吐哈盆地台北凹陷北部山前带二叠系油气勘探前景初步分析
|
摘要
吐哈盆地是中国西部最重要的含油气盆地之一,二叠系在新疆各个盆地中广泛发育,并且是重要的烃源岩层。吐哈盆地台北凹陷北部的博格达山前构造带发育二叠系深湖相泥岩,具有较高的生烃潜能。但由于构造复杂、地震品质差且很少有钻井钻遇二叠系,因此对该区带二叠系油气勘探潜力评价受到极大限制,同时也制约了台北凹陷二叠系生烃前景评价。本文试图根据博格达南缘二叠系发育情况,为本区的油气勘探前景提供新的研究资料。
本文从地质构造背景、研究区二叠世沉积环境、烃源岩评价地化指标以及盆地的热演化特征四个方面探讨了博格达南缘台北凹陷山前带二叠系油气勘探潜力,并进一步推测台北凹陷二叠系生烃前景。
从构造背景入手,结合岩性特征、沉积特征以及地球化学数据分析,探讨了本区二叠纪构造-沉积格局及沉积环境特征。认为早二叠世吐哈盆地及邻区发育了一系列的裂谷盆地,研究区为一槽型深水盆地:中二叠世,研究区在继承早二叠世裂谷型深水盆地的基础上,逐渐向坳陷盆地演化。晚二叠世,博格达地区发生隆升,从此,本区由裂谷-坳陷盆地转变为前陆盆地。
通过系统分析有机质丰度、有机质类型以及有机质成熟度,对研究区二叠系烃源岩进行了综合评价。下二叠统烃源岩残留面积小、热演化程度高。中二叠统的烃源岩分布广、丰度高、类型好、而且均已成熟,为本区重要烃源岩层。上二叠统梧桐沟组有机质总体具丰度低,类型差及成熟度较低等特征,综合评价为较差烃源岩。
在进行区域热事件以及热演化趋势研究的基础上,采用古温标法(镜质体反射率、磷灰石裂变径迹、包裹体测温等)进行热史研究。研究表明,盆地热演化经历二叠纪的急速升温过程,三叠纪-早白垩世的缓慢降温过程以及第三纪-现今的基本稳定阶段。二叠系烃源岩自印支期末开始生烃,燕山期至喜山期大量生烃排烃。
The Tulufan-Hami basin is one of the most important oil/gas enriched large basins in the west of China. The Permian which is the important hydrocarbon mother rock exists in all of the basins in xinjiang.There is Permian lake facies mudstone which has big potence to produce hydrocarbon in the front structural belt of Bogeda mountain in the north of Taibei depression. It is difficult to evaluate the exploration foreground of the north structural belt and Taibei depressed basin,because the seismic data is bad and the tectonic is complex and there is less well in which the Permian can be reached In this article , some new messages of the foreground of exploration can be supplied according to the situation of the existence of Permian. The potence of producing hydrocarbon of the Permian in the south of Bogeda mountain is talked by the analysis of geological background and the character of lithology and sediment and the geochemical character of the mother rock and the trait of thermal evolution of the basin. According to that the potence to produce hydrocarbon of the Permian in Taibei depressed basin can be presumed.
The tectonic-sedimentary and the depositional environment framework is talked by the analysis of the tectonic background, the trait of lithology and sediment the data of geochemistry. The conclusion is that:There is a deep basin which belongs to some of the rifted basin in Tulufan-Hami basin and its adjacent area in the region of interest in Early Permain ; The deep basin turned into depression basin in Middle Permain;Then the depression basin turned into foreland basin in Late Permain when the mountain turned up in the Bogeda region.
The hydrocarbon mother rock of the Permain has been evaluated by the analysis of the Abundance,the Type and the Maturity of organic material. The conclusion is that:There is little hydrocarbon mother rock of early Permain remained of which the thermal evolution is deep; The mother rock of Middle Permain which is good in the Abundance,the Type and the Maturity is widespread. The mother rock of Late Permain of which the Abundance and the Maturity are low and the type is bad is evaluated as bad hydrocarbon mother rock..
The thermal history is reaserched using the palaeotemperature scale means(i?o, fission track and inclusion thermometry) by the analysis of the regional thermal event and the tendency of thermal evolution. It is proved that the basins have experienced fast heating course in Permian, slowly cooling course in Triassic-Early Crataceous and primary steady course in Tertiary to nowadays; The hydrocarbon mother rock of the Permain began to produce hydrocarbon in late Indo Chinese epoch and bleeded off hydrocarbon in big mass in Yanshan-xishan epoch.
本文从地质构造背景、研究区二叠世沉积环境、烃源岩评价地化指标以及盆地的热演化特征四个方面探讨了博格达南缘台北凹陷山前带二叠系油气勘探潜力,并进一步推测台北凹陷二叠系生烃前景。
从构造背景入手,结合岩性特征、沉积特征以及地球化学数据分析,探讨了本区二叠纪构造-沉积格局及沉积环境特征。认为早二叠世吐哈盆地及邻区发育了一系列的裂谷盆地,研究区为一槽型深水盆地:中二叠世,研究区在继承早二叠世裂谷型深水盆地的基础上,逐渐向坳陷盆地演化。晚二叠世,博格达地区发生隆升,从此,本区由裂谷-坳陷盆地转变为前陆盆地。
通过系统分析有机质丰度、有机质类型以及有机质成熟度,对研究区二叠系烃源岩进行了综合评价。下二叠统烃源岩残留面积小、热演化程度高。中二叠统的烃源岩分布广、丰度高、类型好、而且均已成熟,为本区重要烃源岩层。上二叠统梧桐沟组有机质总体具丰度低,类型差及成熟度较低等特征,综合评价为较差烃源岩。
在进行区域热事件以及热演化趋势研究的基础上,采用古温标法(镜质体反射率、磷灰石裂变径迹、包裹体测温等)进行热史研究。研究表明,盆地热演化经历二叠纪的急速升温过程,三叠纪-早白垩世的缓慢降温过程以及第三纪-现今的基本稳定阶段。二叠系烃源岩自印支期末开始生烃,燕山期至喜山期大量生烃排烃。
The Tulufan-Hami basin is one of the most important oil/gas enriched large basins in the west of China. The Permian which is the important hydrocarbon mother rock exists in all of the basins in xinjiang.There is Permian lake facies mudstone which has big potence to produce hydrocarbon in the front structural belt of Bogeda mountain in the north of Taibei depression. It is difficult to evaluate the exploration foreground of the north structural belt and Taibei depressed basin,because the seismic data is bad and the tectonic is complex and there is less well in which the Permian can be reached In this article , some new messages of the foreground of exploration can be supplied according to the situation of the existence of Permian. The potence of producing hydrocarbon of the Permian in the south of Bogeda mountain is talked by the analysis of geological background and the character of lithology and sediment and the geochemical character of the mother rock and the trait of thermal evolution of the basin. According to that the potence to produce hydrocarbon of the Permian in Taibei depressed basin can be presumed.
The tectonic-sedimentary and the depositional environment framework is talked by the analysis of the tectonic background, the trait of lithology and sediment the data of geochemistry. The conclusion is that:There is a deep basin which belongs to some of the rifted basin in Tulufan-Hami basin and its adjacent area in the region of interest in Early Permain ; The deep basin turned into depression basin in Middle Permain;Then the depression basin turned into foreland basin in Late Permain when the mountain turned up in the Bogeda region.
The hydrocarbon mother rock of the Permain has been evaluated by the analysis of the Abundance,the Type and the Maturity of organic material. The conclusion is that:There is little hydrocarbon mother rock of early Permain remained of which the thermal evolution is deep; The mother rock of Middle Permain which is good in the Abundance,the Type and the Maturity is widespread. The mother rock of Late Permain of which the Abundance and the Maturity are low and the type is bad is evaluated as bad hydrocarbon mother rock..
The thermal history is reaserched using the palaeotemperature scale means(i?o, fission track and inclusion thermometry) by the analysis of the regional thermal event and the tendency of thermal evolution. It is proved that the basins have experienced fast heating course in Permian, slowly cooling course in Triassic-Early Crataceous and primary steady course in Tertiary to nowadays; The hydrocarbon mother rock of the Permain began to produce hydrocarbon in late Indo Chinese epoch and bleeded off hydrocarbon in big mass in Yanshan-xishan epoch.
引文
1.柳益群,冯乔,周立发,等.吐哈盆地二叠系含油结核研究及生油前景分析[J].石油学报,2002,23(5):40-45
2.陶明信.吐-哈盆地大地构造环境分析-兼论大陆板内盆地与造山带的成因关系[J].沉积学报,1994,12(4):40-50
3.李文厚,周立发,柳益群,等.吐哈盆地沉积格局与沉积环境的演变[J].新疆石油地质,1997,18(2):135-141
4.邢秀娟,周鼎武,柳益群,等.吐-哈盆地及周缘早二叠世火山岩地球化学特征及大地构造环境探讨[J].新疆地质,2004,22(1):50-55
5.吕锡敏.吐哈盆地构造特征与油气赋存[J].江汉石油学院学报,2001,23(2):75-80
6.张恺.吐哈盆地板块构造条件及其对油气的控制作用[J].新疆石油地质.2000,21(4):261-266
7.卫延召,戴金星,赵长毅.吐哈盆地台北凹陷西部油源浅析[J].石油实验地质,2001,23(2):191-194
8.袁明生,李华明,王志勇.吐哈盆地油源研究新进展[J].新疆石油地质,2001,22(1):17-21
9.徐论勋,李建民,李景义,等.吐哈盆地台北凹陷侏罗系烃源岩特征[J].江汉石油学院学报,2004,26(2):13-15
10.张振英,邵龙义,等.吐哈盆地台北凹陷西部弧形构造带混源原油特征[J].石油学报,2005,26(2):15-20
11.王宗秀,李涛,周高志,等.博格达山晚石炭纪造山活动的变形地质记录[J].地学前缘,2003,10(1):63-69
12.王作勋,邬继易,吕喜朝,等.天山多旋回构造演化及成矿[M].北京:科学出版社,1990:1-217
13.HendrixM S,Graham S A,Carroll A R,et al.Sedimentary record and climatic imp lications of recurrent deformation in the Tian Shan:Evidence from Mesozoic strata of the north Tarim,south Junggar,and Turpan basins,northwest China[J].Geological Society of America Bulletin,1992,104:53-79
14.喻春辉,蒋宜勤,刘树辉,等.准噶尔盆地与吐哈盆地侏罗纪沉积边界的讨论[J].岩相古地理,1996,16:48-54
15.张传恒,刘典波,张传林,等.新疆博格达山初始隆升时间的地层学标定[J].地学前缘,2005,12(1):294-302
16.沈传波,梅廉夫,刘麟,等.新疆博格达山裂变径迹年龄特征及其构造意义[J].石油天然气学报(江汉石油学院学报),2005,27(2):273-277
17.朱文斌,舒良树,万景林,等.新疆博格达山-哈尔里克山白垩纪以来剥露历史的裂变径迹证据[J].地质学报,2006,80(1):16-22
18.汪新伟,汪新文,马永生.新疆博格达山的构造演化及其与油气的关系[J].现代地质,2007,21(1):116-124
19.赵重远.论含油气盆地的整体动态综合分析,见:含油气盆地地质学研究进展,赵重远等主编,西北大学出版社,1993,3-18
20.肖序常,汤耀庆,冯益民,等.新疆北部及其邻区大地构造[M].北京:地质出版社,1992:1-169
21.胡霭琴,等著.新疆北部地质演化及成岩成矿规律[M].北京:科学出版社,1997:1-120
22.周鼎武,柳益群,邢秀娟,等.新疆吐-哈、三塘湖盆地二叠纪玄武岩形成古构造环境恢复及区域构造背景示踪[J].中国科学,2006,36(2):143-153
23.周济元,茅燕石,黄志勋,等.东天山古大陆边缘火山地质[M].成都:成都科技大学出版社,1994:1-280
24.赵文智.吐鲁番-哈密盆地的构造特征[J].石油学报,1992,13(3):9-18
25.周立发.准噶尔盆地南缘山前带构造演化与油气成藏.2007,内部报告
26.李锦轶,何国琦,徐新,等.新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J].地质学报,2006,80(1):148-168
27.王宗秀.博格达山链的造山活动与山体形成演化.博士论文,2003
28.朱文斌,马瑞士,等.新疆觉罗塔格山与吐哈盆地的构造接触关系[J].大地构造与成矿学,2001,25(2):128-135
29.冯先岳.论新疆地震地质特征[J].地震地质,1985,7(2):35-43
30.冯先岳.天山活动断裂与地震[J].新疆地质,1986,4(3)
31.柳益群,周鼎武,冯乔,等.吐鲁番拗陷北部及柴窝堡凹陷油气勘探前景综合评价.西北大学地质系,中石化西部新区勘探指挥部.2005,内部报告
32.马瑞士,王赐银,叶尚夫.东天山构造格架及地壳演化[M].南京:南京大学出版社,1993:1-100
33.何国琦,李茂松,刘德权.中国新疆古生代地壳演化与成矿[M].乌鲁木齐:新疆人民出版社.1994:1-437
34.成守德,徐新.新疆及邻区大地构造编图研究[J].新疆地质,2001,19(1):33-37
35.冯益民,朱宝清,杨军录,张开春.东天山大地构造及演化[J].新疆地质,2002,20(4):309-314
36.陈富文,何国琦,李华芹,等.论东天山觉罗塔格造山带的大地构造属性[J].中国地质,2003,30(4):361-366
37.李锦轶.新疆东部新元古代晚期和古生代构造格局及其演变[J].地质论评,2004,50(3):304-322
38.孙桂华,李锦轶,高立明,等.新疆东部哈尔里克山闪长岩锆石SHRIMP U-Pb定年及其地质意义[J].地质论评,2005,51(4):463-469
39.吴绍祖.新疆早二叠世古气侯[J].新疆地质,1996,14(3):270-277
40.周鼎武,柳益群,等.新疆吐-哈、三塘湖盆地二叠纪玄武岩形成古构造环境恢复及区域构造背景示踪[J].中国科学,2006,36(2):143-153
41.苗建宇.新疆北部主要盆地二叠系烃源岩沉积环境与生烃特征.博士论文,2001
42.周立发,李文厚,等.博格达南缘构造形成与沉积环境.西北大学地质系吐哈盆地研究 队,1994,内部报告
43.周立发,等.柴窝堡盆地前侏罗系油气勘探前景综合分析.西北大学地质系,1998,内部报告
44.姬金生,陶洪祥,曾章仁,等.东天山康古尔塔格金矿带地质与成矿[M].北京:地质出版社,1994
45.Cullers R L et al;Rare earth distributions in clay minerals and clay-sized fractinal of the lower Permian Havensville and Eskridge shales of Kansas and Oklahoma[M];Geochim.et Cosmochim.Acta;1975
46.Roaldset E.Rare earth elements in quaternary clays of numedel area,Southern Norway[J].Lithos,1973,6:349-372
47.Ronov A B,Yaroshevsky A A.Chemical structure of the Earth's crust[J].Genkhimia,1967(11):1 285-1 309(in Russian with English abstract)
48.Gleadow,A.J.W.,Duddy,I.R..A natural long-term annealing experiment for apatite.Nuclear Tracks and Radiation Measurements,1981,5(1-2):169-174
49.Muecke T W.Formation fines and factors controlling their movement in porous media[J].JPT,1979(2):144-50.
50.Bhatia M R.Rare earth element geochemistry of Australian Paleozoic graywackes and mudrocks:Provenance and tectonic control[J].Sediment.Geol.,1985,45:97-113
51.Bhatia M R.Plate tectonics and geochemical composi-tion of sandstones[J].The Journal of Geology,1983,91:611-627
52.Taylor S R,Mclennan S M.The continental crust:its composition and evolution;an examination of the geo-chemical record preserved in sedimentary rocks[M].Oxford:Blackwell Scientific Publications,1985:1-312
53.Bhatia M R,Crook K A W.Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J].Contrib Mineral Petro,1986,(92):181-193
54.Hatch J R,Leventhal J S.Relationship between inferred redox potential of the depositional environment and geochemistry of the Upper Pennsylvanian(Missourian)Stark Shale[J].Member of the Dennis Limestone,Wabaunsee County,Kansas,U.S.A.Chemical Geology,1992,99:65-82
55.彼得斯KE,莫尔多万J.M,等.生物标记化合物指南-古代沉积物和石油中分子化石的解释[M].北京:石油工业出版社,1995
56.周鼎武,董云鹏,等.“磨拉石建造”和“不整合”在地层对比中的意义.地质论评,1996,43(5):416-423
57.苗建宇,周立发,等.新疆北部中二叠统烃源岩地球化学特征与沉积环境[J].地质学报,2004,534-541
58.方世虎,贾承造,等.准噶尔盆地二叠纪盆地属性的再认识及其构造意义[J].地学前缘,2006,13(3):108-121
59.汪新伟,汪新文,马永生.新疆博格达山的构造演化及其与油气的关系[J].现代地质, 2007,21(1):116-124
60.王丹.新疆博格达山南缘上二叠统精细层序地层学研究,硕士论文,2006
61.Tissot B P.Califet-Debyser Y.Derco G,Oudin J L.Origin and evolution of hydrocarbons in early Toarcian Shales.Paris Basin.AAPG Bulletin,1971,55:2177-2193
62.Tissot B P.Durand B.Espitalie J.Combaz.A Influences of the nature and diagenesis of organic matter in the formation of petroleum.AAPG Bulletin,1974,58:499-506
63.Tissot B P,Welte D H.Petroleum formation and oceurence.New York:Springer-Verlag.1978
64.张厚福,张万选.石油地质学.第二版[M].北京:石油工业出版社,1989.152-161
65.程克明,王铁冠,等.烃源岩地球化学[M].科学出版社,1995
66.张厚福.石油地质学[M].北京:石油工业出版社,1989.39-100
67.武守诚.石油资源地质评价导论[M].北京:石油工业出版社,1994.98-125
68.王铁冠,钟宁宁,熊波,等.源岩生烃潜力的有机岩石学评价方法[J].石油学报,1994,15(4):9-16
69.王铁冠,钟宁宁,侯读杰,等.低熟油形成机理与分布[M].北京:石油工业出版社,1995
70.李贤庆,马安来,等.烃源岩有机岩石学研究方法与应用[M].重庆大学出版社,1997
71.王启军,陈建渝.油气地球化学[M].武汉:中国地质大学出版社,1988
72.B.P.蒂索、D.H.威尔特著,郝石生等译,石油形成和分布[M].北京:石油工业出版社,1982
73.李艳红,金奎励.烃源岩成熟度评价指标及选取[J].地质地球化学,2000,28(2):94-96
74.许怀先.石油地质实验测试技术与应用[M].石油工业出版社,2001
75.覃克,赵密福.惠民凹陷临南斜坡带油气成藏模式[J].石油大学学报(自然科学版),2002,26(6):21-24
76.Gleadow A J W,Dubby I R,Lovering J F.Fission track analysis:a new tool for the evaluation of thermal histories and hydrocarbon potential.Aust Petrol Explor Assoc J,1983,23:93-102
77.Naeser C W.Thermal history of sedimentary basins:fission-track dating of subsurface rocks.In:Scholle P A,Schluger R P,eds.Aspect of diagenesis.SEPM special Publication.1979,26:109-112
78.Wagner G A,Van den Haute P.Fission-track-dating.Dordrecht:Enke Verlag-Kluwer Academic Publishers,1992,180-285
79.Green P F,Duddy I R,Laslett G M,et al.Thermal annealing of fission tracks in apatite 4.Qualitative modeling techniques and extensions to geological timescales.Chem Geol,1989,79:155-182
80.Hurford A J,Green P F.A users,guide to fission-track dating calibration.Earth Planet Sci Lett,1982,59:343-354
81.王瑜.构造热年代学-发展与思考.地学前缘,2004,11(40):435-443
82.吴中海,吴珍汉.裂变径迹法在研究造山带隆升过程中的应用介绍.地质科技情报,1999,18(4):27-32
83.康铁笙,王世成.地质热历史研究的裂变径迹法[M].北京:科学出版社,1991.25-40
84.周中毅,潘长春.沉积盆地古地温测定方法及其应用[M].广州:广东科技出版社,1992.1-103
85.胡圣标,张容燕,周礼成.油气盆地热历史恢复方法[J].勘探家,1998,3(4):52-54
86.McKenzie D P.Some remarks on the development of sedimentary basins.Earth Planet Sci Lett,1978,40:25-32
87.Jarvis G T,McKenzie D P.Sedimentary basin formation with finite extension rates.Earth Planet Sci Lett,1980,48:42-52
88.Royden L,Keen C E.Rifting processes and thermal evolution of the continenta lmargin of eastern Canada determined from subsidence curves.Earth Planet Sci Lett,1980,51:343-361
89.Keen C E,Dehler S A.Stretching and subsidence:rifting of conjugate margins in the North Atlantic region.Tectonics,1993,12:1219-1229
90.韩宝福,何国琦,等.后碰撞幔源岩浆活动、底垫作用及准噶尔盆地基底的性质[J].中国科学,1999,29(1):16-21
91.李锦轶,肖序常,等.新疆北部晚石炭世至晚三叠世地壳热演化-东准噶尔考克塞尔盖山荒草坡群的~(40)Ar-~(39)Ar定年[J].地质学报,2000,74(4):303-311
92.赵明,舒良树,等.东疆哈尔里克变质地带变质作用特征及形成构造环境研究[J].高校地质学报,1997,3(1):40-50
93.赵明,舒良树,朱文斌,等.东疆哈尔里克变质带的U-Pb年龄及其地质意义[J].地质学报,2002,76(3):379-383
94.孙桂华.新疆东部哈尔里克山构造变形研究.地质科学院硕士学位论文,2004
95.顾连兴,于春水,等.博格达上大河沿岩体铷-锶同位素年龄及其地质意义[J].矿物岩石地球化学通报,2001,19(1):19-21
96.蔡忠贤,陈发景,等.准噶尔盆地的类型和构造演化[J].地学前缘,2007(4):431-440
97.李向东,王庆明.天山后碰撞阶段构造演化的新信息-来自阿吾拉勒山中段动力变质岩的证据[J].地质论评,1998,44(4):443-448
98.陈富文,李华芹,等.新疆东部金窝子金矿成因讨论-同位素地质年代学证据[J].地质论评,1999,45(3):246-253
99.李华芹,陈富文,等.新疆东部印支期成岩成矿年代学新证据[J].地质学报,2005
100.陈富文,李华芹,等.中国阿尔泰造山带燕山期成岩成矿同位素年代学新证据[J].科学通报,1999,44(11):1142-1148
2.陶明信.吐-哈盆地大地构造环境分析-兼论大陆板内盆地与造山带的成因关系[J].沉积学报,1994,12(4):40-50
3.李文厚,周立发,柳益群,等.吐哈盆地沉积格局与沉积环境的演变[J].新疆石油地质,1997,18(2):135-141
4.邢秀娟,周鼎武,柳益群,等.吐-哈盆地及周缘早二叠世火山岩地球化学特征及大地构造环境探讨[J].新疆地质,2004,22(1):50-55
5.吕锡敏.吐哈盆地构造特征与油气赋存[J].江汉石油学院学报,2001,23(2):75-80
6.张恺.吐哈盆地板块构造条件及其对油气的控制作用[J].新疆石油地质.2000,21(4):261-266
7.卫延召,戴金星,赵长毅.吐哈盆地台北凹陷西部油源浅析[J].石油实验地质,2001,23(2):191-194
8.袁明生,李华明,王志勇.吐哈盆地油源研究新进展[J].新疆石油地质,2001,22(1):17-21
9.徐论勋,李建民,李景义,等.吐哈盆地台北凹陷侏罗系烃源岩特征[J].江汉石油学院学报,2004,26(2):13-15
10.张振英,邵龙义,等.吐哈盆地台北凹陷西部弧形构造带混源原油特征[J].石油学报,2005,26(2):15-20
11.王宗秀,李涛,周高志,等.博格达山晚石炭纪造山活动的变形地质记录[J].地学前缘,2003,10(1):63-69
12.王作勋,邬继易,吕喜朝,等.天山多旋回构造演化及成矿[M].北京:科学出版社,1990:1-217
13.HendrixM S,Graham S A,Carroll A R,et al.Sedimentary record and climatic imp lications of recurrent deformation in the Tian Shan:Evidence from Mesozoic strata of the north Tarim,south Junggar,and Turpan basins,northwest China[J].Geological Society of America Bulletin,1992,104:53-79
14.喻春辉,蒋宜勤,刘树辉,等.准噶尔盆地与吐哈盆地侏罗纪沉积边界的讨论[J].岩相古地理,1996,16:48-54
15.张传恒,刘典波,张传林,等.新疆博格达山初始隆升时间的地层学标定[J].地学前缘,2005,12(1):294-302
16.沈传波,梅廉夫,刘麟,等.新疆博格达山裂变径迹年龄特征及其构造意义[J].石油天然气学报(江汉石油学院学报),2005,27(2):273-277
17.朱文斌,舒良树,万景林,等.新疆博格达山-哈尔里克山白垩纪以来剥露历史的裂变径迹证据[J].地质学报,2006,80(1):16-22
18.汪新伟,汪新文,马永生.新疆博格达山的构造演化及其与油气的关系[J].现代地质,2007,21(1):116-124
19.赵重远.论含油气盆地的整体动态综合分析,见:含油气盆地地质学研究进展,赵重远等主编,西北大学出版社,1993,3-18
20.肖序常,汤耀庆,冯益民,等.新疆北部及其邻区大地构造[M].北京:地质出版社,1992:1-169
21.胡霭琴,等著.新疆北部地质演化及成岩成矿规律[M].北京:科学出版社,1997:1-120
22.周鼎武,柳益群,邢秀娟,等.新疆吐-哈、三塘湖盆地二叠纪玄武岩形成古构造环境恢复及区域构造背景示踪[J].中国科学,2006,36(2):143-153
23.周济元,茅燕石,黄志勋,等.东天山古大陆边缘火山地质[M].成都:成都科技大学出版社,1994:1-280
24.赵文智.吐鲁番-哈密盆地的构造特征[J].石油学报,1992,13(3):9-18
25.周立发.准噶尔盆地南缘山前带构造演化与油气成藏.2007,内部报告
26.李锦轶,何国琦,徐新,等.新疆北部及邻区地壳构造格架及其形成过程的初步探讨[J].地质学报,2006,80(1):148-168
27.王宗秀.博格达山链的造山活动与山体形成演化.博士论文,2003
28.朱文斌,马瑞士,等.新疆觉罗塔格山与吐哈盆地的构造接触关系[J].大地构造与成矿学,2001,25(2):128-135
29.冯先岳.论新疆地震地质特征[J].地震地质,1985,7(2):35-43
30.冯先岳.天山活动断裂与地震[J].新疆地质,1986,4(3)
31.柳益群,周鼎武,冯乔,等.吐鲁番拗陷北部及柴窝堡凹陷油气勘探前景综合评价.西北大学地质系,中石化西部新区勘探指挥部.2005,内部报告
32.马瑞士,王赐银,叶尚夫.东天山构造格架及地壳演化[M].南京:南京大学出版社,1993:1-100
33.何国琦,李茂松,刘德权.中国新疆古生代地壳演化与成矿[M].乌鲁木齐:新疆人民出版社.1994:1-437
34.成守德,徐新.新疆及邻区大地构造编图研究[J].新疆地质,2001,19(1):33-37
35.冯益民,朱宝清,杨军录,张开春.东天山大地构造及演化[J].新疆地质,2002,20(4):309-314
36.陈富文,何国琦,李华芹,等.论东天山觉罗塔格造山带的大地构造属性[J].中国地质,2003,30(4):361-366
37.李锦轶.新疆东部新元古代晚期和古生代构造格局及其演变[J].地质论评,2004,50(3):304-322
38.孙桂华,李锦轶,高立明,等.新疆东部哈尔里克山闪长岩锆石SHRIMP U-Pb定年及其地质意义[J].地质论评,2005,51(4):463-469
39.吴绍祖.新疆早二叠世古气侯[J].新疆地质,1996,14(3):270-277
40.周鼎武,柳益群,等.新疆吐-哈、三塘湖盆地二叠纪玄武岩形成古构造环境恢复及区域构造背景示踪[J].中国科学,2006,36(2):143-153
41.苗建宇.新疆北部主要盆地二叠系烃源岩沉积环境与生烃特征.博士论文,2001
42.周立发,李文厚,等.博格达南缘构造形成与沉积环境.西北大学地质系吐哈盆地研究 队,1994,内部报告
43.周立发,等.柴窝堡盆地前侏罗系油气勘探前景综合分析.西北大学地质系,1998,内部报告
44.姬金生,陶洪祥,曾章仁,等.东天山康古尔塔格金矿带地质与成矿[M].北京:地质出版社,1994
45.Cullers R L et al;Rare earth distributions in clay minerals and clay-sized fractinal of the lower Permian Havensville and Eskridge shales of Kansas and Oklahoma[M];Geochim.et Cosmochim.Acta;1975
46.Roaldset E.Rare earth elements in quaternary clays of numedel area,Southern Norway[J].Lithos,1973,6:349-372
47.Ronov A B,Yaroshevsky A A.Chemical structure of the Earth's crust[J].Genkhimia,1967(11):1 285-1 309(in Russian with English abstract)
48.Gleadow,A.J.W.,Duddy,I.R..A natural long-term annealing experiment for apatite.Nuclear Tracks and Radiation Measurements,1981,5(1-2):169-174
49.Muecke T W.Formation fines and factors controlling their movement in porous media[J].JPT,1979(2):144-50.
50.Bhatia M R.Rare earth element geochemistry of Australian Paleozoic graywackes and mudrocks:Provenance and tectonic control[J].Sediment.Geol.,1985,45:97-113
51.Bhatia M R.Plate tectonics and geochemical composi-tion of sandstones[J].The Journal of Geology,1983,91:611-627
52.Taylor S R,Mclennan S M.The continental crust:its composition and evolution;an examination of the geo-chemical record preserved in sedimentary rocks[M].Oxford:Blackwell Scientific Publications,1985:1-312
53.Bhatia M R,Crook K A W.Trace element characteristics of graywackes and tectonic setting discrimination of sedimentary basins[J].Contrib Mineral Petro,1986,(92):181-193
54.Hatch J R,Leventhal J S.Relationship between inferred redox potential of the depositional environment and geochemistry of the Upper Pennsylvanian(Missourian)Stark Shale[J].Member of the Dennis Limestone,Wabaunsee County,Kansas,U.S.A.Chemical Geology,1992,99:65-82
55.彼得斯KE,莫尔多万J.M,等.生物标记化合物指南-古代沉积物和石油中分子化石的解释[M].北京:石油工业出版社,1995
56.周鼎武,董云鹏,等.“磨拉石建造”和“不整合”在地层对比中的意义.地质论评,1996,43(5):416-423
57.苗建宇,周立发,等.新疆北部中二叠统烃源岩地球化学特征与沉积环境[J].地质学报,2004,534-541
58.方世虎,贾承造,等.准噶尔盆地二叠纪盆地属性的再认识及其构造意义[J].地学前缘,2006,13(3):108-121
59.汪新伟,汪新文,马永生.新疆博格达山的构造演化及其与油气的关系[J].现代地质, 2007,21(1):116-124
60.王丹.新疆博格达山南缘上二叠统精细层序地层学研究,硕士论文,2006
61.Tissot B P.Califet-Debyser Y.Derco G,Oudin J L.Origin and evolution of hydrocarbons in early Toarcian Shales.Paris Basin.AAPG Bulletin,1971,55:2177-2193
62.Tissot B P.Durand B.Espitalie J.Combaz.A Influences of the nature and diagenesis of organic matter in the formation of petroleum.AAPG Bulletin,1974,58:499-506
63.Tissot B P,Welte D H.Petroleum formation and oceurence.New York:Springer-Verlag.1978
64.张厚福,张万选.石油地质学.第二版[M].北京:石油工业出版社,1989.152-161
65.程克明,王铁冠,等.烃源岩地球化学[M].科学出版社,1995
66.张厚福.石油地质学[M].北京:石油工业出版社,1989.39-100
67.武守诚.石油资源地质评价导论[M].北京:石油工业出版社,1994.98-125
68.王铁冠,钟宁宁,熊波,等.源岩生烃潜力的有机岩石学评价方法[J].石油学报,1994,15(4):9-16
69.王铁冠,钟宁宁,侯读杰,等.低熟油形成机理与分布[M].北京:石油工业出版社,1995
70.李贤庆,马安来,等.烃源岩有机岩石学研究方法与应用[M].重庆大学出版社,1997
71.王启军,陈建渝.油气地球化学[M].武汉:中国地质大学出版社,1988
72.B.P.蒂索、D.H.威尔特著,郝石生等译,石油形成和分布[M].北京:石油工业出版社,1982
73.李艳红,金奎励.烃源岩成熟度评价指标及选取[J].地质地球化学,2000,28(2):94-96
74.许怀先.石油地质实验测试技术与应用[M].石油工业出版社,2001
75.覃克,赵密福.惠民凹陷临南斜坡带油气成藏模式[J].石油大学学报(自然科学版),2002,26(6):21-24
76.Gleadow A J W,Dubby I R,Lovering J F.Fission track analysis:a new tool for the evaluation of thermal histories and hydrocarbon potential.Aust Petrol Explor Assoc J,1983,23:93-102
77.Naeser C W.Thermal history of sedimentary basins:fission-track dating of subsurface rocks.In:Scholle P A,Schluger R P,eds.Aspect of diagenesis.SEPM special Publication.1979,26:109-112
78.Wagner G A,Van den Haute P.Fission-track-dating.Dordrecht:Enke Verlag-Kluwer Academic Publishers,1992,180-285
79.Green P F,Duddy I R,Laslett G M,et al.Thermal annealing of fission tracks in apatite 4.Qualitative modeling techniques and extensions to geological timescales.Chem Geol,1989,79:155-182
80.Hurford A J,Green P F.A users,guide to fission-track dating calibration.Earth Planet Sci Lett,1982,59:343-354
81.王瑜.构造热年代学-发展与思考.地学前缘,2004,11(40):435-443
82.吴中海,吴珍汉.裂变径迹法在研究造山带隆升过程中的应用介绍.地质科技情报,1999,18(4):27-32
83.康铁笙,王世成.地质热历史研究的裂变径迹法[M].北京:科学出版社,1991.25-40
84.周中毅,潘长春.沉积盆地古地温测定方法及其应用[M].广州:广东科技出版社,1992.1-103
85.胡圣标,张容燕,周礼成.油气盆地热历史恢复方法[J].勘探家,1998,3(4):52-54
86.McKenzie D P.Some remarks on the development of sedimentary basins.Earth Planet Sci Lett,1978,40:25-32
87.Jarvis G T,McKenzie D P.Sedimentary basin formation with finite extension rates.Earth Planet Sci Lett,1980,48:42-52
88.Royden L,Keen C E.Rifting processes and thermal evolution of the continenta lmargin of eastern Canada determined from subsidence curves.Earth Planet Sci Lett,1980,51:343-361
89.Keen C E,Dehler S A.Stretching and subsidence:rifting of conjugate margins in the North Atlantic region.Tectonics,1993,12:1219-1229
90.韩宝福,何国琦,等.后碰撞幔源岩浆活动、底垫作用及准噶尔盆地基底的性质[J].中国科学,1999,29(1):16-21
91.李锦轶,肖序常,等.新疆北部晚石炭世至晚三叠世地壳热演化-东准噶尔考克塞尔盖山荒草坡群的~(40)Ar-~(39)Ar定年[J].地质学报,2000,74(4):303-311
92.赵明,舒良树,等.东疆哈尔里克变质地带变质作用特征及形成构造环境研究[J].高校地质学报,1997,3(1):40-50
93.赵明,舒良树,朱文斌,等.东疆哈尔里克变质带的U-Pb年龄及其地质意义[J].地质学报,2002,76(3):379-383
94.孙桂华.新疆东部哈尔里克山构造变形研究.地质科学院硕士学位论文,2004
95.顾连兴,于春水,等.博格达上大河沿岩体铷-锶同位素年龄及其地质意义[J].矿物岩石地球化学通报,2001,19(1):19-21
96.蔡忠贤,陈发景,等.准噶尔盆地的类型和构造演化[J].地学前缘,2007(4):431-440
97.李向东,王庆明.天山后碰撞阶段构造演化的新信息-来自阿吾拉勒山中段动力变质岩的证据[J].地质论评,1998,44(4):443-448
98.陈富文,李华芹,等.新疆东部金窝子金矿成因讨论-同位素地质年代学证据[J].地质论评,1999,45(3):246-253
99.李华芹,陈富文,等.新疆东部印支期成岩成矿年代学新证据[J].地质学报,2005
100.陈富文,李华芹,等.中国阿尔泰造山带燕山期成岩成矿同位素年代学新证据[J].科学通报,1999,44(11):1142-1148
© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号 地址：北京市海淀区学院路29号 邮编：100083 电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700 |