郯庐断裂带北段构造特征及构造演化序列
|
摘要
根据大量野外地质调查和盆地地震资料分析,认为郯庐断裂北段在中-新生代发生多期不同性质的活动,形成各具特色的构造变形现象。密山县知一镇敦密断裂韧性剪切带具有左旋走滑特征,其中黑云母~(40)Ar/~(36)Ar-~(39)Ar/~(36)Ar等时线年龄为161±3Ma,是郯庐断裂带被利用发生第二期左旋走滑运动并向北扩展到中国东北-俄罗斯远东地区的产物。四平市叶赫乡佳伊断裂带中负花状断裂形成于早白垩世早中期,是郯庐断裂北段在早白垩世遭受左旋走滑-拉张作用的典型代表。四平市石岭镇佳伊断裂大型走滑-逆冲断褶带、桦甸县敦密断裂"逆地堑"、沈阳-哈尔滨逆冲断裂形成于晚白垩世嫩江运动-晚白垩世末期,这一时期脆性右旋走滑-逆冲事件规模大,影响范围广,导致整个郯庐断裂北段遭受到强烈改造。佳伊断裂带和敦密断裂带中古近纪盆地在横剖面上呈不对称地堑,并且不对称地堑沿断裂带走向发生断、超方向左右变位,是郯庐断裂带北段在古近纪时受右旋走滑、伸展双重机制控制的产物。根据郯庐断裂带北段中-新生代不同地质时期变形特征,建立了郯庐断裂北段构造演化序列。即郯庐断裂北段构造演化分为左旋韧性剪切(J_2末期)、左旋张扭(K_1早中期)、右旋压扭(K_2晚期-末期)、右旋走滑断陷(E)和构造反转(E_3末期)五个阶段。其演化历史主要受控于环太平洋构造域的构造作用。
According to the plenty of field geological survey and basin earthquake data analysis,the author believed that multiperiodic and diversely characteristic activities happened and the tectonic deformed phenomena with characteristics were formed in the northern segment of Tancheng-Lujiang fault zone in Mesozoic-Cenozoic era.Sinistral strike-slip is characteristic of Dunhua-Mishan ductile shear zone near Zhiyi Town,Mishan County,among which the biotite ~(40)Ar/~(36)Ar-~(39)Ar/~(36)Ar isochron age is 161±3Ma.The isochron age is the product of Tancheng-Lujiang fault zone used and of the second left-lateral strike-slip happening and stretching from the Northeast,China to Far East,Russia.The negative flower faults of Yehe Town,Siping City in the Jiamusi-Yitong fault zone were formed in the early mid period of K_1,which is the typical representative of the northern segment of Tancheng-Lujiang fault zone suffering from left-lateral strike-slip and extension in K_1.Large-scale strike-slip and thrust fault-fold zone in Jiamusi-Yitong Fault of Shiling Town,Siping City,"obsequent graben"in Dunhua-Mishan fault of Huadian City and Shenyang-Harbin thrust fault were formed in the Nenjiang movement of later period of K_2-last stage of K_2,when the large-scale and influential extent of brittle right-lateral strikeslip and thrust event caused the northern segment of Tancheng-Lujiang fault zone strongly transformed.Palaeogene basin in the Jiamusi-Yitong and Dunhua-Mishan fault zones took on an asymmetric graben on its transverse profile and the asymmetric graben changed the direction of fault depression and overlap to right or left along the fault zone,which is the product of the northern segment of Tancheng-Lujiang fault zone controlled by right-lateral strike-slip and extensional double machanism in Palaeogene.According to the deformation features of the different geologic periods in the northern segment of Tancheng-Lujiang fault zone of Mesozoic-Cenozoic,tectonic evolution sequence in the northern segment of Tancheng-Lujiang was established,namely,left-lateral strike-slip tenacity shear stage (the last stage of J_2),left-lateral tenso-shear stage(the earlier-mid period of K_1),right-lateral compression shear stage(of later period of K_2-last stage of K_2),right-lateral strike-slip fault depression stage(E) and structural inversion(the end of E_3).The evolutionary history was mainly controlled by circum-Pacific tectonic domain.
According to the plenty of field geological survey and basin earthquake data analysis,the author believed that multiperiodic and diversely characteristic activities happened and the tectonic deformed phenomena with characteristics were formed in the northern segment of Tancheng-Lujiang fault zone in Mesozoic-Cenozoic era.Sinistral strike-slip is characteristic of Dunhua-Mishan ductile shear zone near Zhiyi Town,Mishan County,among which the biotite ~(40)Ar/~(36)Ar-~(39)Ar/~(36)Ar isochron age is 161±3Ma.The isochron age is the product of Tancheng-Lujiang fault zone used and of the second left-lateral strike-slip happening and stretching from the Northeast,China to Far East,Russia.The negative flower faults of Yehe Town,Siping City in the Jiamusi-Yitong fault zone were formed in the early mid period of K_1,which is the typical representative of the northern segment of Tancheng-Lujiang fault zone suffering from left-lateral strike-slip and extension in K_1.Large-scale strike-slip and thrust fault-fold zone in Jiamusi-Yitong Fault of Shiling Town,Siping City,"obsequent graben"in Dunhua-Mishan fault of Huadian City and Shenyang-Harbin thrust fault were formed in the Nenjiang movement of later period of K_2-last stage of K_2,when the large-scale and influential extent of brittle right-lateral strikeslip and thrust event caused the northern segment of Tancheng-Lujiang fault zone strongly transformed.Palaeogene basin in the Jiamusi-Yitong and Dunhua-Mishan fault zones took on an asymmetric graben on its transverse profile and the asymmetric graben changed the direction of fault depression and overlap to right or left along the fault zone,which is the product of the northern segment of Tancheng-Lujiang fault zone controlled by right-lateral strike-slip and extensional double machanism in Palaeogene.According to the deformation features of the different geologic periods in the northern segment of Tancheng-Lujiang fault zone of Mesozoic-Cenozoic,tectonic evolution sequence in the northern segment of Tancheng-Lujiang was established,namely,left-lateral strike-slip tenacity shear stage (the last stage of J_2),left-lateral tenso-shear stage(the earlier-mid period of K_1),right-lateral compression shear stage(of later period of K_2-last stage of K_2),right-lateral strike-slip fault depression stage(E) and structural inversion(the end of E_3).The evolutionary history was mainly controlled by circum-Pacific tectonic domain.
引文
Ben-Avrahanm Z.1992.Development of asymmetric basins along continental transform faults.Tectonophysics,215:209 -220
Bureau of Geology and Mineral Resources of Jilin Province.1988. Regional Geology of Jilin Province.Beijing:Geological Publishing House,546-562(in Chinese)
Bureau of Geology and Mineral Resources of Heilongjiang Province. 1989.Regional Geology of Heilongjiang Province.Beijing: Geological Publishing House,258 -291,617 -629(in Chinese)
Chen XH,Wang XF,Zhang Q,Chen BL,Chen ZL,Harrisson TM and Yin A.2000.Geochronologic study of the formation and evolution of the Tan-Lu fault.Journal of Changchun University of Science and Technology,30(3):215 -220(in Chinese with English abstract)
Ding RX,Shu P,Ji XY,Qu YM,Cheng RH and Zhang B.2007. SHRIMP zircon U-Pb age and geological meaning of reservoir volcanic rocks in Qingshen gas field of the Songliao basin,NE China.Journal of Jilin University(Earth Science Edition),37(3): 525 -530(in Chinese with English abstract)
Hou GT,Feng DC,Wang WM and Yang MH.2004.Reverse structures and their impacts on hydrocarbon accumulation in Songliao basin. Oil & Gas Geology,25(1 ):49 - 53(in Chinese with English abstract)
Huang QH,Tan W and Yang HC.1999.Stratigraphic succession and Chronostrata of Cretaceous in Songliao Basin.Petroleum Geology & Oilfield Development in Daqing,18(6):15 - 17(in Chinese with English abstract)
Huang JQ,Ren JS,Jiang CF et al.1977.An Outline of the tectonic Characteristic of China.Acta Geologica Sinica,51(2 ):117 -135 (in Chinese with English abstract)
Hoisch T.1989.A muscovite-biotite geothermometer.American Mineralogist,74:565 -572
Jia JT,Wang PJ and Wan XQ.2008.Chronostratigraphy of the Yingcheng Formation in the Songliao Basin,Cretaceous,NE China Geological Review,54(4):440 - 448(in Chinese with English abstract)
Li PW,Zhang SH and Shen NH.1997.The contrast of palaeomagnetic results between Nadahada area,Heilongjiang Province and Mino area,Japan,and its significance.Journal of Changchun University of Earth Sciences,27(1):62 - 66(in Chinese with English abstract)
Li SZ,Liu X,Suo YH,Liu LP,Qian CC,Liu XC Zhang GW and Zhao GC.2009.Triassic folding and thrusting in the Eastern Block of the North China Craton and the Dabie-Sulu orogen and its geodynamics. Acta Petrologica Sinica,25(9 ):2031 - 2049(in Chinese with English abstract)
Li XF,Chen QM,Zhang XH,Zhang CH,Zhang FS and Zhang ZW. 2002.The Yitong graben-the structural features and evolution of a strike slip fault basin.Petroleum Geology & Experiment,24(1):19 -24(in Chinese with English abstract)
Liu MQ,Yang BZ,Deng JG and Zhou YH.1993.Geological Tectonic Features and Evolution of the Yitong-Shulan Graben.Beijing: Geological Publishing House,42 -103(in Chinese)
Liu DL and Ma L 1997.Mesozoic tectonic evolution of continental margin in East Asia.Geoscience,11(4):444 - 451(in Chinese with English abstract)
Liu ZJ,Yang HL,Dong QS,Zhu JW,Guo W,Ye SQ,Liu R,Meng QT,Zhang HL and Gan SC.2009.Oil Shale in China.Beijing: Petroleum Industry Press,157 - 167(in Chinese with English abstract)
Marayama S and Seno T.1986.Orogeny and relative plate motions; Example of the Japanese Islands.Tectonophysics,127:305 -329
Marayama S,Isozaki Y,Kimura G and Terabayashi M.1997. Palaeogeographic maps of the Japanese Islands:Plate tectonic synthesis from 750Ma to the present.The Island Arc,6:121 - 142
Mizutani S.Shao JA and Zhang QL.1989.The Nadanhada terrane in relation to Mesozoic tectonics on continental margins of East Asia. Acta Geologica Sinica,63(3 ):204 - 215(in Chinese with English abstract)
Otofuji Y,Hayashida A and Torii M.1985.When was the Japan Sea opened? Paleomagnetic evidence from southwest Japan.In:Nasu N, Uyeda S,Kushiro I,Kobayashi K and Kagami H(eds.).Formation of Active Ocean Margins.Tokyo:Terra,551- 566
Ren JY,Lu YC,Li ST,Yang SG and Zhuang XG.1999.The tectonic evolution of Yishu graben and its depositional filling response. Scientia Geologica Sinica,34(2 ):196 - 203(in Chinese with English abstract)
Rosenberg CL and Stunitz H.2003.Deformation and recrystallization of plagioclase along a temperature gradient:An example from the Bergell tonalite.Journal of Structural Geology,25:389 -408
Shu P,Ding RX,Ji XY and Qu YM.2007.SHRIMP zircon geochronology of reservoir volcanic rocks in the Qingshen gas field, Songliao Basin.Acta Petrologica et Mineralogica,26(3):239 - 245 (in Chinese with English abstract)
Sun G,Sha JG and Wang YG et al.1989.Jurassic-cretaceous boundary of Dong' an zhen,Raohe,Heilongjiang with a new knowledge of Buchia.Acta Palaeontologica sinica,28(5):579 - 597(in Chinese with English abstract)
Sun XM,Long SX,Zhang MS,Uu XY and Hao FJ.2006.Discovery and timing of major thrustbelt in Jiamusi-Yitong fault zone.Oil & Gas Geology,27(5):637 -643(in Chinese with English abstract)
Sun XM,Zhu DF,Zheng CQ,Shan XL,Cheng RH and Sun QC.2007. Faulted structure features,formation epochs and reservoir significance of Mesozoic in eastern Songliao basin.Journal of Jilin University(Earth Science Edition ),37(6 ):1055 - 1063(in Chinese with English abstract)
Sun XM,Liu YJ,Sun QC,Han GQ,Wang SQ and Wang YD.2008. ~(40)Ar/~(39) Ar geochronology evidence of strike-slip movement in Dunhua-Mishan fault zone.Journal of Jilin University(Earth Science Edition),38(6):965 -972(in Chinese with English abstract)
Wan TF.1995.Evolution of Tancheng-Lujiang fault zone and palaeostress fields.Earth Science-Journal of China University of Geosciences,20 (5):526 -534(in Chinese with English abstract)
Wan TF.1996.Length and penetration depth of Tancheng-Lujiang fault zone in eastern Asia.Geoscience.10(4):518 - 525(in Chinese with English abstract)
Wan TF and Zhu H.1996.The maximum sinistral strike-slip and its forming age of Tancheng-Lujiang fault zone.Geological Journal of Universities,2(1):14 -27(in Chinese with English abstract)
Wang Y and Dou LR.1997.Formation time and dynamic characteristics of the northern part of the Tan Lu fault zone in east China Seismology and Geology,19(2):186 - 194
Wang Y.2006.The onset of the Tan-Lu fault movement in eastern China:Constraints from zircon(SHRIMP) and ~(40)Ar/~(39) Ar dating. Terra Nova,18(6):423-431
Wang YS,Zhu G,Chen W,Song CZ and Uu GS.2005. Thermochronologic information from the Tan-Lu fault zone and its relationship with the exhumation of the Dabie Mountains. Geochimica,34(3):193 -214(in Chinese with English abstract)
Wang YS,Zhu G,Shong CZ,Uu GS,Xiang BW,Li CC and Xie CL. 2006.~(40)Ar/~(39) Ar Geochronology records of transition from strike-slip to extension in the Tan-Lu fault zone on eastern terminal of the Dabie mountains.Chinese Journal of Geology,41(2 ):242 - 255(in Chinese with English abstract)
Wang XF,Li ZJ and Chen BL 2000.On Tan-Lu Fault Zone.Beijing: Geological Publishing House,1 - 40,222 - 244(in Chinese with English abstract)
Wang PJ,Liu WZ,Wang SX and Bian WH.2002a.~(40)Ar/~(39)Ar and K/ Ar dating on the volcanic rocks in the Songliao Basin,NE China: Constraints on stratigraphy and basin dynamics.International Journal of Earth Sciences,91:331 -340
Wang PJ,Ren YG,Shan XL,Sun SB,Wan CB and Bian WH.2002b. The Cretaceous volcanic succession around the Songliao Basin,NE China:Relationship between volcanism and sedimentation. Geological Journal,37(2):97 -115
Wang PJ,Chi YL,Ren YG,Shan XL and Wan CB.2003.Tephra event deposits and their application to the Correlation of dumb strata of the Songliao basin.Journal of Jilin University(Earth Science Edition), 34(suppl.),109 -114(in Chinese with English abstract)
Wang PJ,Chen FK,Chen SM,Siebel W and Satir M.2006. Geochemical and Nd-Sr-Pb isotopic composition of Mesozoic volcanic rocks in the Songliao basin,NE China Geochemical Journal,40: 149 -159
Wang PJ,GaoYF,Ren YG,Uu WZ and Zhang JG.2009.~(40)Ar/~(39) Ar age and geochemical features of mugearite from the Qingshankou Formation:Significances for basin formation,hydrocarbon generation and petroleum accumulation of the Songliao Basin in Cretaceous. Acta Petrologica Sinica,25(5 ):1178 - 1190(in Chinese with English abstract)
Wang YC.2001.The Petroliferous System and Oil-Gas Accumulation in Yitong Graben.Beijing:Petroleum Industry Press,119 - 129(in Chinese)
White JC and Mawer CK.1986.Extreme ductility of feldspars from a mylonite,Parry Sound,Canada J.Sruct.Geol.,8(2):133—143
Wu FY,Ge WC,Sun DY and Guo CL 2003.Discussions on the lithospheric thinning in eastern China Earth Science Frontiers.10 (3):51 -60(in Chinese with English abstract)
Wu GY,Liang X and Chen HJ.2007.An approach to the Tancheng-Lujiang fault zone:Its creation,evolution and character.Chinese Journal of Geology,42(1 ):160 - 175(in Chinese with English abstract)
Xu JW and Ma GF.1992.Review of the years of research on the Tancheng-Lujiang fault zone.Geological Review,38(4):316 -324 (in Chinese with English abstract)
Xu JW and Zhu G.1995.Discussion on tectonic models for the Tan-Lu fault zone,eastern China Jour.Geol.& Min.Res.North China, 10(2):121 - 134(in Chinese with English abstract)
Yao C,Jiao GH,Wang TH and Xin HS.2004.The Petroleum Tectonic Styles in China Beijing:Petroleum Industry Press,228(in Chinese)
Yu HL 1996.Structural characters of Dun-Mi fracture belts and its coal controlling rule.Coal Technology of Northeast China,(3 ):36 - 45 (in Chinese with English abstract)
Zhang H.1993.Discussion on the horizontal displacement of Dunhua-Mishan faulf zone.In:Memoirs of Shenyang Institute of Geology and Mineral Resources,Chinese Academy of Geological Sciences,(2): 35 -43(in Chinese with English abstract)
Zhang Q,Zhu G,Uu GS,Teyssier C and Dunlap WJ.2008.Sinistral transpressive deformation in the northern part of Zhangbaling uplift in the Tan-Lu fault zone and its ~(40)Ar/~(39) Ar dating.Earth Science Frontiers,15(3):234 -249(in Chinese with English abstract)
Zhang QL,Wang LS,Xie GA et al.2005.Discussion on northward extension of Tanlu fault zone and its tectonic regime transformation. Geological Journal of China universities,11(40):577 - 584(in Chinese with English abstract)
Zhang QY.1992.Ecologic characteristics of radiolarian fauna in the Nadanhada terrene.In:Memoirs of Shenyang Institute of Geology and Mineral Resources,Chinese Academy of Geological Sciences,(1): 18 -22(in Chinese with English abstract)
Zhang YQ,Zhao Y,Dong SW and Yang N.2004.Tectonic evolution stages of the Early Cretaceous rift basins in Eastern China and adjacent areas and their geodynamic background.Earth Science Frontiers,11(3):123 -133(in Chinese with English abstract)
Zhang YQ and Dong SW.2008.Mesozoic tectonic evolution history of the Tan-Lu fault zone,China:Advances and new understanding. Geological Bulletin of China,27(9):1371 - 1390(in Chinese with English abstract)
Zhang YX,Sun YS,Zhang XZ and Yang BJ.1999.Manzhouli-Suifenhe Global Geoscience Transect(GGT) of North China Beijing: Geological Publishing House,31(in Chinese)
Zhu G,Xu JW and Sun SQ.1995.Isotopic age evidence for the timing of strike-slip movement of the Lan-Lu fault zone.Geological Review, 41(5):452 -456(in Chinese with English abstract)
Zhu G,Liu GS,Song CZ and Wang DX.2000.Pulsative extensional activities of the Tan-Lu fault zone.Geological Journal of China Universities,6(3):396 -404(in Chinese with English abstract)
Zhu G,Song CZ,Wang DX,Uu GS and Xu JW.2001a.~(40)Ar-~(39) Ar geochronology strike-slip era in Tan-Lu fault zone and its tectonic implication.Science in China(Series D),44(11):2002 -2009
Zhu G,Wang DX,Liu GS,Song CZ,Xu JW and Niu ML 2001b. Extensional activities along the Tan-Lu fault zone and its geodynamic setting.Chinese Journal of Geology,36(3):269 - 278(in Chinese with English abstract)
Zhu G,Niu ML,Liu GS,Wang DX and Song CZ.2002a.Structural, magmatic and sedimentary events of the Tan-Lu fault belt during its Early cretaceous strike-slip movement Acta Geologica Sinica,76 (3):325 -334(in Chinese with English abstract)
Zhu G,Song CZ,Niu ML,Liu GS and Wang YS.2002b.Lithospheric textures of the Tan-Lu fault zone and their genetic analysis. Geological Journal of China Universities,8(3):248 - 256(in Chinese with English abstract)
Zhu G,Liu GS,Niu ML,Song CZ and Wang DX.2003.Transcurrent movement and genesis of the Tan-Lu fault zone.Geological Bulletin of China,22(3):200 -207(in Chinese with English abstract)
Zhu G,Uu GS,Dunlap WJ,Teyssier C,Wang YS and Niu ML 2004a ~(40)Ar-~(39) Ar geochronologicai constraints on syn-orogenic strke-slip movement of the Tan-Lu fault zone.Chinese Sci.Bull.,49(5):499 -508
Zhu G,Wang DX,Liu GS,Niu ML and Song CZ.2004b.Evolution of the Tan-Lu fault zone and its responses to plate movements in west pacific basin.Chinese Journal of Geology,39(1 ):36 - 49(in Chinese with English abstract)
Zhu G,Wang YS,Wang DX,Niu ML,Liu GS and Xie CL 2006a. Constraints of foreland sedimentation and deformation on synorogenic motion of the Tan-Lu fault zone.Chinese Journal of Geology,41(1): 102 - 121(in Chinese with English abstract)
Zhu G,Xu YD,Liu GS,Wang YS and Xie CL.2006b.Structural and deformational characteristics of strike-slippings along the middle-southern sector of the Tan-Lu fault zone.Chinese Journal of Geology, 41(2):226 -241(in Chinese with English abstract)
陈宣华,王小凤,张青,陈柏林,陈正乐,Harrison TM,Yin A.2000.郯庐断裂带形成演化的年代学研究.长春科技大学学报,30(3): 215-220
丁日新,舒萍,纪学雁,曲延明,程日辉,张斌.2007.松辽盆地庆深气田储层火山岩锆石U-Pb同位素年龄及其地质意义.吉林大学学报(地球科学版),37(3):525-530
黑龙江省地质矿产局.1989.黑龙江省区域地质志.北京:地质出版社,258-291,617-629
侯贵廷,冯大晨,王文明,杨默涵.2004.松辽盆地的反转构造作用及其对油气成藏的影响.石油与天然气地质,25(1):49-53
黄清华,谭伟,杨会臣.1999.松辽盆地白垩纪地层序列与年代地层.大庆石油地质与开发,18(6):15-17
黄汲清,任纪舜,姜春发等.1977.中国大地构造基本轮廓.地质学报,51(2):117-135
贾军涛,王璞珺,万晓樵.2008.松辽盆地断陷期白垩纪营城组的时代归属.地质论评,54(4):440-448
吉林省地质矿产局.1988.吉林省区域地质志.北京:地质出版社, 554-562
李朋武,张世红,申宁华.1997.黑龙江省那丹哈达与日本美浓地区古地磁结果对比及其意义.长春地质学院学报,27(1):62-66
李三忠,刘鑫,索艳慧,刘丽萍,钱存超,刘晓春,张国伟,赵国春. 2009.华北克拉通东部地块和大别-苏鲁造山带印支期褶皱-逆冲构造与动力学背景.岩石学报,25(9):2031-2049
李献甫,陈全茂,张学海,张春华,张付生,张振威.2002.伊通地堑-走滑断陷盆地的构造特征及演化.石油实验地质,24(1):19 -24
刘德来,马莉.1997.中生代东亚大陆边缘构造演化.现代地质,11 (4):444-451
刘茂强,杨丙中,邓俊国,周永辉.1993.伊通—舒兰地堑地质构造特征及其演化.北京:地质出版社,42-103
刘招君,杨虎林,董清水,朱建伟,郭巍,叶松青,柳蓉,孟庆涛,张海龙,甘树才.2009.中国油页岩.北京:石油工业出版社,157 -167
任建业,陆永潮,李思田,杨士恭,庄新国.1999.伊舒地堑构造演化的沉积充填响应.地质科学,34(2):196-203
水谷伸治郎,邵济安,张庆龙.1989.那丹哈达地体与东亚大陆边缘中生代构造的关系.地质学报,63(3):204-215
舒萍,丁日新,纪学雁,曲延明.2007.松辽盆地庆深气田储层火山岩锆石地质年代学研究.岩石矿物学杂志,26(3):239-245
孙革,沙金庚,王义刚等.1989.黑龙江饶河东安镇侏罗-白垩系界线及Buchia新知.古生物学报,28(5):579-597
孙晓猛,龙胜祥,张梅生,刘晓燕,郝福江.2006.佳木斯-伊通断裂带大型逆冲构造带的发现及形成时代.石油与天然气地质,27(5): 637-643
孙晓猛,朱德丰,郑常青,单玄龙,程日辉,孙庆春.2007.松辽盆地东缘中生代断裂构造特征、形成期次及其储层意义.吉林大学学报(地球科学版),37(6):1055-1063
孙晓猛,刘永江,孙庆春,韩国卿,王书琴,王英德.2008.敦密断裂带走滑运动的~(40)Ar/~(39)Ar年代学证据.吉林大学学报(地球科学版),38(6):965-972
徐嘉炜,马国烽.1992.郯庐断裂带研究的十年回顾.地质论评,38 (4):316-324
徐嘉炜,朱光.1995.中国东部郯庐断裂带构造模式讨论.华北地质矿产杂志,10(2):121-134
万天丰.1995.郯庐断裂带的演化与古应力场.地球科学-中国地质大学学报,20(5):526-534
万天丰.1996.郯庐断裂带的延伸与切割深度.现代地质.10(4): 518-525
万天丰,朱鸿.1996.郯庐断裂带的最大左行走滑断距及其形成时期.高校地质学报,2(1):14-27
王小凤,李中坚,陈柏林.2000.郯庐断裂带.北京:地质出版社,1- 40,222-244
王璞珺,迟元林,任延广,单玄龙,万传彪.2003.火山灰事件沉积在松辽盆地哑地层对比中的应用.吉林大学学报(地球科学版), 34(增刊):109-114
王璞珺,高有峰,任延广,刘万洙,张建光.2009.松辽盆地青山口组橄榄粗安岩:~(40)Ar/~(39)Ar年龄、地球化学及其成盆、成烃和成藏意义.岩石学报,25(5):1178-1190
王永春.2001.伊通地堑含油气系统与油气成藏.北京:石油工业出版社,10-50,119-129
王勇生,朱光,陈文,宋传中,刘国生.2005.郯庐断裂带热年代学信息及其与大别造山带折返的关系.地球化学,34(3):193-214
王勇生,朱光,宋传中,刘国生,向必伟,李长城,谢成龙.2006.大别山东端郯庐断裂带由走滑向伸展运动转换的~(40)Ar/~(39)Ar年代学记录.地质科学,41(2):242-255
吴福元,葛文春,孙德有,郭春丽.2003.中国东部岩石圈减薄研究中的几个问题.地学前缘,10(3):51-60
吴根耀,梁兴,陈焕疆.2007.试论郯城-庐江断裂带的形成、演化及其性质.地质科学,42(1):160-175
姚超,焦贵浩,王同和,邢厚松.2004.中国含油气构造样式.北京:石油工业出版社,228
于鸿禄.1996.敦密断裂带构造特征与控煤规律.东北煤炭技术,(3): 36-45
张宏.1993.敦化-密山断裂带平移问题讨论.见:中国地质科学院沈阳地质矿产研究所集刊,(2):35-43
张青,朱光,刘国生,Teyssier C,Dunlap WJ.2008.郯庐断裂带张八岭隆起北段的左旋走滑挤压变形及其~(40)Ar/~(39)Ar定年,地学前缘,15(3):234-249
张庆龙,王良书,谢国爱等.2005.郯庐断裂带北延及中新生代构造体制转换问题的探讨.高校地质学报,11(40):577-584
张勤运.1992.那丹哈达地体放射虫动物群的生态特征.见:中国地质科学院沈阳地质矿产研究所集刊,(1):18-22
张岳桥,赵越,董树文,杨农.2004.中国东部及邻区早白垩世裂陷盆地构造演化阶段地学前缘,11(3):123-133
张岳桥,董树文.2008.郯庐断裂带中生代构造演化史:进展与新认识.地质通报,27(9):1371-1390
张贻侠,孙运生,张兴洲,杨宝俊.1999.中国满洲里—绥芬河地学断面.北京:地质出版社,31
朱光,徐嘉炜,孙世群.1995.郯庐断裂带平移时代的同位素年龄证据.地质论评,41(5):452-456
朱光,刘国生,宋传中,王道轩.2000.郯庐断裂带的脉动式伸展活动.高校地质学报,6(3):396-404
朱光,宋传中,王道轩,刘国生,徐嘉炜.2001a.郯庐断裂带走滑时代的~(40)Ar-~(39)Ar年代学研究及其构造意义.中国科学(D辑),31 (3):250-256
朱光,王道轩,刘国生,宋传中,徐嘉炜,牛漫兰.2001b.郯庐断裂带的伸展活动及其动力学背景.地质科学,36(3):269-278
朱光,牛漫兰,刘国生,王道轩,宋传中.2002a.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件.地质学报,76(3):325-334
朱光,宋传中,牛漫兰,刘国生,王勇生.2002b.郯庐断裂带的岩石圈结构及其成因分析.高校地质学报,8(3):248-256
朱光,刘国生,牛漫兰,宋传中,王道轩.2003.郯庐断裂带的平移运动与成因.地质通报,22(3):200-207
朱光,刘国生,Dunlap WJ,Teyssier C,王勇生,牛漫兰.2004a.郯庐断裂带同造山走滑运动的~(40)Ar-~(39)Ar年代学证据.科学通报,49 (2):190-198
朱光,王道轩,刘国生,牛漫兰,宋传中.2004b.郯庐断裂带的演化及其对西太平洋板块运动的响应.地质科学,39(1):36-49
朱光,王勇生,王道轩,牛漫兰,刘国生,谢成龙.2006a.前陆沉积与变形对郯庐断裂带同造山运动的制约.地质科学,41(1):102 -121
朱光,徐佑德,刘国生,王勇生,谢成龙.2006b.郯庐断裂带中南段走滑构造特征与变形规律.地质科学,41(2):226-241
[1]吉林省地质矿产局.1985.1:20万磐石县幅地质图
[1]吉林省地质矿产局.1985.1:5万中心街幅
Bureau of Geology and Mineral Resources of Jilin Province.1988. Regional Geology of Jilin Province.Beijing:Geological Publishing House,546-562(in Chinese)
Bureau of Geology and Mineral Resources of Heilongjiang Province. 1989.Regional Geology of Heilongjiang Province.Beijing: Geological Publishing House,258 -291,617 -629(in Chinese)
Chen XH,Wang XF,Zhang Q,Chen BL,Chen ZL,Harrisson TM and Yin A.2000.Geochronologic study of the formation and evolution of the Tan-Lu fault.Journal of Changchun University of Science and Technology,30(3):215 -220(in Chinese with English abstract)
Ding RX,Shu P,Ji XY,Qu YM,Cheng RH and Zhang B.2007. SHRIMP zircon U-Pb age and geological meaning of reservoir volcanic rocks in Qingshen gas field of the Songliao basin,NE China.Journal of Jilin University(Earth Science Edition),37(3): 525 -530(in Chinese with English abstract)
Hou GT,Feng DC,Wang WM and Yang MH.2004.Reverse structures and their impacts on hydrocarbon accumulation in Songliao basin. Oil & Gas Geology,25(1 ):49 - 53(in Chinese with English abstract)
Huang QH,Tan W and Yang HC.1999.Stratigraphic succession and Chronostrata of Cretaceous in Songliao Basin.Petroleum Geology & Oilfield Development in Daqing,18(6):15 - 17(in Chinese with English abstract)
Huang JQ,Ren JS,Jiang CF et al.1977.An Outline of the tectonic Characteristic of China.Acta Geologica Sinica,51(2 ):117 -135 (in Chinese with English abstract)
Hoisch T.1989.A muscovite-biotite geothermometer.American Mineralogist,74:565 -572
Jia JT,Wang PJ and Wan XQ.2008.Chronostratigraphy of the Yingcheng Formation in the Songliao Basin,Cretaceous,NE China Geological Review,54(4):440 - 448(in Chinese with English abstract)
Li PW,Zhang SH and Shen NH.1997.The contrast of palaeomagnetic results between Nadahada area,Heilongjiang Province and Mino area,Japan,and its significance.Journal of Changchun University of Earth Sciences,27(1):62 - 66(in Chinese with English abstract)
Li SZ,Liu X,Suo YH,Liu LP,Qian CC,Liu XC Zhang GW and Zhao GC.2009.Triassic folding and thrusting in the Eastern Block of the North China Craton and the Dabie-Sulu orogen and its geodynamics. Acta Petrologica Sinica,25(9 ):2031 - 2049(in Chinese with English abstract)
Li XF,Chen QM,Zhang XH,Zhang CH,Zhang FS and Zhang ZW. 2002.The Yitong graben-the structural features and evolution of a strike slip fault basin.Petroleum Geology & Experiment,24(1):19 -24(in Chinese with English abstract)
Liu MQ,Yang BZ,Deng JG and Zhou YH.1993.Geological Tectonic Features and Evolution of the Yitong-Shulan Graben.Beijing: Geological Publishing House,42 -103(in Chinese)
Liu DL and Ma L 1997.Mesozoic tectonic evolution of continental margin in East Asia.Geoscience,11(4):444 - 451(in Chinese with English abstract)
Liu ZJ,Yang HL,Dong QS,Zhu JW,Guo W,Ye SQ,Liu R,Meng QT,Zhang HL and Gan SC.2009.Oil Shale in China.Beijing: Petroleum Industry Press,157 - 167(in Chinese with English abstract)
Marayama S and Seno T.1986.Orogeny and relative plate motions; Example of the Japanese Islands.Tectonophysics,127:305 -329
Marayama S,Isozaki Y,Kimura G and Terabayashi M.1997. Palaeogeographic maps of the Japanese Islands:Plate tectonic synthesis from 750Ma to the present.The Island Arc,6:121 - 142
Mizutani S.Shao JA and Zhang QL.1989.The Nadanhada terrane in relation to Mesozoic tectonics on continental margins of East Asia. Acta Geologica Sinica,63(3 ):204 - 215(in Chinese with English abstract)
Otofuji Y,Hayashida A and Torii M.1985.When was the Japan Sea opened? Paleomagnetic evidence from southwest Japan.In:Nasu N, Uyeda S,Kushiro I,Kobayashi K and Kagami H(eds.).Formation of Active Ocean Margins.Tokyo:Terra,551- 566
Ren JY,Lu YC,Li ST,Yang SG and Zhuang XG.1999.The tectonic evolution of Yishu graben and its depositional filling response. Scientia Geologica Sinica,34(2 ):196 - 203(in Chinese with English abstract)
Rosenberg CL and Stunitz H.2003.Deformation and recrystallization of plagioclase along a temperature gradient:An example from the Bergell tonalite.Journal of Structural Geology,25:389 -408
Shu P,Ding RX,Ji XY and Qu YM.2007.SHRIMP zircon geochronology of reservoir volcanic rocks in the Qingshen gas field, Songliao Basin.Acta Petrologica et Mineralogica,26(3):239 - 245 (in Chinese with English abstract)
Sun G,Sha JG and Wang YG et al.1989.Jurassic-cretaceous boundary of Dong' an zhen,Raohe,Heilongjiang with a new knowledge of Buchia.Acta Palaeontologica sinica,28(5):579 - 597(in Chinese with English abstract)
Sun XM,Long SX,Zhang MS,Uu XY and Hao FJ.2006.Discovery and timing of major thrustbelt in Jiamusi-Yitong fault zone.Oil & Gas Geology,27(5):637 -643(in Chinese with English abstract)
Sun XM,Zhu DF,Zheng CQ,Shan XL,Cheng RH and Sun QC.2007. Faulted structure features,formation epochs and reservoir significance of Mesozoic in eastern Songliao basin.Journal of Jilin University(Earth Science Edition ),37(6 ):1055 - 1063(in Chinese with English abstract)
Sun XM,Liu YJ,Sun QC,Han GQ,Wang SQ and Wang YD.2008. ~(40)Ar/~(39) Ar geochronology evidence of strike-slip movement in Dunhua-Mishan fault zone.Journal of Jilin University(Earth Science Edition),38(6):965 -972(in Chinese with English abstract)
Wan TF.1995.Evolution of Tancheng-Lujiang fault zone and palaeostress fields.Earth Science-Journal of China University of Geosciences,20 (5):526 -534(in Chinese with English abstract)
Wan TF.1996.Length and penetration depth of Tancheng-Lujiang fault zone in eastern Asia.Geoscience.10(4):518 - 525(in Chinese with English abstract)
Wan TF and Zhu H.1996.The maximum sinistral strike-slip and its forming age of Tancheng-Lujiang fault zone.Geological Journal of Universities,2(1):14 -27(in Chinese with English abstract)
Wang Y and Dou LR.1997.Formation time and dynamic characteristics of the northern part of the Tan Lu fault zone in east China Seismology and Geology,19(2):186 - 194
Wang Y.2006.The onset of the Tan-Lu fault movement in eastern China:Constraints from zircon(SHRIMP) and ~(40)Ar/~(39) Ar dating. Terra Nova,18(6):423-431
Wang YS,Zhu G,Chen W,Song CZ and Uu GS.2005. Thermochronologic information from the Tan-Lu fault zone and its relationship with the exhumation of the Dabie Mountains. Geochimica,34(3):193 -214(in Chinese with English abstract)
Wang YS,Zhu G,Shong CZ,Uu GS,Xiang BW,Li CC and Xie CL. 2006.~(40)Ar/~(39) Ar Geochronology records of transition from strike-slip to extension in the Tan-Lu fault zone on eastern terminal of the Dabie mountains.Chinese Journal of Geology,41(2 ):242 - 255(in Chinese with English abstract)
Wang XF,Li ZJ and Chen BL 2000.On Tan-Lu Fault Zone.Beijing: Geological Publishing House,1 - 40,222 - 244(in Chinese with English abstract)
Wang PJ,Liu WZ,Wang SX and Bian WH.2002a.~(40)Ar/~(39)Ar and K/ Ar dating on the volcanic rocks in the Songliao Basin,NE China: Constraints on stratigraphy and basin dynamics.International Journal of Earth Sciences,91:331 -340
Wang PJ,Ren YG,Shan XL,Sun SB,Wan CB and Bian WH.2002b. The Cretaceous volcanic succession around the Songliao Basin,NE China:Relationship between volcanism and sedimentation. Geological Journal,37(2):97 -115
Wang PJ,Chi YL,Ren YG,Shan XL and Wan CB.2003.Tephra event deposits and their application to the Correlation of dumb strata of the Songliao basin.Journal of Jilin University(Earth Science Edition), 34(suppl.),109 -114(in Chinese with English abstract)
Wang PJ,Chen FK,Chen SM,Siebel W and Satir M.2006. Geochemical and Nd-Sr-Pb isotopic composition of Mesozoic volcanic rocks in the Songliao basin,NE China Geochemical Journal,40: 149 -159
Wang PJ,GaoYF,Ren YG,Uu WZ and Zhang JG.2009.~(40)Ar/~(39) Ar age and geochemical features of mugearite from the Qingshankou Formation:Significances for basin formation,hydrocarbon generation and petroleum accumulation of the Songliao Basin in Cretaceous. Acta Petrologica Sinica,25(5 ):1178 - 1190(in Chinese with English abstract)
Wang YC.2001.The Petroliferous System and Oil-Gas Accumulation in Yitong Graben.Beijing:Petroleum Industry Press,119 - 129(in Chinese)
White JC and Mawer CK.1986.Extreme ductility of feldspars from a mylonite,Parry Sound,Canada J.Sruct.Geol.,8(2):133—143
Wu FY,Ge WC,Sun DY and Guo CL 2003.Discussions on the lithospheric thinning in eastern China Earth Science Frontiers.10 (3):51 -60(in Chinese with English abstract)
Wu GY,Liang X and Chen HJ.2007.An approach to the Tancheng-Lujiang fault zone:Its creation,evolution and character.Chinese Journal of Geology,42(1 ):160 - 175(in Chinese with English abstract)
Xu JW and Ma GF.1992.Review of the years of research on the Tancheng-Lujiang fault zone.Geological Review,38(4):316 -324 (in Chinese with English abstract)
Xu JW and Zhu G.1995.Discussion on tectonic models for the Tan-Lu fault zone,eastern China Jour.Geol.& Min.Res.North China, 10(2):121 - 134(in Chinese with English abstract)
Yao C,Jiao GH,Wang TH and Xin HS.2004.The Petroleum Tectonic Styles in China Beijing:Petroleum Industry Press,228(in Chinese)
Yu HL 1996.Structural characters of Dun-Mi fracture belts and its coal controlling rule.Coal Technology of Northeast China,(3 ):36 - 45 (in Chinese with English abstract)
Zhang H.1993.Discussion on the horizontal displacement of Dunhua-Mishan faulf zone.In:Memoirs of Shenyang Institute of Geology and Mineral Resources,Chinese Academy of Geological Sciences,(2): 35 -43(in Chinese with English abstract)
Zhang Q,Zhu G,Uu GS,Teyssier C and Dunlap WJ.2008.Sinistral transpressive deformation in the northern part of Zhangbaling uplift in the Tan-Lu fault zone and its ~(40)Ar/~(39) Ar dating.Earth Science Frontiers,15(3):234 -249(in Chinese with English abstract)
Zhang QL,Wang LS,Xie GA et al.2005.Discussion on northward extension of Tanlu fault zone and its tectonic regime transformation. Geological Journal of China universities,11(40):577 - 584(in Chinese with English abstract)
Zhang QY.1992.Ecologic characteristics of radiolarian fauna in the Nadanhada terrene.In:Memoirs of Shenyang Institute of Geology and Mineral Resources,Chinese Academy of Geological Sciences,(1): 18 -22(in Chinese with English abstract)
Zhang YQ,Zhao Y,Dong SW and Yang N.2004.Tectonic evolution stages of the Early Cretaceous rift basins in Eastern China and adjacent areas and their geodynamic background.Earth Science Frontiers,11(3):123 -133(in Chinese with English abstract)
Zhang YQ and Dong SW.2008.Mesozoic tectonic evolution history of the Tan-Lu fault zone,China:Advances and new understanding. Geological Bulletin of China,27(9):1371 - 1390(in Chinese with English abstract)
Zhang YX,Sun YS,Zhang XZ and Yang BJ.1999.Manzhouli-Suifenhe Global Geoscience Transect(GGT) of North China Beijing: Geological Publishing House,31(in Chinese)
Zhu G,Xu JW and Sun SQ.1995.Isotopic age evidence for the timing of strike-slip movement of the Lan-Lu fault zone.Geological Review, 41(5):452 -456(in Chinese with English abstract)
Zhu G,Liu GS,Song CZ and Wang DX.2000.Pulsative extensional activities of the Tan-Lu fault zone.Geological Journal of China Universities,6(3):396 -404(in Chinese with English abstract)
Zhu G,Song CZ,Wang DX,Uu GS and Xu JW.2001a.~(40)Ar-~(39) Ar geochronology strike-slip era in Tan-Lu fault zone and its tectonic implication.Science in China(Series D),44(11):2002 -2009
Zhu G,Wang DX,Liu GS,Song CZ,Xu JW and Niu ML 2001b. Extensional activities along the Tan-Lu fault zone and its geodynamic setting.Chinese Journal of Geology,36(3):269 - 278(in Chinese with English abstract)
Zhu G,Niu ML,Liu GS,Wang DX and Song CZ.2002a.Structural, magmatic and sedimentary events of the Tan-Lu fault belt during its Early cretaceous strike-slip movement Acta Geologica Sinica,76 (3):325 -334(in Chinese with English abstract)
Zhu G,Song CZ,Niu ML,Liu GS and Wang YS.2002b.Lithospheric textures of the Tan-Lu fault zone and their genetic analysis. Geological Journal of China Universities,8(3):248 - 256(in Chinese with English abstract)
Zhu G,Liu GS,Niu ML,Song CZ and Wang DX.2003.Transcurrent movement and genesis of the Tan-Lu fault zone.Geological Bulletin of China,22(3):200 -207(in Chinese with English abstract)
Zhu G,Uu GS,Dunlap WJ,Teyssier C,Wang YS and Niu ML 2004a ~(40)Ar-~(39) Ar geochronologicai constraints on syn-orogenic strke-slip movement of the Tan-Lu fault zone.Chinese Sci.Bull.,49(5):499 -508
Zhu G,Wang DX,Liu GS,Niu ML and Song CZ.2004b.Evolution of the Tan-Lu fault zone and its responses to plate movements in west pacific basin.Chinese Journal of Geology,39(1 ):36 - 49(in Chinese with English abstract)
Zhu G,Wang YS,Wang DX,Niu ML,Liu GS and Xie CL 2006a. Constraints of foreland sedimentation and deformation on synorogenic motion of the Tan-Lu fault zone.Chinese Journal of Geology,41(1): 102 - 121(in Chinese with English abstract)
Zhu G,Xu YD,Liu GS,Wang YS and Xie CL.2006b.Structural and deformational characteristics of strike-slippings along the middle-southern sector of the Tan-Lu fault zone.Chinese Journal of Geology, 41(2):226 -241(in Chinese with English abstract)
陈宣华,王小凤,张青,陈柏林,陈正乐,Harrison TM,Yin A.2000.郯庐断裂带形成演化的年代学研究.长春科技大学学报,30(3): 215-220
丁日新,舒萍,纪学雁,曲延明,程日辉,张斌.2007.松辽盆地庆深气田储层火山岩锆石U-Pb同位素年龄及其地质意义.吉林大学学报(地球科学版),37(3):525-530
黑龙江省地质矿产局.1989.黑龙江省区域地质志.北京:地质出版社,258-291,617-629
侯贵廷,冯大晨,王文明,杨默涵.2004.松辽盆地的反转构造作用及其对油气成藏的影响.石油与天然气地质,25(1):49-53
黄清华,谭伟,杨会臣.1999.松辽盆地白垩纪地层序列与年代地层.大庆石油地质与开发,18(6):15-17
黄汲清,任纪舜,姜春发等.1977.中国大地构造基本轮廓.地质学报,51(2):117-135
贾军涛,王璞珺,万晓樵.2008.松辽盆地断陷期白垩纪营城组的时代归属.地质论评,54(4):440-448
吉林省地质矿产局.1988.吉林省区域地质志.北京:地质出版社, 554-562
李朋武,张世红,申宁华.1997.黑龙江省那丹哈达与日本美浓地区古地磁结果对比及其意义.长春地质学院学报,27(1):62-66
李三忠,刘鑫,索艳慧,刘丽萍,钱存超,刘晓春,张国伟,赵国春. 2009.华北克拉通东部地块和大别-苏鲁造山带印支期褶皱-逆冲构造与动力学背景.岩石学报,25(9):2031-2049
李献甫,陈全茂,张学海,张春华,张付生,张振威.2002.伊通地堑-走滑断陷盆地的构造特征及演化.石油实验地质,24(1):19 -24
刘德来,马莉.1997.中生代东亚大陆边缘构造演化.现代地质,11 (4):444-451
刘茂强,杨丙中,邓俊国,周永辉.1993.伊通—舒兰地堑地质构造特征及其演化.北京:地质出版社,42-103
刘招君,杨虎林,董清水,朱建伟,郭巍,叶松青,柳蓉,孟庆涛,张海龙,甘树才.2009.中国油页岩.北京:石油工业出版社,157 -167
任建业,陆永潮,李思田,杨士恭,庄新国.1999.伊舒地堑构造演化的沉积充填响应.地质科学,34(2):196-203
水谷伸治郎,邵济安,张庆龙.1989.那丹哈达地体与东亚大陆边缘中生代构造的关系.地质学报,63(3):204-215
舒萍,丁日新,纪学雁,曲延明.2007.松辽盆地庆深气田储层火山岩锆石地质年代学研究.岩石矿物学杂志,26(3):239-245
孙革,沙金庚,王义刚等.1989.黑龙江饶河东安镇侏罗-白垩系界线及Buchia新知.古生物学报,28(5):579-597
孙晓猛,龙胜祥,张梅生,刘晓燕,郝福江.2006.佳木斯-伊通断裂带大型逆冲构造带的发现及形成时代.石油与天然气地质,27(5): 637-643
孙晓猛,朱德丰,郑常青,单玄龙,程日辉,孙庆春.2007.松辽盆地东缘中生代断裂构造特征、形成期次及其储层意义.吉林大学学报(地球科学版),37(6):1055-1063
孙晓猛,刘永江,孙庆春,韩国卿,王书琴,王英德.2008.敦密断裂带走滑运动的~(40)Ar/~(39)Ar年代学证据.吉林大学学报(地球科学版),38(6):965-972
徐嘉炜,马国烽.1992.郯庐断裂带研究的十年回顾.地质论评,38 (4):316-324
徐嘉炜,朱光.1995.中国东部郯庐断裂带构造模式讨论.华北地质矿产杂志,10(2):121-134
万天丰.1995.郯庐断裂带的演化与古应力场.地球科学-中国地质大学学报,20(5):526-534
万天丰.1996.郯庐断裂带的延伸与切割深度.现代地质.10(4): 518-525
万天丰,朱鸿.1996.郯庐断裂带的最大左行走滑断距及其形成时期.高校地质学报,2(1):14-27
王小凤,李中坚,陈柏林.2000.郯庐断裂带.北京:地质出版社,1- 40,222-244
王璞珺,迟元林,任延广,单玄龙,万传彪.2003.火山灰事件沉积在松辽盆地哑地层对比中的应用.吉林大学学报(地球科学版), 34(增刊):109-114
王璞珺,高有峰,任延广,刘万洙,张建光.2009.松辽盆地青山口组橄榄粗安岩:~(40)Ar/~(39)Ar年龄、地球化学及其成盆、成烃和成藏意义.岩石学报,25(5):1178-1190
王永春.2001.伊通地堑含油气系统与油气成藏.北京:石油工业出版社,10-50,119-129
王勇生,朱光,陈文,宋传中,刘国生.2005.郯庐断裂带热年代学信息及其与大别造山带折返的关系.地球化学,34(3):193-214
王勇生,朱光,宋传中,刘国生,向必伟,李长城,谢成龙.2006.大别山东端郯庐断裂带由走滑向伸展运动转换的~(40)Ar/~(39)Ar年代学记录.地质科学,41(2):242-255
吴福元,葛文春,孙德有,郭春丽.2003.中国东部岩石圈减薄研究中的几个问题.地学前缘,10(3):51-60
吴根耀,梁兴,陈焕疆.2007.试论郯城-庐江断裂带的形成、演化及其性质.地质科学,42(1):160-175
姚超,焦贵浩,王同和,邢厚松.2004.中国含油气构造样式.北京:石油工业出版社,228
于鸿禄.1996.敦密断裂带构造特征与控煤规律.东北煤炭技术,(3): 36-45
张宏.1993.敦化-密山断裂带平移问题讨论.见:中国地质科学院沈阳地质矿产研究所集刊,(2):35-43
张青,朱光,刘国生,Teyssier C,Dunlap WJ.2008.郯庐断裂带张八岭隆起北段的左旋走滑挤压变形及其~(40)Ar/~(39)Ar定年,地学前缘,15(3):234-249
张庆龙,王良书,谢国爱等.2005.郯庐断裂带北延及中新生代构造体制转换问题的探讨.高校地质学报,11(40):577-584
张勤运.1992.那丹哈达地体放射虫动物群的生态特征.见:中国地质科学院沈阳地质矿产研究所集刊,(1):18-22
张岳桥,赵越,董树文,杨农.2004.中国东部及邻区早白垩世裂陷盆地构造演化阶段地学前缘,11(3):123-133
张岳桥,董树文.2008.郯庐断裂带中生代构造演化史:进展与新认识.地质通报,27(9):1371-1390
张贻侠,孙运生,张兴洲,杨宝俊.1999.中国满洲里—绥芬河地学断面.北京:地质出版社,31
朱光,徐嘉炜,孙世群.1995.郯庐断裂带平移时代的同位素年龄证据.地质论评,41(5):452-456
朱光,刘国生,宋传中,王道轩.2000.郯庐断裂带的脉动式伸展活动.高校地质学报,6(3):396-404
朱光,宋传中,王道轩,刘国生,徐嘉炜.2001a.郯庐断裂带走滑时代的~(40)Ar-~(39)Ar年代学研究及其构造意义.中国科学(D辑),31 (3):250-256
朱光,王道轩,刘国生,宋传中,徐嘉炜,牛漫兰.2001b.郯庐断裂带的伸展活动及其动力学背景.地质科学,36(3):269-278
朱光,牛漫兰,刘国生,王道轩,宋传中.2002a.郯庐断裂带早白垩世走滑运动中的构造、岩浆、沉积事件.地质学报,76(3):325-334
朱光,宋传中,牛漫兰,刘国生,王勇生.2002b.郯庐断裂带的岩石圈结构及其成因分析.高校地质学报,8(3):248-256
朱光,刘国生,牛漫兰,宋传中,王道轩.2003.郯庐断裂带的平移运动与成因.地质通报,22(3):200-207
朱光,刘国生,Dunlap WJ,Teyssier C,王勇生,牛漫兰.2004a.郯庐断裂带同造山走滑运动的~(40)Ar-~(39)Ar年代学证据.科学通报,49 (2):190-198
朱光,王道轩,刘国生,牛漫兰,宋传中.2004b.郯庐断裂带的演化及其对西太平洋板块运动的响应.地质科学,39(1):36-49
朱光,王勇生,王道轩,牛漫兰,刘国生,谢成龙.2006a.前陆沉积与变形对郯庐断裂带同造山运动的制约.地质科学,41(1):102 -121
朱光,徐佑德,刘国生,王勇生,谢成龙.2006b.郯庐断裂带中南段走滑构造特征与变形规律.地质科学,41(2):226-241
[1]吉林省地质矿产局.1985.1:20万磐石县幅地质图
[1]吉林省地质矿产局.1985.1:5万中心街幅
版权所有：© 2023 中国地质图书馆 中国地质调查局地学文献中心