三江—中阿穆尔盆地石油地质条件综合研究
|
摘要
在大地构造背景与演化、区域地层、构造、沉积特征等区域性基础地质研究基础上,综合应用沉积学、地震地层学、石油地质学理论,对三江-中阿穆尔盆地的地层层序特征、沉积特征、石油地质条件等开展了综合研究。本文以三江-中阿穆尔盆地西南部(中国境内)中生界地层和三江-中阿穆尔盆地东北部(俄罗斯境内)新生界地层为主建立了整个盆地的地层综合柱状图。结合盆地沉积演化特征,确定出盆地主要时期的岩相古地理特征,认为中、晚侏罗世盆地以浅海、半深海沉积环境为主,早白垩世城子河组时期为统一近海边缘盆地,以海陆交互相及河湖相沉积为主,晚白垩世以河流、河泛相沉积为主,新生代主要为河流、湖泊沉积环境。应用石油地质学理论对盆地的生油层、储集层、盖层以及生储盖组合特征进行了综合分析研究,确定出四套生储盖组合。
结合地层特征、沉积环境特征及生储盖条件,认为该盆地具有良好的含油气远景,其中盆地东部前进坳陷和宾利亚斯断陷应该加强深部无机成因气藏的开发研究。
Sanjiang-Middle Amur basin is located at the northeast Asia continental margin, in the territories of Russia and China, which spans the boundary as a unique basin. It is elongated in a NE-direction over 500 km with a width of 200 km from Jiamusi of China to Komsomolsk-na-amure of Russia. The total area of the basin is 90370 km2, in which more than 60% is in Russia. It is necessary to reinforce research as the area in China (Sanjiang basin) is one of the largest sedimentary basins in northeast china, for the purpose of searching for new oil and gas resources. Although much has been done, most of them are concentrated on either the Chinese part or Russian part without correlations between them. So, this thesis carries out the integrated study on stratigraphic sequence, sedimentary character and petroleum geological conditions from the perspective of the entire basin.
Its geotectonic position locates at the joint region where Paleo-Asian Ocean structural domain and the littoral Pacific Ocean structural domain connect. The separation and amalgamation of micro-continental block is complicated. The western part of Sanjiang-Middle Amur basin's overlies the Precambrian Bureya-Jiamusi massif, while its central and eastern parts overlie the Sikhote-Alin Mesozoic orogenic belt. The basin's general structure is seen as a system of grabens and horsts. There are three first-order structures in the southwestern sector of the basin (in China): Suibing depression, Fujing uplift, and Qianjin depression. In the northeastern sector (in Russia), the first-order structures are mainly made up of Birofeld、Kur-Urmi fault depression, Uldura-Churkinsk uplift, Vandan-Gorbylyakh uplift, Khekhtsir and Petropaclovsk uplift, Pereyaslavsky-Anyuy fault depression.
Middle-upper Jurassic, Cretaceous, Cenozoic sediments are the main deposits of Sanjiang-Middle Amur basin. Based on Mesozoic sequence of the southwestern sector of the basin in China and Cenozoic sequence in the northeastern sector in Russia, the author established an uniform general stratigraphic column. The formational sequence is identified as follows(bottom-up): Suibin formation in middle Jurassic and Dongrong formation in upper Jurassic. Didao formation, Chenzihe formation, Muling formation and Dongshan formation in lower Cretaceous, Houshigou formation, Hailang formation, Qixinghe formation and Yanwo formation in upper Cretaceous. The Cenozoic consist of Chernaya Rechka formation, Birofeld formation, Ushumun formation, Golovin formation, Priamurskaya formation.
Southwestern sector of Sanjiang-Middle Amur basin as to Sanjiang area of China is the only Mesozoic sedimentary basin that has marine facies and continental-oceanic interaction facies in northeast China, and a residual basin which reformed by many times tectonic movements. According to the integrative analysis of cores, field sections, utilizing logging data, seismic materials and paleontology datas, it is indicated that the sedimental feature and assemblages in this area are mostly made up of the continental facies, and others are marine-continental transitional and marine facies. There are two major gulfs from Russia to China at the period of Chengzihe Formation. One flows to Bikin basin along the Ussuri River, then comes into Hulin basin as a cove along Dunmi fault, while the other flows along Heilongjiang(Amur River) south into Suibin depression. Sanjiang-Middle Amur basin is considered to be a large submaritime basin in Mesozoic. Cenozoic maily develops fluvial facies, lacustrine facies, paludal facies, etc.
According to the sedimentary environment studying, it meets the requirements of source rocks which is rich in organic matrix. Suibin formation and Dongrong formation, middle and upper Chenzihe formation, Muling formation, Chernaya Rechka formation, Birofeld formation are the main source rock.
Suibin formation in middle Jurassic and Dongrong formation in upper Jurassic, Chenzihe formation, Muling formation in lower Cretaceous are characterized by low porosity and low permeability and the reservoir physical property is poor. The Cenozoic most potential reservoirs are middle and upper Chernaya Rechka formation, Birofeld formation and Ushumun formation. Comprehensive study on the character of the source rock reservoir and cap cover shows, there are two main types of source reservoir cap assemblage which are self-generating and self-accumulating, bottom source-top reservior.
While, whether there is oil or gas shows is the most direct evidence of the petroleum potential in a basin or depression. For the time being there have been several oil and gas occurrences in Sanjiang-Middle Amur basin. The presence of low resistivity zone and deep fault zone in the eastern basin provide a certain basis to find inorganic gas reservoirs.
In the end, on the basis of geology and petroleum geology conditions studying, this paper points out that Suibin depression and Qianjin depression which locate at the southwestern sector of the basin (in China) are the most favorable exploration areas. The main exploration layer in Suibin depression is middle and upper Jurassic, in Qianjin depression is upper Cretaceous and Paleogene. The favorable exploration areas in northeastern sector (in Russia) are Birofeld and Pereyaslavsky fault depression, and Paleogene, Ushumun formation of Lower-Middle Miocene is the main exploration layer.
By means of large number of real and basic geological documents and petroleum geology materials, stratigraphic sequence, sedimentary characters have been researched in detail from the perspective of unique basin, and petroleum geological conditions evaluation has completed, then favorable exploration areas has put forward. The above study results possess much more important theoretical significance and practical value for further exploration and the exploitation of Sanjaing-Middle Amur basin and other China-Russia transboundary basin.
结合地层特征、沉积环境特征及生储盖条件,认为该盆地具有良好的含油气远景,其中盆地东部前进坳陷和宾利亚斯断陷应该加强深部无机成因气藏的开发研究。
Sanjiang-Middle Amur basin is located at the northeast Asia continental margin, in the territories of Russia and China, which spans the boundary as a unique basin. It is elongated in a NE-direction over 500 km with a width of 200 km from Jiamusi of China to Komsomolsk-na-amure of Russia. The total area of the basin is 90370 km2, in which more than 60% is in Russia. It is necessary to reinforce research as the area in China (Sanjiang basin) is one of the largest sedimentary basins in northeast china, for the purpose of searching for new oil and gas resources. Although much has been done, most of them are concentrated on either the Chinese part or Russian part without correlations between them. So, this thesis carries out the integrated study on stratigraphic sequence, sedimentary character and petroleum geological conditions from the perspective of the entire basin.
Its geotectonic position locates at the joint region where Paleo-Asian Ocean structural domain and the littoral Pacific Ocean structural domain connect. The separation and amalgamation of micro-continental block is complicated. The western part of Sanjiang-Middle Amur basin's overlies the Precambrian Bureya-Jiamusi massif, while its central and eastern parts overlie the Sikhote-Alin Mesozoic orogenic belt. The basin's general structure is seen as a system of grabens and horsts. There are three first-order structures in the southwestern sector of the basin (in China): Suibing depression, Fujing uplift, and Qianjin depression. In the northeastern sector (in Russia), the first-order structures are mainly made up of Birofeld、Kur-Urmi fault depression, Uldura-Churkinsk uplift, Vandan-Gorbylyakh uplift, Khekhtsir and Petropaclovsk uplift, Pereyaslavsky-Anyuy fault depression.
Middle-upper Jurassic, Cretaceous, Cenozoic sediments are the main deposits of Sanjiang-Middle Amur basin. Based on Mesozoic sequence of the southwestern sector of the basin in China and Cenozoic sequence in the northeastern sector in Russia, the author established an uniform general stratigraphic column. The formational sequence is identified as follows(bottom-up): Suibin formation in middle Jurassic and Dongrong formation in upper Jurassic. Didao formation, Chenzihe formation, Muling formation and Dongshan formation in lower Cretaceous, Houshigou formation, Hailang formation, Qixinghe formation and Yanwo formation in upper Cretaceous. The Cenozoic consist of Chernaya Rechka formation, Birofeld formation, Ushumun formation, Golovin formation, Priamurskaya formation.
Southwestern sector of Sanjiang-Middle Amur basin as to Sanjiang area of China is the only Mesozoic sedimentary basin that has marine facies and continental-oceanic interaction facies in northeast China, and a residual basin which reformed by many times tectonic movements. According to the integrative analysis of cores, field sections, utilizing logging data, seismic materials and paleontology datas, it is indicated that the sedimental feature and assemblages in this area are mostly made up of the continental facies, and others are marine-continental transitional and marine facies. There are two major gulfs from Russia to China at the period of Chengzihe Formation. One flows to Bikin basin along the Ussuri River, then comes into Hulin basin as a cove along Dunmi fault, while the other flows along Heilongjiang(Amur River) south into Suibin depression. Sanjiang-Middle Amur basin is considered to be a large submaritime basin in Mesozoic. Cenozoic maily develops fluvial facies, lacustrine facies, paludal facies, etc.
According to the sedimentary environment studying, it meets the requirements of source rocks which is rich in organic matrix. Suibin formation and Dongrong formation, middle and upper Chenzihe formation, Muling formation, Chernaya Rechka formation, Birofeld formation are the main source rock.
Suibin formation in middle Jurassic and Dongrong formation in upper Jurassic, Chenzihe formation, Muling formation in lower Cretaceous are characterized by low porosity and low permeability and the reservoir physical property is poor. The Cenozoic most potential reservoirs are middle and upper Chernaya Rechka formation, Birofeld formation and Ushumun formation. Comprehensive study on the character of the source rock reservoir and cap cover shows, there are two main types of source reservoir cap assemblage which are self-generating and self-accumulating, bottom source-top reservior.
While, whether there is oil or gas shows is the most direct evidence of the petroleum potential in a basin or depression. For the time being there have been several oil and gas occurrences in Sanjiang-Middle Amur basin. The presence of low resistivity zone and deep fault zone in the eastern basin provide a certain basis to find inorganic gas reservoirs.
In the end, on the basis of geology and petroleum geology conditions studying, this paper points out that Suibin depression and Qianjin depression which locate at the southwestern sector of the basin (in China) are the most favorable exploration areas. The main exploration layer in Suibin depression is middle and upper Jurassic, in Qianjin depression is upper Cretaceous and Paleogene. The favorable exploration areas in northeastern sector (in Russia) are Birofeld and Pereyaslavsky fault depression, and Paleogene, Ushumun formation of Lower-Middle Miocene is the main exploration layer.
By means of large number of real and basic geological documents and petroleum geology materials, stratigraphic sequence, sedimentary characters have been researched in detail from the perspective of unique basin, and petroleum geological conditions evaluation has completed, then favorable exploration areas has put forward. The above study results possess much more important theoretical significance and practical value for further exploration and the exploitation of Sanjaing-Middle Amur basin and other China-Russia transboundary basin.
引文
[1] A.A.Vrublevsky.Tectonics of the Sikhote-Alin fold system[J].大地构造与成矿学, ,1988,12(2):101-116.
[2] A.L.Khanchuk.Geodynamics magmatism and metallogeny of the Russian east[M]. Vladivostok:Vladivostok Dalnauka,2006.
[3] A.P. Sorokin,T.V. Artemenko,V.Z. Mezhakov,et al.Natural-resource potential of the trans-boundary territory of Russia and the PRC within the Upper and Middle Amur basin[J].Geography and Natural Resources,2008,29:363-368.
[4] B.A. Natal'in,L.M. Parfenov,et al.Main Fault Systems of the Soviet Far East[J].Philosophical Transactions of the Royal Society of London. Series A,Mathematical and Physical Sciences,1986, 317(1539):267-275.
[5] F.M.PERSITS,G. F. ULMISHEK,D. W.Steinshouer. Maps showing Geology,Oil and Gas Fields and Geologic Provinces of the Former Soviet Union. Usgs open file report,1998.
[6] G.L. Kirillova. Comparative characteristics of intracontinental rift basins of East Asia:Songliao and Amur-Zeya [J].Geology of the Pacific Ocean,1995,11:909-935.
[7] G.L. Kirillova. Cretaceous tectonics and geological environments in East Russia [J]. Journal of Asian Earth Sciences,2003,21:967-977.
[8] G.L. Kirillova.Late Mesozoic-Cenozoic sedimentary basins of active continental margin of Southeast Russia:paleogeography,tectonics,and coal-oil-gas presence[J].Marine and Petroleum Geology, 2003,20;385-397.
[9] G.L. Kirillova.Stages of late mesozoic and cenozoic rifting in southeastern Russia and adjacent regions:Implication for the petroleum potential[J].Doklady Earth Science,2008,419(1):104-107.
[10] G.L.Kirillova,Liu Zhao Jun,Wang Si Min,et al.Stratigraphic correlation of the Upper Mesozoic–Cenozoic sequences of the Middle Amur(Sangjiang)sedimentary basin[J]. Geology of Pacific Ocean,1997,13:1081-1109.
[11] G.L.Kirillova,V.N. Gagayev. Petroleum prospectivity,main directions of studies and exploration targets in the Middle Amur potential petroleum basin (in Russian)[C].Prospects of development of the fuel and energy basis of the Far Eastern economicdistrict, and hydrocarbon resources of the Russian north-east and far eastern offshore,1998,191-203.
[12] G.L.Kirillova,V.V. Kiriyanova.J/K boundary in southeastern Russia and possible analogue of the Tetori Group,Japan[J]. Memoir of the Fukui Prefectural Dinosaur Museum,2003,2:75-102.
[13] G.L.Kirillova.Jurassic-Cretaceous Continental Margin of Southeastern Russia:Outcrop Sequence Stratigraphy,Sedimentation and Tectonics[Z].Yu.A. Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences, 2009.
[14] G.L.Kirillova.三江-中阿穆尔盆地层序地层分析、地球动力学与含油气性[R].哈巴罗夫斯克:俄罗斯科学院远东分院构造与地球物理研究所,2002.
[15] IHS.Information on Russia,China Middle Amur/Sanjiang[R]. IHS Energy and its affiliated and subsidiary companies,2009.
[16] Khanchuk A.I..Pre-Neogene tectonics of the Sea-of-Japan region:a view from the Russian side[J]. Earth Science,2001,55:275-291.
[17] Kingston D R,Dishroon C P,Williams P A.Global basin classification system[C].AAPG, 672,67(2):2175-2193 .
[18] Kohei SATO,Anatoly A,et al.Mid-Cretaceous Episodic Magmatism and Tin Mineralization inKhingan-Okhotsk Volcano-Plutonic belt Far East Russia[J].Resource Geology,2002,52(1):1-14.
[19] Kojima, S..Mesozoic terrane accretion in Northeast China,Sikhote-Alin and Japan regions[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,1989,69:213-232.
[20] Sergei Zyabrev,Atsushi Matsuoka. Late Jurassic (Tithonian) radiolarians from a clastic unit of the Khabarovsk complex (Russian Far East): Significance for subduction accretion timing and terrane correlation[J].The Island Arc,1999,8(1):30-37.
[21] Sha Jingeng,Matsukawa M,et al.The Upper Jurassic–Lower Cretaceous of eastern Heilongjiang, northeast China:Stratigraphy and regional basin history. Cretaceous Res,2003,24:715-728.
[22] Sha JinGeng,Wang JianPo,G.L. Kirillova.Upper Jurassic and Lower Cretaceous of Sanjiang-Middle Amur basin:Non-marine and marine correlation[J]. Science in China Series D: Earth Sciences,2009,52(10):1-17.
[23] T.V. Merkulova,E.P. Razvozzhaeva. Cenozoic graben facies in the Middle Amur sedimentary basin as inferred from seismic and electrical exploration[J].Russian Journal of Pacific Geology,2007,1(4):335-351.
[24] Utkin Valentine P.A synsedimentary structure formation model for the Far East Jurassic-Early Cretaceous basins and uplifts,Russia[J]. Sci in China Ser D-Earth Sci,2009,52(12):1979-1992.
[25] V.A. Buryak,Yu.I. Bakulin,et al.Petroleum Occurrence in Southern Far East and Adjacent Territories(in Russian)[C].Far EastInstitute of Mineral Resources of the Ministry of Natural Resources,1998:1-282.
[26] V.B. Kaplun.Geoelectric section of the lithosphere in the central part of the Middle Amur sedimentary basin(Far East)based on the magnetotelluric sounding data[J]. Russian Journal of Pacific Geology,2009,3(2):185-196.
[27] V.G. Varnavsky. Paleogene and Neogene Deposits of Middle-Amur Depression(in Russian)[M]. Moscow:Science,1971,160.
[28] V.G. Varnavsky.Sedimentogenic aspect of the evolution of Cenozoic structures of southwestern part of the Middle Amur sedimentary basin(Far East)аnd their petroliferous prospects. Geology of Pacific ocean,2008,27(2):107-118.
[29] Zonenshain,M.Kuzmin,Natapov.Geology of the USSR:A Plate-Tectonic Synthesis[J].AGU Geodynamics Series,1990,21.
[30]В.г.Варнавский.СЕДИМЕНТОГЕННЫЙАСПЕКТЭВОЛЮЦИИКАЙНОЗОЙСКИХСТРУКТУРЮГО-ЗАПАДНОЙЧАСТИСРЕДНЕАМУРСКОГООСАДОЧНОГОБАССЕЙНАИПЕРСПЕКТИВИХНЕФТЕГАЗОНОСНОСТИ(ДАЛЬНИЙВОСТОК)[J].ТихоокеанскаяГеология,2008,27 (22):107-118.
[31]Г.Л.Кириллова.ЭтапыПозднемезозойскогоиКайнозойскогоРифтогенезаНаюго-востокеРоссииивСопредельныхРегионахвСвязисПроблемойНефтегазоносности[J].ДокладыАкадемииНаук,2008,419(1):104-107.
[32]МедведеваС.А..ГеологическоеСтроениеПозднемезозойскогоТерригенногоКомплексаСреднегоПриамурьяВСвязиСОценкойПерспективНефтегазоносности[D].Иркутск,2010.
[33]Т.В.Меркулова,Г.Л.Кириллова.СтроениеИПерспективыНефтегаОносностиСеверныхЗвеньевИтун-ИланьскойВетвиРазломовТан-Лу[J].ТихоокеанскаяГеология,2004, 23(6):55-75.
[34]陈发景,赵海玲,陈昭年等.中国东部中、新生代伸展盆地构造特征及地球动力学背景[J].中国地质大学学报(地球科学),1996,21(4):357-365.
[35]大庆油田研究院.三江盆地石油地质条件及下步勘探部署设想[R].大庆油田研究院,2001.
[36]戴金星,宋岩,戚厚发等.中国东部无机成因气及其气藏形成条件[M].北京:科学出版社,1995.
[37]葛肖虹,马文璞.东北亚南区中-新生代大地构造轮廓[J].中国地质,2007,34(2):212-228.
[38]郭少斌,王红亮.绥滨坳陷中生界层序地层特征及油气勘探远景[J].石油勘探与开发,2008,35(1):44-51.
[39]何玉平.黑龙江省东部早白垩世沉积特征与原型盆地恢复[D].吉林大学地球科学学院,2006.
[40]黑龙江省地质矿产局.黑龙江省区域地质志[M].地质出版社,1993.
[41]胡志方,马义忠,乔桂林.三江盆地石油地质条件与勘探前景[J].河南石油.2006,20(1):1-4.
[42]胡志方.三江盆地绥滨坳陷中生界层序地层与有利目标预测[D].中国地质大学(北京),2006.
[43]黄汲青,陈炳蔚.中国及邻区特提斯域演化[M].地质出版社,1987.
[44]黄清华,杨建国,孔惠.东北依兰-伊通地堑方正断陷方正组的建立及其意义[J].地层学杂志,2003,27(2):138-145.
[45]姜贵周.中国东北中新生代盆地成因与演化[J].大庆石油学院学报,1997,21(l):l-6.
[46]姜在兴等.沉积学[M].北京:石油工业出版社,2003.
[47]荆凤,申旭辉,洪顺英等.基于遥感技术研究依兰-伊通断裂带[J].地震,2006,26(3):79-84.
[48]李福川.中国应加紧开发三江盆地的油气资源[J].俄罗斯中亚东欧市场,2005,5:46-47.
[49]李国玉,吕鸣岗等.中国含油气盆地图集[M].北京:石油工业出版社,2002.
[50]李国玉.世界油田图集[M].北京:石油工业出版社,2000.
[51]李锦轶.布列亚-佳木斯古板块的构成及演化[J].地学研究,1995,28:96-98.
[52]李思田,路凤香,林畅松.中国东部及邻区中新生代盆地演化和动力学背景[M].武汉:中国地质大学出版社,1997.
[53]李思田等.断陷盆地分析与聚煤规律[M].武汉:中国地质大学出版社,1988.
[54]李子俊,姜剑虹.三江-穆棱河中晚侏罗世沉积体系与聚煤模式[J].东北煤炭技术,1996,3:9-18.
[55]刘海山,郝天珧.勃利盆地侏罗系、白垩系、第三系古地磁研究及其意义[J].沈阳地质矿产所集刊.北京:地质出版社,1992.
[56]刘云武,唐振国,刘文龙.三江盆地演化特征与油气勘探方向[J].石油天然气学报(江汉石油学院学报),2006,28(2):1-5.
[57]刘招君,董清水,王嗣敏等.陆相层序地层学导论与应用[M].北京:石油工业出版社,2002.
[58]陆克政.含油气盆地分析[M].东营:石油大学出版社,2001.
[59]马金苹.大庆探区外围东部盆地群油气远景评价[D].吉林:吉林大学地球科学学院,2008.
[60]马小刚,王东坡,薛林福,王青海,王孔伟.三江盆地绥滨坳陷构造特征及其与油气的关系[J].长春科技大学学报,2000,30(1):46-50.
[61]马杏垣,刘和甫,王维襄.中国东部中、新生代裂陷作用和伸展构造[J].地质学报,1983,57(1):22-31.
[62]孟庆龙.大庆探区外围东部主要盆地数值模拟及其地质意义研究[D].吉林:吉林大学地球科学学院.2007.
[63]谯汉生,于兴河.裂谷盆地石油地质[M].北京:石油工业出版社,2004.
[64]郄瑞卿.大庆探区外围中、新生代断陷盆地群油气地质条件及远景评价[D].吉林:吉林大学地球科学学院.2009.
[65]任文忠.盆地分析的原理和方法[M].北京:煤炭工业出版社,1993.
[66]邵济安,唐克东,王成源等.那丹哈达地体的构造特征及演化[J].中国科学(B辑), 1991,7:744-751.
[67]邵济安,唐克东.中国东北地体与东北亚大陆边缘演化[M].北京:地震出版社,1995.
[68]邵济安,王成源,唐克东.乌苏里地区构造新探索[J].地质论评,1992,38(l):33-38.
[69]水谷申治郎,邵济安,张庆龙.1989.那丹哈达地体与东亚大陆中生代构造的关系[J].地质学报,63:204-215.
[70]宋兰斌.三江盆地绥滨坳陷中、新生界生油层早期评价[A].第三届全国沉积学大会论文摘要汇编,2004.
[71]孙永传,李蕙生编.碎屑岩沉积相和沉积环境[M].地质出版社,1986.
[72]唐振海,张亚金,赵玉珍.三江盆地绥滨坳陷石油地质特征.大庆石油地质与开发,2005,24(3):31-32.
[73]田在艺,张庆春.中国含油气沉积盆地论[M].北京:石油工业出版社,1996.
[74]童亨茂.伊通地堑边界断裂的性质与演化[J].地质力学学报,2002,8(1):35-42.
[75]汪新文.东北亚大陆边缘中新生带构造事件与演化序列[J].地质科技情报,1997,16(4):9-14.
[76]王鸿祯,杨森楠,李思田.中国东部及邻区中、新生代盆地发育及大陆边缘区的构造发展[J].地质学报,1983,57(3):213-223.
[77]王鸿祯.中国古地理图集[M].北京:地图出版社,1985.
[78]王骏,王东坡,C.A.乌沙科夫等.东北亚中新生代沉积类型及其地质特征[M].北京:地质出版社,1997:1-87.
[79]王良忱,张金亮.沉积环境和沉积相[M].北京:石油工业出版社,1999.
[80]王世辉,王立民,唐金生.兴安岭盆地群成盆机制及含油气远景评价[J].大庆石油地质与开发,2001,20(5):5-7.
[81]吴福元,曹林.东北亚地区的若干重要基础地质问题[J].世界地质,1999,18(2):1-13.
[82]萧德铭,王荣华,蔡天成等.俄罗斯东西伯利亚及远东地区含油气盆地[M].北京:石油工业出版社,2000.
[83]谢鸣谦.拼贴板块构造及其驱动机理-中国东部及相邻区的大地构造演化[M].北京:科学出版社,2000.
[84]杨建国,赵传本,张海桥.东北地区三江盆地海陆相侏罗-白垩系层序.第三届全国地层会议论文集[C].北京:地质出版社,2000,270-274.
[85]杨绍芳.泛三江盆地成藏机制分析[J].石油天然气学报,2005,27(4):413-415.
[86]于明德,王璞珺,王冶.三江盆地西大林子地区构造特征与圈闭样式[J].石油天然气学报(江汉石油学院学报),2008,30(1):1-6.
[87]云金表,罗笃清,李玉喜.东北地区中生代断陷盆地群构造演化与成油关系探讨[J].石油勘探与开发,1994,21(6):40-45.
[88]张梅生,彭向东,孙晓猛.中国东北区古生代构造古地理格局[J].辽宁地质, 1998, (2):91-96.
[89]张兴洲,周建波,迟效国等.东北地区晚古生代构造-沉积特征与油气资源[J].吉林大学学报(地球科学版),2008,38(5):719-725.
[90]张旭东.东北地区中生代断陷盆地群成盆机制及油气远景[D].吉林:吉林大学地球科学学院,2007.
[91]赵传本,叶得泉,魏德恩.中国油气区第三系(Ⅲ)[M].北京:石油工业出版社,1994.
[92]赵霞,于兴河,易荣龙等.三江盆地构造演化分析[J].内蒙古石油化工,2007,5:310-313.
[93]周建波,张兴洲,马志红等.中国东北地区的构造格局与盆地演化[J].石油与天然气地质,2009,30(5):530-538.
[94]朱建伟,刘招君,董清水,刘葵,郭巍.松辽盆地层序地层格架及油气聚集规律[J].石油地球物理勘探,2001,36(3):339-344.
[95]朱建伟等.三江-中阿穆尔盆地层对比、构造特征及含油气性分析[R].吉林大学地球科学学院,2004.
[96]邹艳荣,蔡玉兰.东北三江盆地演化分析[J].中国煤田地质,1997,9(1):19-21.
[2] A.L.Khanchuk.Geodynamics magmatism and metallogeny of the Russian east[M]. Vladivostok:Vladivostok Dalnauka,2006.
[3] A.P. Sorokin,T.V. Artemenko,V.Z. Mezhakov,et al.Natural-resource potential of the trans-boundary territory of Russia and the PRC within the Upper and Middle Amur basin[J].Geography and Natural Resources,2008,29:363-368.
[4] B.A. Natal'in,L.M. Parfenov,et al.Main Fault Systems of the Soviet Far East[J].Philosophical Transactions of the Royal Society of London. Series A,Mathematical and Physical Sciences,1986, 317(1539):267-275.
[5] F.M.PERSITS,G. F. ULMISHEK,D. W.Steinshouer. Maps showing Geology,Oil and Gas Fields and Geologic Provinces of the Former Soviet Union. Usgs open file report,1998.
[6] G.L. Kirillova. Comparative characteristics of intracontinental rift basins of East Asia:Songliao and Amur-Zeya [J].Geology of the Pacific Ocean,1995,11:909-935.
[7] G.L. Kirillova. Cretaceous tectonics and geological environments in East Russia [J]. Journal of Asian Earth Sciences,2003,21:967-977.
[8] G.L. Kirillova.Late Mesozoic-Cenozoic sedimentary basins of active continental margin of Southeast Russia:paleogeography,tectonics,and coal-oil-gas presence[J].Marine and Petroleum Geology, 2003,20;385-397.
[9] G.L. Kirillova.Stages of late mesozoic and cenozoic rifting in southeastern Russia and adjacent regions:Implication for the petroleum potential[J].Doklady Earth Science,2008,419(1):104-107.
[10] G.L.Kirillova,Liu Zhao Jun,Wang Si Min,et al.Stratigraphic correlation of the Upper Mesozoic–Cenozoic sequences of the Middle Amur(Sangjiang)sedimentary basin[J]. Geology of Pacific Ocean,1997,13:1081-1109.
[11] G.L.Kirillova,V.N. Gagayev. Petroleum prospectivity,main directions of studies and exploration targets in the Middle Amur potential petroleum basin (in Russian)[C].Prospects of development of the fuel and energy basis of the Far Eastern economicdistrict, and hydrocarbon resources of the Russian north-east and far eastern offshore,1998,191-203.
[12] G.L.Kirillova,V.V. Kiriyanova.J/K boundary in southeastern Russia and possible analogue of the Tetori Group,Japan[J]. Memoir of the Fukui Prefectural Dinosaur Museum,2003,2:75-102.
[13] G.L.Kirillova.Jurassic-Cretaceous Continental Margin of Southeastern Russia:Outcrop Sequence Stratigraphy,Sedimentation and Tectonics[Z].Yu.A. Kosygin Institute of Tectonics and Geophysics, Far East Branch, Russian Academy of Sciences, 2009.
[14] G.L.Kirillova.三江-中阿穆尔盆地层序地层分析、地球动力学与含油气性[R].哈巴罗夫斯克:俄罗斯科学院远东分院构造与地球物理研究所,2002.
[15] IHS.Information on Russia,China Middle Amur/Sanjiang[R]. IHS Energy and its affiliated and subsidiary companies,2009.
[16] Khanchuk A.I..Pre-Neogene tectonics of the Sea-of-Japan region:a view from the Russian side[J]. Earth Science,2001,55:275-291.
[17] Kingston D R,Dishroon C P,Williams P A.Global basin classification system[C].AAPG, 672,67(2):2175-2193 .
[18] Kohei SATO,Anatoly A,et al.Mid-Cretaceous Episodic Magmatism and Tin Mineralization inKhingan-Okhotsk Volcano-Plutonic belt Far East Russia[J].Resource Geology,2002,52(1):1-14.
[19] Kojima, S..Mesozoic terrane accretion in Northeast China,Sikhote-Alin and Japan regions[J]. Palaeogeography,Palaeoclimatology,Palaeoecology,1989,69:213-232.
[20] Sergei Zyabrev,Atsushi Matsuoka. Late Jurassic (Tithonian) radiolarians from a clastic unit of the Khabarovsk complex (Russian Far East): Significance for subduction accretion timing and terrane correlation[J].The Island Arc,1999,8(1):30-37.
[21] Sha Jingeng,Matsukawa M,et al.The Upper Jurassic–Lower Cretaceous of eastern Heilongjiang, northeast China:Stratigraphy and regional basin history. Cretaceous Res,2003,24:715-728.
[22] Sha JinGeng,Wang JianPo,G.L. Kirillova.Upper Jurassic and Lower Cretaceous of Sanjiang-Middle Amur basin:Non-marine and marine correlation[J]. Science in China Series D: Earth Sciences,2009,52(10):1-17.
[23] T.V. Merkulova,E.P. Razvozzhaeva. Cenozoic graben facies in the Middle Amur sedimentary basin as inferred from seismic and electrical exploration[J].Russian Journal of Pacific Geology,2007,1(4):335-351.
[24] Utkin Valentine P.A synsedimentary structure formation model for the Far East Jurassic-Early Cretaceous basins and uplifts,Russia[J]. Sci in China Ser D-Earth Sci,2009,52(12):1979-1992.
[25] V.A. Buryak,Yu.I. Bakulin,et al.Petroleum Occurrence in Southern Far East and Adjacent Territories(in Russian)[C].Far EastInstitute of Mineral Resources of the Ministry of Natural Resources,1998:1-282.
[26] V.B. Kaplun.Geoelectric section of the lithosphere in the central part of the Middle Amur sedimentary basin(Far East)based on the magnetotelluric sounding data[J]. Russian Journal of Pacific Geology,2009,3(2):185-196.
[27] V.G. Varnavsky. Paleogene and Neogene Deposits of Middle-Amur Depression(in Russian)[M]. Moscow:Science,1971,160.
[28] V.G. Varnavsky.Sedimentogenic aspect of the evolution of Cenozoic structures of southwestern part of the Middle Amur sedimentary basin(Far East)аnd their petroliferous prospects. Geology of Pacific ocean,2008,27(2):107-118.
[29] Zonenshain,M.Kuzmin,Natapov.Geology of the USSR:A Plate-Tectonic Synthesis[J].AGU Geodynamics Series,1990,21.
[30]В.г.Варнавский.СЕДИМЕНТОГЕННЫЙАСПЕКТЭВОЛЮЦИИКАЙНОЗОЙСКИХСТРУКТУРЮГО-ЗАПАДНОЙЧАСТИСРЕДНЕАМУРСКОГООСАДОЧНОГОБАССЕЙНАИПЕРСПЕКТИВИХНЕФТЕГАЗОНОСНОСТИ(ДАЛЬНИЙВОСТОК)[J].ТихоокеанскаяГеология,2008,27 (22):107-118.
[31]Г.Л.Кириллова.ЭтапыПозднемезозойскогоиКайнозойскогоРифтогенезаНаюго-востокеРоссииивСопредельныхРегионахвСвязисПроблемойНефтегазоносности[J].ДокладыАкадемииНаук,2008,419(1):104-107.
[32]МедведеваС.А..ГеологическоеСтроениеПозднемезозойскогоТерригенногоКомплексаСреднегоПриамурьяВСвязиСОценкойПерспективНефтегазоносности[D].Иркутск,2010.
[33]Т.В.Меркулова,Г.Л.Кириллова.СтроениеИПерспективыНефтегаОносностиСеверныхЗвеньевИтун-ИланьскойВетвиРазломовТан-Лу[J].ТихоокеанскаяГеология,2004, 23(6):55-75.
[34]陈发景,赵海玲,陈昭年等.中国东部中、新生代伸展盆地构造特征及地球动力学背景[J].中国地质大学学报(地球科学),1996,21(4):357-365.
[35]大庆油田研究院.三江盆地石油地质条件及下步勘探部署设想[R].大庆油田研究院,2001.
[36]戴金星,宋岩,戚厚发等.中国东部无机成因气及其气藏形成条件[M].北京:科学出版社,1995.
[37]葛肖虹,马文璞.东北亚南区中-新生代大地构造轮廓[J].中国地质,2007,34(2):212-228.
[38]郭少斌,王红亮.绥滨坳陷中生界层序地层特征及油气勘探远景[J].石油勘探与开发,2008,35(1):44-51.
[39]何玉平.黑龙江省东部早白垩世沉积特征与原型盆地恢复[D].吉林大学地球科学学院,2006.
[40]黑龙江省地质矿产局.黑龙江省区域地质志[M].地质出版社,1993.
[41]胡志方,马义忠,乔桂林.三江盆地石油地质条件与勘探前景[J].河南石油.2006,20(1):1-4.
[42]胡志方.三江盆地绥滨坳陷中生界层序地层与有利目标预测[D].中国地质大学(北京),2006.
[43]黄汲青,陈炳蔚.中国及邻区特提斯域演化[M].地质出版社,1987.
[44]黄清华,杨建国,孔惠.东北依兰-伊通地堑方正断陷方正组的建立及其意义[J].地层学杂志,2003,27(2):138-145.
[45]姜贵周.中国东北中新生代盆地成因与演化[J].大庆石油学院学报,1997,21(l):l-6.
[46]姜在兴等.沉积学[M].北京:石油工业出版社,2003.
[47]荆凤,申旭辉,洪顺英等.基于遥感技术研究依兰-伊通断裂带[J].地震,2006,26(3):79-84.
[48]李福川.中国应加紧开发三江盆地的油气资源[J].俄罗斯中亚东欧市场,2005,5:46-47.
[49]李国玉,吕鸣岗等.中国含油气盆地图集[M].北京:石油工业出版社,2002.
[50]李国玉.世界油田图集[M].北京:石油工业出版社,2000.
[51]李锦轶.布列亚-佳木斯古板块的构成及演化[J].地学研究,1995,28:96-98.
[52]李思田,路凤香,林畅松.中国东部及邻区中新生代盆地演化和动力学背景[M].武汉:中国地质大学出版社,1997.
[53]李思田等.断陷盆地分析与聚煤规律[M].武汉:中国地质大学出版社,1988.
[54]李子俊,姜剑虹.三江-穆棱河中晚侏罗世沉积体系与聚煤模式[J].东北煤炭技术,1996,3:9-18.
[55]刘海山,郝天珧.勃利盆地侏罗系、白垩系、第三系古地磁研究及其意义[J].沈阳地质矿产所集刊.北京:地质出版社,1992.
[56]刘云武,唐振国,刘文龙.三江盆地演化特征与油气勘探方向[J].石油天然气学报(江汉石油学院学报),2006,28(2):1-5.
[57]刘招君,董清水,王嗣敏等.陆相层序地层学导论与应用[M].北京:石油工业出版社,2002.
[58]陆克政.含油气盆地分析[M].东营:石油大学出版社,2001.
[59]马金苹.大庆探区外围东部盆地群油气远景评价[D].吉林:吉林大学地球科学学院,2008.
[60]马小刚,王东坡,薛林福,王青海,王孔伟.三江盆地绥滨坳陷构造特征及其与油气的关系[J].长春科技大学学报,2000,30(1):46-50.
[61]马杏垣,刘和甫,王维襄.中国东部中、新生代裂陷作用和伸展构造[J].地质学报,1983,57(1):22-31.
[62]孟庆龙.大庆探区外围东部主要盆地数值模拟及其地质意义研究[D].吉林:吉林大学地球科学学院.2007.
[63]谯汉生,于兴河.裂谷盆地石油地质[M].北京:石油工业出版社,2004.
[64]郄瑞卿.大庆探区外围中、新生代断陷盆地群油气地质条件及远景评价[D].吉林:吉林大学地球科学学院.2009.
[65]任文忠.盆地分析的原理和方法[M].北京:煤炭工业出版社,1993.
[66]邵济安,唐克东,王成源等.那丹哈达地体的构造特征及演化[J].中国科学(B辑), 1991,7:744-751.
[67]邵济安,唐克东.中国东北地体与东北亚大陆边缘演化[M].北京:地震出版社,1995.
[68]邵济安,王成源,唐克东.乌苏里地区构造新探索[J].地质论评,1992,38(l):33-38.
[69]水谷申治郎,邵济安,张庆龙.1989.那丹哈达地体与东亚大陆中生代构造的关系[J].地质学报,63:204-215.
[70]宋兰斌.三江盆地绥滨坳陷中、新生界生油层早期评价[A].第三届全国沉积学大会论文摘要汇编,2004.
[71]孙永传,李蕙生编.碎屑岩沉积相和沉积环境[M].地质出版社,1986.
[72]唐振海,张亚金,赵玉珍.三江盆地绥滨坳陷石油地质特征.大庆石油地质与开发,2005,24(3):31-32.
[73]田在艺,张庆春.中国含油气沉积盆地论[M].北京:石油工业出版社,1996.
[74]童亨茂.伊通地堑边界断裂的性质与演化[J].地质力学学报,2002,8(1):35-42.
[75]汪新文.东北亚大陆边缘中新生带构造事件与演化序列[J].地质科技情报,1997,16(4):9-14.
[76]王鸿祯,杨森楠,李思田.中国东部及邻区中、新生代盆地发育及大陆边缘区的构造发展[J].地质学报,1983,57(3):213-223.
[77]王鸿祯.中国古地理图集[M].北京:地图出版社,1985.
[78]王骏,王东坡,C.A.乌沙科夫等.东北亚中新生代沉积类型及其地质特征[M].北京:地质出版社,1997:1-87.
[79]王良忱,张金亮.沉积环境和沉积相[M].北京:石油工业出版社,1999.
[80]王世辉,王立民,唐金生.兴安岭盆地群成盆机制及含油气远景评价[J].大庆石油地质与开发,2001,20(5):5-7.
[81]吴福元,曹林.东北亚地区的若干重要基础地质问题[J].世界地质,1999,18(2):1-13.
[82]萧德铭,王荣华,蔡天成等.俄罗斯东西伯利亚及远东地区含油气盆地[M].北京:石油工业出版社,2000.
[83]谢鸣谦.拼贴板块构造及其驱动机理-中国东部及相邻区的大地构造演化[M].北京:科学出版社,2000.
[84]杨建国,赵传本,张海桥.东北地区三江盆地海陆相侏罗-白垩系层序.第三届全国地层会议论文集[C].北京:地质出版社,2000,270-274.
[85]杨绍芳.泛三江盆地成藏机制分析[J].石油天然气学报,2005,27(4):413-415.
[86]于明德,王璞珺,王冶.三江盆地西大林子地区构造特征与圈闭样式[J].石油天然气学报(江汉石油学院学报),2008,30(1):1-6.
[87]云金表,罗笃清,李玉喜.东北地区中生代断陷盆地群构造演化与成油关系探讨[J].石油勘探与开发,1994,21(6):40-45.
[88]张梅生,彭向东,孙晓猛.中国东北区古生代构造古地理格局[J].辽宁地质, 1998, (2):91-96.
[89]张兴洲,周建波,迟效国等.东北地区晚古生代构造-沉积特征与油气资源[J].吉林大学学报(地球科学版),2008,38(5):719-725.
[90]张旭东.东北地区中生代断陷盆地群成盆机制及油气远景[D].吉林:吉林大学地球科学学院,2007.
[91]赵传本,叶得泉,魏德恩.中国油气区第三系(Ⅲ)[M].北京:石油工业出版社,1994.
[92]赵霞,于兴河,易荣龙等.三江盆地构造演化分析[J].内蒙古石油化工,2007,5:310-313.
[93]周建波,张兴洲,马志红等.中国东北地区的构造格局与盆地演化[J].石油与天然气地质,2009,30(5):530-538.
[94]朱建伟,刘招君,董清水,刘葵,郭巍.松辽盆地层序地层格架及油气聚集规律[J].石油地球物理勘探,2001,36(3):339-344.
[95]朱建伟等.三江-中阿穆尔盆地层对比、构造特征及含油气性分析[R].吉林大学地球科学学院,2004.
[96]邹艳荣,蔡玉兰.东北三江盆地演化分析[J].中国煤田地质,1997,9(1):19-21.