“盆”“山”耦合和脱耦的反转点和切入点研究

吴根耀; 马力

doi:10.11781/sysydz200501008

“盆”“山”耦合和脱耦的反转点和切入点研究

doi: 10.11781/sysydz200501008

吴根耀¹,
马力²

1.
中国科学院, 地质与地球物理研究所, 北京, 100029
2. 中国石油化工集团公司, 江苏油田, 江苏, 扬州, 225009

详细信息

作者简介:
吴根耀(1946- ),男(汉族),上海市人,研究员,主要从事大地构造学研究.

中图分类号: TE121.2
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- 被引次数: 0
出版历程
- 收稿日期: 2004-11-05
- 刊出日期: 2005-01-25

AN APPROACH TO THE STUDY OF INVERSION POINTS AND TANGENCY-IN POINTS FOR OROGENY AND COUPLED/DECOUPLED BASIN DEVELOPMENT

Wu Genyao¹,
Ma Li²

1.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
2. Jiangsu Oilfield, SINOPEC, Yangzhou, Jiangsu 225009, China

摘要

摘要: 反转构造的反转点和“盆”“山”关系的切入点是“盆”“山”耦合和脱耦研究的方法论中的关键问题。抓准抓好反转点,一是要深刻认识中国大地构造特征所决定的“盆”“山”关系的复杂性,二是要全面了解区域内“盆”“山”耦合和脱耦的关键问题。“盆”“山”关系的切入点,既应视具体的研究对象多方位、多角度、多层次、多侧面地确定,也要强调首要的和必要的切入点是造山作用的类型。抓对反转点的必由途径是“盆”“山”研究中把“正序”与“反序”结合起来而以“反序”的研究为主,文章简要介绍了反序地编制“盆”“山”演化图的经验。反转点和切入点的确定体现在盆地研究中,是在给予时间约束和厘定盆地含义的前提下正确认识盆地的世代更迭和各世代的构造格架及构造样式,特别是正确认识重大构造运动时期的盆地世代更迭。“盆”“山”耦合和脱耦的反转点和切入点研究的突破,必将造成盆地研究生动活泼的新局面,进而给残留海相盆地的油气勘探带来新的启示。
- 反转点 /
- 切入点 /
- 反序研究 /
- 盆地世代更迭 /
- “盆”“山”耦合和脱耦
Abstract: The study of orogeny and coupled/decoupled basin development regarded orogeny and basin development as a whole and explored a uniform kinematic process and geodynamic mechanics between the both. The key of methodology for the study was to grasp, correctly and practically, inversion points and tangency-in points, the former representing obvious changes of tectonic patterns or styles, and the latter constituting a key link connecting basins with orogeny. For the inversion points, we should, first of all, understand the essential problems of orogeny and coupled/decoupled basin development in a given regional framework. In addition, the tectonic features of Chinese continent decided the difficulties and complexities of discerning inversion points, which supported, in turn, a wide platform for the study of tengency-in points. The tangency-in points might be decided by a poly-direction, poly-visual angle, poly-level and poly-aspect means, in which the orogenic types and structural styles should be the first important and necessary one. As the road one must take for the study of inversion points and tangency-in points, a combination of "normal succession" and "reversal succession" was emphasized, with stress on the study of "reversal succession". Namely, regional evolution and basin development should be worked from the ancient to the present, and the oil-gas accumulation analysed from the young structural layers to the older ones. The paper introduced some experiences to compile some profiles, perpendicular to the regional tectonic strike, across both an orogen and neighbouring basins. With the inversion points and tangency-in points being embodied in the basin research, the alternation of basin generations as well as tectonic patterns and structural styles in each generation should be correctly distinguished, particularly, to distinguish the basin generations changed in the periods of main tectono-thermal events. The prerequisite for understanding basin generations was to constrain a geohistorical phase and to stipulate a basin definition. The advances in the study of inversion points and tangency-in points for orogeny and coupled/decoupled basin development must open up a new prospect of the basin research, and then draw a new inspiration in the oil-gas exploration of relict marine basins.
- inversion point /
- tangency-in point /
- study of “reversal succession” /
- alternation of basin generations /
- orogeny and coupled/decoupled basin development

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参考文献(60)

[1]	吴根耀,马力."盆""山"耦合和脱耦:含油气盆地研究的新思路[A]. 见:中国石油学会石油地质专业委员会编. 油气盆地研究新进展第一辑[C]. 北京:石油工业出版社, 2002. 20～36
[2]	汤良杰,金之钧,贾承造等. 叠合盆地构造解析几点思考[J]. 石油实验地质,2001,23(3):251～255
[3]	吴根耀,马力,陈焕疆等. 苏皖地块演化,苏鲁造山带形成及其耦合的盆地发育[J]. 大地构造与成矿学,2003, 27(4):336～352
[4]	何建坤,卢华复,张庆龙等. 南大巴山冲断构造及其剪切挤压动力学机制[J]. 高校地质学报,1997, 3(4):419～428
[5]	马力,陈焕疆,甘克文等. 中国南方大地构造和海相油气地质[J]. 北京: 地质出版社, 2004. 865
[6]	吴根耀,王晓鹏,钟大赉等. 川滇藏交界区二叠纪-早三叠世的两套弧火山岩[J]. 地质科学,2000, 35(3):350～362
[7]	孙晓猛,吴根耀,郝福江等. 秦岭-大别造山带北部中-新生代逆冲推覆构造期次及时空迁移规律[J]. 地质科学,2004, 39(1):63～76
[8]	赵宗举,朱琰,徐春华等. 合肥盆地与大别-张八岭造山带的耦合关系[J]. 石油实验地质,2003,25(6):670～678
[9]	吴根耀,马力. 试论"盆""山"的耦合和脱耦及其运动学[J]. 石油实验地质, 2003, 25(2):99～109
[10]	吴根耀. 古缝合线活化和华南中生代陆内造山运动[A]. 见:中国地质学会编. 第31届国际地质大会中国代表团学术论文集[C]. 北京:地质出版社,2001. 32～39
[11]	吴根耀. 古深断裂活化与燕山期陆内造山运动——以川南-滇东和中扬子褶皱-冲断系为例[J]. 大地构造与成矿学,2001, 25(3):246～253
[12]	吴根耀. 燕山运动和中国大陆晚中生代的活化[J]. 地质科学,2002, 37(4):453～461
[13]	吴根耀. 造山带地层学[M]. 成都:四川科学技术出版社,乌鲁木齐:新疆科技卫生出版社,2000. 218
[14]	汤加富,许卫. 郯庐断裂带南段并无巨大平移——来自安徽境内的证据[J]. 地质论评, 2002,48(5):449～462
[15]	乔秀夫,张安棣. 华北块体、胶辽朝块体与郯庐断裂[J].中国地质,2002,29(4):337～345
[16]	杨文采,胡振运,程振炎等. 郯城-涟水综合地球物理剖面[J]. 地球物理学报,1999, 42(2):206～217
[17]	吴根耀,陈焕疆,马力等. 中国东部燕山期高原的发育及对矿产和油气资源评价的启示[J]. 石油实验地质,2002,24(1):3～12
[18]	薛良清. 层序地层学在湖相盆地中的应用探讨[J]. 石油勘探与开发,1990, 17(6):29～34
[19]	徐怀大. 层序地层学理论用于我国断陷盆地分析中的问题[J]. 石油与天然气地质,1991,12(1):52～57
[20]	李思田,杨士恭. 论沉积盆地的等时地层格架和基本建造单元[J]. 沉积学报,1992,10(4):11～22
[21]	吴根耀. 构造层序地层学[J]. 地球科学进展,1996, 11(3):310～313
[22]	顾家裕. 陆相盆地层序地层学格架概念及模式[J]. 石油勘探与开发,1995, 22(4):6～10
[23]	操应长,姜在兴,夏斌等. 陆相断陷湖盆T-R层序的特点及其控制因素[J]. 地质科学,2004,39(1):111～122
[24]	曾允孚, 纪相田.天全芦山地区晚白垩世-早第三纪陆相盆地层序地层分析. 矿物岩石,1992,12(4):56～73
[25]	赵玉光,丘东洲. 西准噶尔界山前陆盆地晚期(T-J)层序地层与油气勘探[J]. 新疆石油地质,1993, 14(4):323～331
[26]	赵玉光,许效松. 克拉通边缘前陆盆地动力层序地层学[J]. 岩相古地理,1997, 17(1):1～10
[27]	Cross T A. Controls on coal distribution in transgressive-regressive cycle, Upper Cretaceous, Western Interior, U S A[J]. SEPM Special Publication 42, 1988. 371～380
[28]	Van Wagoner J C, Mitchum R M, Campion K M, et al. Siliciclastic sequence stratigraphy in well logs, cores and outcrops: concepts for high-resolution correlation of time and facies[J]. AAPG Methods in Exploration Series 7, 1990. 55
[29]	Brown F L. Benson Jr J M, Brink G L, et al. Sequence stratigraphy in offshore south African divergent basin[J]. AAPG Studies in Geology 41, 1995. 184
[30]	王洪亮,邓宏文. 地层基准面原理在湖相储层预测中的应用[J]. 石油与天然气地质,1997,18(2):96～102
[31]	郑荣才,彭军. 陕北志丹三角洲长6油层组高分辨率层序分析与等时对比[J]. 沉积学报,2002,21(1):90～100
[32]	邓宏文,王洪亮,宁宁. 层序地层基准面的识别、对比技术及应用[J]. 石油与天然气地质,1996,17(3):177～184
[33]	赵俊青,纪友亮,张世奇等. 陆相高分辨率层序界面识别的地球化学方法[J]. 沉积学报,2004,22(1):79～86
[34]	Sengor A M C, Natal'in B S. Paleotectonics of Asia: fragments of a synthesis[A]. In: Yin A, Harrison T M. eds. The Tectonic Evolution of Asia[M]. Cambridge: Cambridge Univ Press, 1996. 486～640
[35]	吴根耀,马力,钟大赉等. 滇桂交界区印支期增生弧型造山带:兼论与造山作用耦合的盆地演化[J]. 石油实验地质,2001, 23(1):8～18
[36]	刘和甫,夏义平,殷进垠等. 走滑造山带与盆地耦合机制[J]. 地学前缘,1999, 6(3):121～132
[37]	吴根耀,马力,许效松等. 喜马拉雅运动:对川滇交界区古地理重建的制约和楚雄盆地的改造[J]. 古地理学报,2001, 3(2):3～10
[38]	Dahlstrom C D A. Balanced cross section[J]. Can Jour Earth Sci, 1969, 6:743～757
[39]	漆家福,杨桥,王子煜. 编制盆地复原古构造图的若干问题的讨论[J]. 地质科学,2003,38(3):413～424
[40]	何光玉,卢华复,李树新. 库车盆地秋里塔格构造带构造圈闭及油气勘探方向[J]. 地质科学,2003,38(4):506～513
[41]	张进,马宗晋,任文军. 对盆地耦合研究的新看法[J]. 石油实验地质,2004,26(2):169～175
[42]	McClay K R. The Mapping of Geological Structures[M]. Chichester: John Wiley & Sons,1992. 161
[43]	吴根耀. 初论造山带古地理学[J]. 地层学杂志,2003, 27(2):81～98
[44]	吴根耀,马力."盆""山"耦合和脱耦在含油气盆地分析中的应用[J]. 石油实验地质, 2003, 25(6):648～660
[45]	吴根耀. 盆地研究的活动论构造观[J]. 石油实验地质,1998, 20(4):309～318
[46]	吴根耀. 中国滇西-泰国地区侏罗纪-第四纪盆地发育及其对比研究[J]. 地质科学, 1991,26(4):359～368
[47]	Wu G Y. Collision tectonics in the central sector of the Sanjiang Indosinides bordering Xizang (Tibet), Sichuan and Yunnan, China[A]. In: Proceedings of the International Conference on Stratigraphy and Tectonic Evolution of Southeast Asia and the Pacific[C]. Bangkok: 347～359
[48]	Yano T, Wu G Y, Tan M Q, et al. Tectono-sedimentary development of backarc continental basin in Yunnan, southern China[J]. Journal of SE Asian Earth Sciences, 1994, 9(1-2):153～166
[49]	吴根耀. 滇西北地区第三纪的逆冲-推覆构造[J]. 大地构造与成矿学, 1994,18(4):331～338
[50]	Wu Genyao, Sun Xiaomeng, Zhong Dalai. Structural Geology of the Central Sector of the Hengduan Mountains[M]. Beijing: Geological Publ House,1996. 40
[51]	季建清,钟大赉,张连生. 滇西南新生代走滑断裂运动学、年代学及对青藏高原东南部块体运动的意义[J]. 地质科学,2000,35(3):336～349
[52]	杨振德. 云南临沦花岗岩的冲断叠瓦构造与推覆构造[J]. 地质科学,1996, 31(2):130～139
[53]	刘善印,钟大赉,吴根耀. 滇西南景谷-镇沅地区早第三纪陆-陆碰撞期走滑挤压盆地[J]. 地质科学, 1998,33(1):1～8
[54]	Wu Genyao, Yano T, Inomata M. Yanshanian orogenics in South China: a relation to Neotethyan evolution[J]. Scientia Geologica Sinica, 1998, 7(1):1～10
[55]	吴海威,张连生,嵇少丞. 红河-哀牢山断裂——一条喜山期大型陆内左行走滑剪切带[J]. 地质科学,1989,24(1):1～8
[56]	Chung S-L, Lo C-H, Lee T-Y, et al. Diachronous uplift of the Tibetan plateau starting 40 Myr ago[J]. Nature, 1998, 394:769～773
[57]	Liu Shanyin, Wu Genyao, Zhong Dalai. Tectono-sedimentary development of Jinggu pull-apart basin in southwestern Yunnan, China[J]. Scientia Geologica Sinica, 1996, 5(1):17～24
[58]	Liu S Y, Wu G Y, Zhong D L. Pull-apart basins as a response to post-collisional shearing tectonics: an example from Jinggu, southwestern Yunnan, China[A]. In: Proceedings of the International Conference on Stratigraphy and Tectonic Evolution of Southeast Asia and the Pacific[C]. Bangkok. 361～367
[59]	王晓鹏,吴根耀,钟大赉. 受红河断裂控制的晚第三纪走滑松弛盆地——以漠沙盆地为例[J]. 地质科学,2001,36(3):370～379
[60]	吴根耀. 中缅泰交界区的断裂及其新构造活动方式[J]. 第四纪研究, 1991, 11(1):28～37