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Table of Content

    25 September 2000, Volume 21 Issue 3
    GENESIS OF CENOZOIC BASINS IN NORTHWEST PACIFIC MARGIN(2): LINKED DEXTRAL PULL-APART BASIN SYSTEM
    Xu Junyuan, Zhang Linyun
    2000, 21(3):  185-190.  doi:10.11743/ogg20000301
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    Based on the premise of plain strain thinned crust for the first order approximation,the paleo tectonics of northwest Pacific margin at the beginning of collision between Indian and Eurasian Plates have been reconstructed in this paper.The suture between the two plates was located at 26° southward,the north coast of South China Sea at about 14° southward,the north coast of Japan sea at about 4.5° south and Southwest Japan Island at about 8.5° south to the their present positions respectivily.The collision of Indian Plate and Eurasian Plate accelerated the north retreat of Eurasian Plate,caused right shear along the margin from Sumatera to Far East of Russia and the opening of marginal basins including South Chian Sea,Sulu Sea,Celebes Sea,Philippine Sea,Japan Sea,Okhotsk Sea and so on.These basins constituted a huge chain dextral pull-apart rift system in order to be balanced kinematically,Qinling and Bajkalj Stanovoj was the derived sinistral R′fault belt.Globally,the north retreat of Eurasia Plate possibly harmonized with south shift of North American Plate,and in the east margin of Pacific Plate,San Andreas Fault took dextral displacement.

    EFFECT OF WAVELET EXTRACTING WITH A SEISMIC TRACE NEAR WELL BASED ON NORMAL INCIDENCE ASSUMPTION AND ITS IMPROVING METHOD
    Ma Jingfeng, Zhang Zhongwei, Wang Jiamin
    2000, 21(3):  191-196.  doi:10.11743/ogg20000302
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    Wavelet extracting is the essential technique of impedance inversion.A wavelet is generally extracted based on the assumption of normal incidence by the deconvolution of reflectivities obtained from well log with a seismic trace near the well.But actural seismic waves do not always strike a interface normally,and the reflectivities change with offset.Therefore,there must be considerable differences between the reflectivities obtained and the real ones.In this case,a newly derived recursion formula for calculating reflection coefficient by slope incidence is proposed in this paper,and it could improve the acuracy of wavelet extracting and impedance inversion and seismic interpretation.The result of model calcultion has proved that the accuracy of wavelet extracting and the result of deconvolution have been improved.

    RELATIONSHIP BETWEEN OIL(GAS)SATURATION AND MIGRATION
    Wang Zhixin, Zhang Yiwei
    2000, 21(3):  197-200,213.  doi:10.11743/ogg20000303
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    The viewpoint that oil and gas in rocks can migrate only when they reach certain threshold is not correct.The primary condition for oil and gas migration(secondary migration)is that the dynamic force must be greater than capillary resistance and fractional resistance.The dynamic force includes hydrodynamic force and buoyancy,both of which are related to the length of oil and gas phases.That is to say,oil and gas can migrate so long as the length of oil or gas phase is sufficient.This suggests that there is no inevitable relationship betwee oil and gas migration and saturation.It is pointed out that differental pressure greater than 10 MPa between the two ends of the oil or gas phase is needed to cause the migration.Only sudden event can produce such differential pressure but not formation residual pressure.When dynamic differential pressure is certain,the reservoir's pore texture and wettability remain invariable,water driving oil may reach stable residual oil saturation.But the residual saturation would change with the variation of water driving condition.So it is considered that oil and gas can migrate or not is determined by the lengh of continuous oil(gas)phase but not the oil saturation.

    SPACE-TIME RELATIONSHIP BETWEEN TECTONICS AND SEDIMENTATION OF MESO-CENOZOIC BOHAI BASIN
    Hou Guiting, Qian Xianlin, Cai Dongsheng
    2000, 21(3):  201-206.  doi:10.11743/ogg20000304
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    The main structural characteristics of the Bohai Basin is that synsedimentary growth faults widely developed in the basin.These faults are mainly tensile and tenso-shear ones and the structural types includes extensional,strike slip and inversion structures.Great thickness of continental deposits developed in the Meo-Cenozoic Bohai Basin.The Tertiary Period was the principal fault depressed stage.The fourth member of the Shahejie Formation and the Kongdian Formation of the Lower Tertiary scattered incompletely and the basin was small and narrow;She-3 member and the Dongying Formation were distributed extinsively and the basin extended wider.The Upper Tertiary System developed well,the depocenter was formed in the central part of the basin.According to the analysis of structural sedimentary environment,the sedimentry facies of the west of Bohai Basin was controlled by NW directional faults while that of the east region was controlled by NNE directional structures.The major growth index of faults that controlled the the basin indicates that there were three peak stages of fault activities:the Mesozoic,Sha-3 sedimentary stage and Dongying stage.The Sha-3 sedimentary stage was the most intensive stage both for tectonic activities and sedimentation.

    COMPLEX PETROLEUM SYSTEM AND MULTICYCLE BASIN IN TARIM
    He Zhiliang, Mao Hongbin, Zhou Xiaofeng, Gong Ming, She Xiaoyu
    2000, 21(3):  207-213.  doi:10.11743/ogg20000305
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    The evolution history of multicycle in Tarim Basin is determined by long distance drifted small plates,complicated basement and complex tectomic activities of the neighbouring plates.The basin underwent four evolution stages such as Paleoasian Ocean,Paleotithys Ocean,Mesotithys Ocean and Neotethys Ocean,which resulted in a milti-prototype basins,the superimposition in which the basin united as a whole at first,then disintegrated later and reunited again at last with variable thermal regime.The multicyclic evolution of the basin resulted in multiple petroleum system,multi set of souce rocks,multiple oil generating depression,multi-stage of oil generation,multi-type of reservoiring spaces,multi-type of sealing and covering system,complex passage networks and multi-type of trap system.The reformation,resealing and preservationg of post formation of oil and gas led to complicated hydrocarbon pool-forming history in multiple hydrocarbon accumulation belts.On this basis,oil and gas exploration in Tarim Basin from now on should aim at the discovered oil and gas fields,increase reserves and expand exploration realm.

    DEVELOPING BOTTOM WATER POOLS WITH HORIZONTAL WELL
    Chen Zhihai
    2000, 21(3):  214-219,231.  doi:10.11743/ogg20000306
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    Taking a water bottom reservoir in Tarim Basin as an example,the results of developing the reservoir with horizontal well and vertical well are compared and studied in this paper.The results prove that horizontal well development is superior to the vertical well development.Then the mode of developing the reservoir with horizontal well according to reservoir engineering,physical test and reservoir numeric simulation were studied.A new method of calculating critical production and critical bettom flowing is proposed.It is suggested that,in developing water bottom reservoir with horizontal well,one should pay attention to the effect of horizontal and vertical permeability,and that different primary allocations may have different effects on developing results.The horizontal section of the horizontal well should be limited within 70%~90% of the relative thickness of oil layer.

    STUDY ON SEQUENCE STRATIGRAPHY OF PENGLAIZHEN FORMATION IN XINCHANG,WEST SICHUAN AND RESERVOIR LATERAL PREDICTION
    Wei Limin, Liu Meiqing
    2000, 21(3):  220-225.  doi:10.11743/ogg20000307
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    Based on drilling,logging and seismic data,principles of high resolution sequence stratigraphy and correlation method using datum cycle as reference framework are used in this paper.Five drilling datum mid-term cycles and five corresponding seismic sequences are recognized and the framework of high resolution sequence stratigraphy correlation is established in Penglaizhen Formation of Upper Jurassic in Xinchang of West Sichuan Depression according to formation denudation phenomena,remained deposits,short-term cycle superimposed pattern,seismic reflection end type and important variation of reflective character.It is pointed out that the main body of Penglaizhen Formation deposited in the position of transititional part from deltaic subwater-plain to river mouth bar during the process of late descending-early rising of the mid-term datum and mostly occurred in both sides of sequence boundary.Seismic response of the gas-bearing sand bodies was used for lateral prediction.Consequently,the accuracy of predicting time-space distribution of the favorable sand bodies and description of smaller sand bodies is significantly increased.

    SELECTING EXPLORATION TARGETS ACCORDING AS OIL-PROVIDING CONDITION IN JIZHONG REGION
    Li Bo, Liang Xingru, Huang Hairong, Wang Zhisheng, Li Jie
    2000, 21(3):  226-231.  doi:10.11743/ogg20000308
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    There are two kinds of oil supply ways in the Tertiary clastic rock oil reservoirs in Jizhong Region:one is fractured surface supply oil;the other is bedded permeable layer supply oil.Oil diverting faults did not only control trap formation and reservoir distribution,but also controlled the migration paths.The bedded permeable layer supply oil is controlled by structural hights,the migration paths are usually the counter lines of vertical structures,and oil migrates towards the height of noze structure along the noze bridg.The traps along oil and gas migration paths are favourable for hydrocarbon pool formation.It thus suggested that the middle and the lower parts close to oil diverting fault and the bridge of the noze structure are most favourable for future rolling exploration.

    ANALYSIS ON HYDROCARBON POOL-FORMING CONDITION OF CENTRAL DIAPIRIC ZONE IN YINGGEHAI SEA BASIN
    Gong Shaobo, Wang Yan
    2000, 21(3):  232-235.  doi:10.11743/ogg20000309
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    Yinggehai Sea Basin is situated in the west of Hainan Island and the east of Zhongnan Peninsula and stretches in NW-SE direction.The basin consists of central diapiric zone and a slope zone.Two sets of source rocks including Miocene Yinggehai,Huangliu,Meishan and Sanya Formations and Oligocene Yacheng Formation developed in the diapiric zone.Oil threshold is between 2 800~3 000 m depth.The traps were formed by the upward arch of diapiric fluid,and episodic diapir activity determined hydrocarbon episodic migration.Different migration dynamic forces resulted in different types of oil and gas pools:under high temperature,high pressure and uncompaction,the Miocene source rocks formed high pressure pocket which break overlying strata and formed deep and shallow gas pools;deep seated inorganic CO2 under high pressure expelled the hydrocarbon gas near fractures,destoried the original gas pools and formed new hydrocarbon gas pools with little Co2.

    EVIDENCE AND CHARACTERISTICS OF OIL AND GAS VERTICAL MICRO-MIGRATION
    Cheng Jun, Liu Congxi, Zhao Kebin, Guo Xusheng, Yang Zhibin
    2000, 21(3):  236-240.  doi:10.11743/ogg20000310
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    Hydrocarbon vertical micro-migration is a complicated geological-geochemical process.It is strictly controlled by boundary condition,possesses stages in geological history.The mineralization degree of ground water shows gradient variation and ionic combinatiom changes due to the action of ground water and hydrocarbon during the vertical micro-migration.Hydrocarbon vertical micro-migration can change the ion combination,causes regular variation in component of light hydrocarbons and the fluorescent intensity of aromatic hydrocarbons.That is to say,light hydrocarbons with small molecular weight and small radius relatively increases from reservoir to the caprocks,but the fluorescent intensity of aromatic hydrocarbon decreases distinctly,and the carbon isotopic value of methane of both deep seated reservoir and groud surface are basically the same.Since hydrocarbon vertical miero migration is periodical and intermittent,the geochemical index usually in cycles from high to low or from low to high on geochemical exploration index colunm.

    SPECIAL SEQUENCE STRATIGRAPHIC MODEL IN NORTH SLOPE OF BAIYUN SAG
    Yang Fei, Wei Fujun, Peng Dajun, Pang Xiong, Wang Lin, Liu Jian
    2000, 21(3):  241-243,267.  doi:10.11743/ogg20000311
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    The north slope of Baiyun Depression possesses a special sequence stratigraphic model.Its stratigraphic gradient is lower and has no shelf break.Fault activities make the throw of fault acting as shelf break,and cause its lowstand system trace to have the characteristics of type-1 sequence of steep slope.The slope consists maimly of basin fan,incised valley and fillings.This new sequence stratigraphic style is called fault controlled type-1 gentle slope sequence.

    SEQUENCE STRATIGRAPHY AND SOURCE-RESERVOIR CAP ROCK ASSEMBLAGE OF QDN BASIN
    Zhou Xiaoying, Wei Kuisheng
    2000, 21(3):  244-248.  doi:10.11743/ogg20000312
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    QDN Basin is an extensional basin which fractured first and then depressed.The basin could be divided into 5 second order sequences and 19 third-order sequences.The basin's chronostratic framework was built according to basin's evolution history and formation characteristics.Two source reservoir cap rock assemblages were discovered in the basin.The lower assemblage consists of several source beds such as lake and transitional facies of the Eocene Series and Yacheng Formation;the reservoirs are mainly fan delta,sand beach,sand bars,foreset wedges and slope fans.The source rocks of the upper assemblage are the dense section of Meishan Formation,the shallow-abysmal argillaceous sediments of Yinggehai Formation;the reservoirs are deltaic sandbodies on continental slope.The regional cap rocks of the both are thick mudstone of the Yinggehai Formation and the abysmal ar gillaceous sediments of the Meishan Formation.It is considered that the basin possesses favourable hydrocarbon potential.

    GEOCHEMICAL CHARACTERISTICS OF CRUDE OIL AND CORRELATION OF OIL SOURCE IN CHAGAN SAG
    Lin Weidong
    2000, 21(3):  249-251.  doi:10.11743/ogg20000313
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    Chagan Sag is a Meso-Cenozoic fault depression.The crude oil in it is of low density,low viscosity,low sulfur content,mid paraffin and lightweight oil characterized by high saturated hydrocarbon contents(80%~90%)and rich C27 sterane.The second member of Bayingebi Formation(K1b2)and the first member of Suhongtu Formation(K1s1)of the Lower Cretaceous are potential source rocks of the sag.The ratio of ααα(20R)C27/C29 and ααα(20R)C28/C29 of crude oil and the extract from oil bearing sand is 0.39~0.75 and 0.4~0.7 respectively.The ratio of Pr/Ph and Pr/nC 17 is 0.79~0.94 and 0.83~1.34.The carbon isotopic characteristic curve of crude oil is more similar to dolomitic mudstone of K1b2 and differs from the dark grey mudstone of K1s1.Synthetical correlation shows that the crude oil is mainly derived from the second member of Bayingebi Formation(K1b2)dolomitic mudstane.

    FRACTURES OF ORDOVICIAN CARBONATE ROCKS IN HETIAN RIVER GASFIELD
    Yang Wei, Wang Qinghua, Zhao Rende
    2000, 21(3):  252-255.  doi:10.11743/ogg20000314
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    Three sorts of diagenetic fractures and five stages of structural fractures developed in Ordovician carbonate rocks in Hetian River Gasfield.Their characters of development time,attitude,scale,packing degree and so on are different each other.The fractures are characterized by high angle and small micro fractures,most of them are filled by mud and calcite.The suture and 2~5 stage structural fractures contain spaces for hydrocarbon preservation and migration.Fractures are the principal contributors of permeability(supplying 99.4% of total permeability),and it is the main cause for carbonate rocks to be efficient reservoirs.development degree of fractures was controlled by lithology and tectonic movement.

    CHARACTERISTICS OF MICROFACIES AND DISTRIBUTION OF REMAINING OIL IN UPPER MEMBER OF GUANTAO FORMATION FROM GUDAO AND GUDONG OILFIELDS
    Cai Zhong
    2000, 21(3):  256-258.  doi:10.11743/ogg20000315
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    The upper member of Guantao Formation consists mainly channel bar,point bar,arrested deposits on valley floor,natural levee,crevasse splay,alluvial lake and alluvial flat microfacies.The diposits are principally sandstone and siltrock with mid lower composition maturity and small cross bedding.1~4 sand set are meandering stream deposits,5~6 sand sets are braided channel deposits.The reservoirs of the study area have good physical property,big porosity and high permeability.Sedimentary facies zones controlled the variation of the physical property and improved the porosity and permeability.The channel bars and point bars contain less remaining oil,but alluvial flats and natural levee have relatively rich remaining oil.

    PROSPECTS OF JURASSIC HYDROCARBON EXPLORATION IN SOUTHEAST TARIM BASIN
    Wang Jianguo, Wang Linfeng, Zhou Qi
    2000, 21(3):  259-263,267.  doi:10.11743/ogg20000316
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    The structures in the southeast of Tarim Basin could be divided into two structural units such as southeast depression and southeast uplift.The depression was a dust-pan shape faulted depression in Jurassic,including Minfeng,Qiemo and Ruoqiang three depocenters and subsidence centers.The depression faulted in the south part but overlapped in the north,with Altun Mountains as the primary provenance and then the uplift being secondary.The main reservoirs are Jurassic System,coal measures and deep lake mudstone are the main source beds.It is considered that the depression is favourable for the formation of small- and mid-size oil and gas fields,oil and gas exploration should focus on anticline fault blook traps;the weathered crusts of Luobuzhuang and north Minfeng Uplifts,Minfeng and Andir circular structural belts,-Qigelek pidemont low terraced structural belt are target areas for oil and gas exploration.

    MESO-PALEOZOIC FRACTURES IN CHENGDAO REGION AND THEIR RELATION TO OIL AND GAS
    Li Li Dai, Junsheng, Xie Chuanli
    2000, 21(3):  264-267.  doi:10.11743/ogg20000317
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    Two groups of Mesozoic and Paleozoic fractures developed in Chengdao Region,one strike is northeast 30°,the other is nearly east west.The fractures'dip angles are mostly more than 70° and their width is 0.3~2.0 mm.Most of the fractures formed in Himalayan Period,some of them formed in Yenshan Period.The fractures formed in Himalayan Period are distributed in the south and the north parts of Chenodao Region,they are fine reservoiring spaces and migration passages since their formation time matched well with hydrocarbon expelling stage.The fractures formed in Yenshan Period could form favourable reservoiring spaces and migration passages.

    ACCUMULATION REGULARITY OF UPPER PALEOZOIC GAS IN NORTH ORDOS BASIN
    Li Liang, Yuan Zhixiang, Hui Kuanyang, Liu Shuping
    2000, 21(3):  268-271,282.  doi:10.11743/ogg20000318
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    The Upper Paleozoic of north Ordos Basin is an independent gas system with a complete source reservoir cap rock assemblage.Gas generation centre along Wushen Flag is characterized by large distribution area,big gas generation intensity and abundant gas resources.Sandbodies deposited in rvier channels,fan deltas and tidal flat are favourable for the formation of larg and mid scale traps;the source-reservoir-cap rock assemblage within the same stratum is favourable to form gasfield;large and mid scale sandbodies at the higher part of the gas generation centre are suitable for gas migration and accumulation.Trap types of the study area are mainly lithologic and structural-lithologic traps.It is suggested that Xinjie-Wushen Flag-Hongshiqiao in the east section of Yishaan Slope,the south part of Hangjing Flag fault terrace and Tianhuan Depression are the targets for gas exploration.

    JURASSIC SEDIMENTARY SYSTEM OF EAST JUNGGAR BASIN AND ITS HYDROCARBON SIGNIFICANCE
    Zhang Manlang, Zhu Xiaomin, Zhang Qin
    2000, 21(3):  272-278.  doi:10.11743/ogg20000319
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    Jurassic System developed in the east part of Junggar Basin could be divided into six sedimentary sequences and two tectonic sequences.The sedimentary sequences inclose alluvial fan,braided river,braide river delta and lake sedimentary systems Seatimentary environment includes wetland fan,braided river,braided river delta meandering stream,normal delta,slump turbidite fan,lake shore and shallow lake.The distribution and evolution of the sedimentary systems possess distinct inheritance.There were two provenances in the study area.In sequence I,the north provenance was rich in source materials and formed alluvial fan braided river-braided river delta sedimentary system;in sequence Ⅱ~Ⅲ,lake basin extended and the north provenance receded and formed meandering stream normal deta slump turbidite fan lake sedimentary system;sequences Ⅳ~Ⅴ were controlled by south provenance and small meandering stream deltas formed,the basin rapidly shrank away and meandering stream sediments developed well and distributed extensively.The coal bearing formations in Changji Sag and the slope area,especially the mudstone resulted from lake ingression in sequence Ⅲ are potential source rocks of the study area.The main reservoirs are the sandbodies deposited in the meandering streams and the deltaic sandbodies in sequence Ⅲ in Cainan and the slope area,the sondbodies developed in delta front subaqueous distributive channels of sequences Ⅰ,Ⅲ,Ⅴ in Santai and north Santai areas,the meandering stream sand bars of sequence Ⅵ.

    ORIGIN AND INTENSION OF CONCEPT IN PETROLEUM SYSTEM
    Wang Shicheng, Zhou Qingfan
    2000, 21(3):  279-282.  doi:10.11743/ogg20000320
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    The original concept of petroleum system was put forward by an American petroleum geologist Dow in 1972,and then it was supplemented and improved by Porrodon,Demaison,Meissner and others.The petroleum system consists of a effective source rock mass associated with all relative natural hydrocarbon systems and necessary geological elements for oil and gas pools.The petroleum system,together with sedimentary basin,pool-forming assemblage and play,constitute a petroleum investigation series.So the petroleum system does not belong to the category of new theory,but really a new method suitable for oil and gas researches.The object of the research is a petroleum unit of certain origin.The petroleum system could be divided into generation subsystem,migration subsystem and accumulation(preservation)subsystem due to different geological elements and functions.The petroleum systems in China are usually complex systems.When introduce and apply the method of this system,one should neither apply it indiscriminately,nor revise it without considering our own geological condition.

    QUASI-PETROLEUM SYSTEMS IN SONGLIAO BASIN
    Han Xiaodong
    2000, 21(3):  283-285.  doi:10.11743/ogg20000321
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    Three petroleum systoms are divided according to high potential surface caprock combination in Songliao Basin.This division is lags behind the present exploration of the basin.So it's necessary to subdivide each petroleum system into more favourable petroleum units.The so called quasi-petroliferous system is actually a kind of hydrocarbon accumulation unit that between the petroliferous system and hydrocarbon pool-forming assemblage.The core of the oil accumulation unit is that it has similar static pool-forming condition such as oil generation-reservoir-caprock and dynamic process of oil migration and accumulation.The middle petroliferous system of Songliao Basin is dominated by oil and gas upward expulsion and lateral migration.This system could be subdivided into three quasi-petroliferous systems according to different hydrocarbon accumulation ways:Daqing Placanticline quasi-petroliferous system of confluent type;Taikang-Yingtai quasi-petroliferous system dominated by lateral migration and accumulation;the south quasi-petroliferous system of divergent accumulation.The lower petroliferous system of the basin is dominated by downward expulsion and vertical migration,and could be subdivided into 4 types of quasi-petroliferous systems:Sanzhao,Qijia,Gulong,Changling subsystems of detained and divergent accumulation;Daqing Placanitcline and Fuxin-Chaoyanggou subsystems of confluent accumulation.