造山带与前陆盆地结构构造及动力学研究思路和进展

doi:10.11867/j.issn.1001-8166.1997.01.0001

地球科学进展 ›› 1997, Vol. 12 ›› Issue (1): 1 -6. doi: 10.11867/j.issn.1001-8166.1997.01.0001

学科发展与研究下一篇

造山带与前陆盆地结构构造及动力学研究思路和进展

董云鹏，张国伟

西北大学地质系西安 710069

收稿日期:1996-05-09 修回日期:1996-08-06 出版日期:1997-02-01
通讯作者: 董云鹏,男,1967年11月出生,博士生,构造地质学专业。

SOME IDEAS AND ADVANCES IN STUDIES OF TECTONICS AND DYNAMICS OF OROGENIC BELT AND FORELAND BASIN

DONG Yunpeng, ZHANG Guowei

Department of Geology,Northwest University,Xi'an 710069

Received:1996-05-09 Revised:1996-08-06 Online:1997-02-01 Published:1997-02-01

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运用大量的研究成果，综合分析了大陆岩石圈结构和动力学特征，在此基础上探讨了造山带研究的思路和方法，总结了造山带结构、构造及其形成演化研究的新进展。指出前陆盆地的研究是深入研究造山带的关键，前陆盆地是前陆冲断作用引起岩石圈挠曲变形的结果，阐述了前陆盆地形成机制的研究进展。

关键词: 造山带, 前陆盆地, 挠曲变形, 逆冲构造, Membrane fouling, Sludge bulking property, Membrane Bio-reactor

The combination studies of orogenic belt and foreland basin is becoming a main trend of the continent research. The orogenic belt and foreland basin were formed in a same geodynamic system. Their formational and evolutionary processes are affected by the rheological structure of continental lithosphere. Based on a large number of study results and the synthetical studies of the structure and dynamics of continental lithosphere, some ideas and methods of the orogenic belt and foreland basin research are discussed, and the advances in the studies of structure and evolution of orogenic belt and foreland basin are reviewed. The authors point out that a foreland basin, which was formed by the flexural deformation due to foreland thrust loading, is a key to solving the major problems of orogenic belt.

Key words: Orogenic belt, Foreland basin, Flexural deformation, Thrust

中图分类号:

P542

1 肖庆辉,李晓波,贾跃明,等.当代造山带研究中值得重视的若干前沿问题.地学前缘,1995,2(1):43-50.
2 肖庆辉,贾跃明,刘树臣,等.地质科学的机会与挑战.北京:中国地质矿产信息研究院,1991.
3 宋鸿林,单文琅,傅昭仁.论壳内韧性流层及其构造表现.现代地质,1992,6(4):494-503.
4 张国伟,周鼎武,于在平.大陆造山带成因研究.见:肖庆辉等著.当代地质科学前沿.武汉:中国地质大学出版社,1993.145-154.
5 张国伟,孟庆任,赖绍聪.秦岭造山带的结构构造.中国科学,1995,25(19):994-1003.
6 吴福元,葛文春,孙德有.走滑构造及对中国东部中生代地质研究的意义.世界地质,1994, 13(1): 105-113.
7 Woodwock N H. The role of strike-slip fault systems at plate boundaries. Royal Society of London Philosophical Transactions. Ser A, 1986,317:13-29.
8 单文琅,宋鸿林,傅昭仁.构造变形分析的理论、方法和实践.武汉:中国地质大学出版社, 1991.
9 牛树银,孙爱群,白文吉.造山带与相邻盆地间物质的横向迁移.地学前缘,1995,2(1):85-92.
10 Watts A B, Ryan W B F.Flexure of the lithosphere and continental margin basins. Tectonophysics, 1976,36:25-44.
11 Jordan T E.Thrust loads and foreland basin evolution,Cretaceous,western United States. AAPG Bull, 1981,65(12):2506-2520.
12 Karner G D, Watts A B.Gravity anomalies and flexure of the lithosphere at mountain ranges.J Geophys Res, 1983,88:10449-10477
13 Winter H de la R. A tectonic classification of certain South African depositional basins and criteria for recognition of major unconformity-bounded sequences. South African J Geology, 1989,92(2):167-182
14 Wiltschko D V, Dorr J A.Timing of deformation in overthrust belt and foreland of Idaho, Wyoming and Utah.AAPG Bull, 1983,67:1304-1322.
15 Schedl A, Wiltschko D V.Sedimentological effects of a moving terrain. J Geology,1984,92:273-287.
16 Flemings P B, Jordan T E. Stratigraphic modeling of foreland basins:Interpreting thrust deformation and lithosphere rheology.Geology,1990,18:430-434.
17 Beaumont C, Quinlan G M, Hamilton J. Orogeny and stratigraphy:numerical models of the Paleozoic in the eastern interior of North America. Tectonics,1988,7:389-416.
18 Quinlan G M, Beaumont C.Appalachian thrusting,lithospheric flexure,and the Paleozoic stratigraphy of the eastern interior of North America.Can J Earth Sci, 1984,21:973-996.
19 Tankard A J. On the depositional response to thrusting and lithospheric flexure:examplesfrom the Appalachian and Rocky Mountain basins.Foreland Basin, Spec Publ Int Ass Sediment, 1986.
20 刘少峰,李思田,庄新国,等.鄂尔多斯西南缘前陆盆地沉降和沉积过程模拟.地质学报,1996,70(1):12-22.

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