It is universal that both the anaerobic bacterial degradation and oxidative bacterial degradation of crude oil exist in the hydrocarbon evelution.They do not only distroy some hydrocarbons,but also reproduce some new hydrocarbons,and even result in new hydrocarbon pools for exploration.A lot of shallow transitional gas pools actually resulted from anaerobic degradation.The products of the anaerobic bacterial degradation of crude oil possess light methane carbon isotope(δ13C1<-5.5%),very light ethane carbon isotope (δ13C2<-4.0%)and the negative anomaly of carbon isotope of separate hydrocarbons (δ13Cn<-3.7%~-5.3%).Natural gas produced in central Tarim Basin contains at least 20% bacterial degrated methane.

    NONTECTONIC FRACTURED SANDSTONE RESERVOIRS OF UPPER TRIASSIC IN MIDDLEWEST SICHUAN BASIN
    Wang Honghui, Lu Zhengyuan
    1998, 19(1):  35-41.  doi:10.11743/ogg19980106
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    The fractures in Upper Triassic sandstones in middle west ares of Sichuan Basin has controlled the reservoiring and penetration of fluids.The fracture forming mechanism in Upper Triassic of the area is mainly nontectonic origin,including differential compaction,corrossion,karst collapse and gravity sliding.The top and upper parts of paleo unaka are favourable places for nontectonic fracture system,thus they are perfect places for both test wells and development wells.

    FUZZY RECOGNITION SYSTEM OF LOGGING-SEDIMENTARY FACIES FOR CARBONATE ROCKS
    You Zhanglong, Wang Xuyan
    1998, 19(1):  42-48.  doi:10.11743/ogg19980107
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    The fuzzy characters of log layering and log parameter distritution are difficult problems in log-sedimentary facies recognition of carbonatite section of Carboniferous Huanglong Formation in East Sichuan.Based on the introduced conception of subordinate function,the fuzzy recognition system of log-sedimentary facies of carbonatite section is deveolped according to the principle of fuzzy recognition and fuzzy expert dicision.The results of three wells’recognition of the sedimentary microfacies of Huanglong Formation show that the rate of correct recognition of the system is up to 85%,which brings it a bright application prospect.

    CHARACTERS AND ORIGIN OF TAR MATS IN YAHA OIL-GAS FIELDS,TARIM BASIN:FEATURES OF HYDROCARBONS AND ORIGIN OF TAR MATS
    Zhang Min, Zhang Jun
    1998, 19(1):  49-52,58.  doi:10.11743/ogg19980108
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    The characteristics of saturated hydrocarbons and n alkane hydrocarbons of reservoir core extracts and crude oil in Yaha oil and gas fields in Tarim Basin are analyzed and studied systematically in this paper,the results show similarities in n alkane distribution,biomarkers distribution and their combined characteristics of saturated hydrocarbons as well as geochemical characteristics of aromatic hydrocarbons for tar mats,oil sand,asphaltic sandstone and crude oil.These characteristics suggest that hydrocarbons of these samples originated from the same source rocks.However,geochemical characteristics of tar mats reveal that the formation mechanism of tar mats is the intrusion of gases which results in the deposition of asphaltene in crude oils.

    PALEOZOIC RESERVOIR-CAP COMPLEX AND EVALUATION IN SOUTH ORDOS
    Wu Xichun, Li Peihua, Zhang Fuli, Yuan Weiguo
    1998, 19(1):  53-58.  doi:10.11743/ogg19980109
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    Following reservoirs of Lower Paleozoic in South Ordos are prospective for oil and gas exploration:dolomite intercrystalline pore reservoir of Middle Cambrian Zhangxia Formation;dolomite corroded pore and vug reservoir of tidal flat facies of Lower Ordovician Liangjiashan Formation;gypsum cast corroded pore and vug reservoir of supratidal flat facies of the 3rd and 5th Members of Lower Ordovician Majiagou Formation;the interlayer karst weathered crust karst reservoirs of the 2nd~4th Members of the Upper Majiagou Formation;dolomite reservoirs of marginal reef bank complex of Middle Ordovician Pingliang Jinghe Formations.The shale and coal series of Upper Paleozoic Benxi~Taiyuan~Shanxi Formations serve as regional cap rocks.Five reservoir cap rock complexes have been recognized,and within the seven prospecting target blocks in South Ordos,the first and second blocks have the best reservoir cap rock assemblages.

    A NEW METHOD OF BUILD-UP PRESSURE DATA INTERPRETATION FOR LOW PERMEABILITY GAS WELLS
    Guo Kangliang, Zhou Lijuan
    1998, 19(1):  59-62.  doi:10.11743/ogg19980110
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    Early-time pressure build-up data of low permeable gas reservoirs,affected by fluid phase changs and non-Darcy effect,can not be used in pressure data interpretation.In this paper,a new method is developed in which phase change is used as the condition,and Duhamel’s principle is used to derive formation pressure equation and then calculate the formation pressure in low permeability wells with early time data,and use this pressure as a match point to match the early time data,thus getting the formation parameters.It has been proved by practice that the parameters obtained by this method possess high reliability.

    STRUCTURAL FRAMEWORK AND EVOLUTION OF BOHAI BAY BASIN
    Li Jun, Wang Xiepei
    1998, 19(1):  63-67.  doi:10.11743/ogg19980111
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    An unique structural framework of Early Tertiary exists in Bohai Bay Basin,its radiate fault system and circular fault system are distributed around Bozhong Depression.The framework resulted from mantle diapirism.The Bohai Bay Basin has undergone two faulting thermal contraction stages ever since Early Tertiary.When the mantle swelled initially,the earth crust thinned,the basin began its faulting-controlled subsidence.Then the mantle’s temperature decreased,the basin entered its thermal contraction subsidence.

    POOL-FORMING CHARACTERS OF COMPLEX FAULT-BLOCK OIL AND GAS FIELDS IN DONGXIN
    Jiang Youlu
    1998, 19(1):  68-73.  doi:10.11743/ogg19980112
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    China’s largest complex fault-block oil and gas fields-Dongxin oil and gas fields possess sufficient oil and gas sources and well developed reservoir rocks.The inherited uplift helts developed there are favourable for hydrocarbon accumulation.Multi stage faultings resulted in active vertical migration of oil and gas.During bady faulting,hydrocarbons were injected upward along the faults;during stable stage,faults closed gradually,and hydrocarbon that entered shallow strata migrated along the faults to form secondary oil and gas pools,thus forming vertical multi layer hydrocarbon assemblayes.The pools imbricated and formed oil pooloil-gas poolgas pool sequences in ascending order.

    RESERVOIR CHARACTERS OF CLASTIC ROCKS FROM FIRST MEMBER OF KONGDIAN FORMATION, WANGGUANTUN OIL-FIELD
    Wang Zhenqi, He Zhenmin, Xu Long, Zhang Changmin, Zhao Mingyue
    1998, 19(1):  74-79.  doi:10.11743/ogg19980113
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    According to the description of cores,conventional thin sections,injecting thin sections,SEM observation,X-ray analysis of clay minerials and pattern analysis of pore structure,it is found that the heterogeneity and physical property of the sandy river bed,sandbar deposit,conglomeratic river bed,flood plain deposit and debris flow deposit gradully increase and vary worse and wores.Based on the relationship between pore throat types and rock fabric,six types of reservoir pore structure models could be established.The pore structure models of type-Ⅰ and type-Ⅱ reservoirs are mainly primary intergranular pore and solution pore types;that of type-Ⅲ are solution pore micropore types;that of type-Ⅳ is interstitial material micropore type.

    AN EXAMPLE OF DETECTING HYDROCARBON MICROSEEPAGE BY BOTANICAL ANOMALY
    Wang Jinyi, Yu Qixiang, Zeng Huasheng, Liu Xiaoke
    1998, 19(1):  80-82.  doi:10.11743/ogg19980114
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    Hydrocarbon microseepage could result in trace element content anomaly of ground plant.The ground plants above the hydrocarbon pools of Yakela in North Tarim and Lunpola in North Tibeit grow poorer than those of the neighbouring areas,and their abundances of Li,Fe,Mn,Ni are usually higher than those of the later,but their abundances of Rb,Ca,Sr,Ba are lower than those of the later.This correspounds well with the geochemical exploration anomaly in the study areas.

    ORIGIN OF DOLOMITES IN DENGYING FORMATION, UPPER SINIAN,SUIZHOU,HUBEI
    Hu Mingyi, Xiao Chuantao, Gong Wenping
    1998, 19(1):  83-84,89.  doi:10.11743/ogg19980115
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    The Late Sinian Dengying Formation at Xiejiadian in Suizhou,Hubei Province is dominated by deep-water carbonate deposits of slope basin facies.Dolomitas develoved well in study area,and are characterized by fine crystals,poor crystal forms,stable lateral distribution and well horizontal lamination.The isotope analysis of carbon and oxygen show that the salinity decreases with the increase of water depth,indicating that the dolomites were the products of penecontemporaneous dolomitization,the Mg2+ was dervied from high salinity water in platform.According to above mentiioned,model of dolomitization has been established.

    BREAKING THE SINGLE MODLE OF THINKING IN GEOLOGICAL RESEARCHES
    He Ziai
    1998, 19(1):  85-88.  doi:10.11743/ogg19980116
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    In China,geological research thinking has been formed a single modle.That is to say,the accumulative research mode predominated by induction play the main part,and the suceessive transformation is emphasised from the image to abstract thought.But the geological phenomeana which are the basis of all research reasoning are only the relics remaind during the evolution of geological history,thus the role which is intrinsic strength of induction thinking is restricted.The modle in research thinking must be breaked,the deduction thinking enhanced and the effect of the non-logic thinking developed when logic breakup befor the research thinking in geology can be produced activity and transformed from single-dimension to multi dimension,traditional type to opening type.