前陆盆地构造作用的沉积响应

摘要/Abstract

摘要： 前陆盆地与造山带具有良好的耦合性，可以用盆山耦合的思想来研究前陆盆地与构造事件的响应关系。逆冲构造运动对盆地的可容纳空间产生了深刻的影响，从而对盆地充填和层序叠置样式起重要的控制作用。整个前陆盆地区域具有两个阶段的盆地发展过程，第一个沉积阶段与冲断带附近的载荷侵位引起的构造沉降密切相关，第二个阶段发生于冲断带的侵蚀期，导致了盆地的再次沉积。前陆盆地不同的沉积层序是不同的构造事件的沉积响应。

关键词: 前陆盆地, 逆冲构造, 耦合, 沉积响应

Abstract: There are excellent coupling between foreland basin and orogenic belt. Study shows that thrust tectonic events could produce profound influences to basinal accommodation, hence control the basinal fillings and the stratigraphic superposed forms. There are two stages during the development of foreland basin. The first stage is closely interrelated with the subsidence caused by loading emplacement, and the second stage appears the erosion phase of the trust belt which may cause the continued sedimentation. The different depositional sequences reflect the different tectonic events which are the sedimentary responses of different tectonic movements.

Key words: foreland basin, thrust structure, coupling, sedimentary response

中图分类号:

TE111.3

刘亢, 曲国胜, 许华明. 前陆盆地构造作用的沉积响应[J]. 新疆石油地质, 2008, 29(6): 778-781.

LIU Kang, QU Guo-sheng, XU Hua-ming. The Sedimentary Response to the Tectonism in Foreland Basin[J]. Xinjiang Petroleum Geology, 2008, 29(6): 778-781.

参考文献

[1] Price R A. Large-scale gravitational flow of supracrustal rocks, southern Canadian Rockies[A]. Dejong K A, Scholten R. Gravity and tectonics[C]. New York：Wiley Interscience, 1973：491-502.
[2] Dickinson W R. Plate tectonic and sedimentation[A]. Dickinson W R. Tectonics and sedimentation[C].Spec. Publ. Paleont. Miner, Tulsa, 1974：1-27.
[3] 刘和甫. 前陆盆地类型及褶皱——冲断层样式分析[J]. 地学前缘，1995，2 (3)：59-68.
[4] 汤济广，梅廉夫，沈传波，等. 前陆盆地结构单元与油气成藏响应[J]. 新疆石油地质，2006，27(2)：242-245.
[5] 罗志立，刘树根，雍自树，等. 中国陆内俯冲(C-俯冲)论的形成和发展[J].新疆石油地质，2003，24(1)：1-7.
[6] Lu Huafu, Howell D G, Dong J, et al. Rejuvenation of the Kuqa foreland basin[J]. International Geology Review, 1994， 36：1 151-1 158.
[7] Decelles P G, Giles K A. Foreland basin systems[J]. Basin Research, 1996, 8：105-123.
[8] 王清晨，李忠. 盆山耦合与沉积盆地成因[J]. 沉积学报，2003，21(1)：24-30.
[9] 吴根耀，马力.“盆”、“山”耦合和脱耦：含油气盆地研究的新思路[J]. 大地构造与成矿学，2004，28(2)：81-97.
[10] 刘和甫，李晓清，刘立群，等. 盆山耦合与前陆盆地成藏区带分析[J]. 现代地质，2004，18(4)：389-403.
[11] Catuneanu, Hancox, Rubidge. Reciprocal flexural behaviour and contrasting stratigraphies: a new basin development model for the Karoo retroarc foreland system, South Africa [J]. Basin Research, 1998,10: 417-439.
[12] Sinclair H D. Flysch to molasses transition in peripheral foreland basins: the role of the passive margin versus slab breakoff[J]. Geology, 1997. 25(12)：1 123-1 126.
[13] Covey M. The evolution of foreland basins to steady state:evidence from the western Taiwan foreland basin[A]. Allen G P. Foreland basins[C]. Special Publication of the International Assocation of Sedimentologists, 1986：77-90.
[14] Stockmal G S, Beaumont C, Boutilier R. Geodynamic models of convergent tectonics: the transition from rifted margin to overthrust belt and consequences for foreland basin development [J]. AAPG Bulletin, 1986, 70：181-190.
[15] Desegaulx P, Kooi H, Cloetingh S. Consequences of foreland basin development on thinned continental lithosphere: application to the aquitane basin(SW France)[J]. Earth Planetary Science Letters, 1991,106：116-132.
[16] Quintijn Clevis. Three-dimensional modeling of thrust-controlled foreland basin stratigraphy[J]. Universiteit Utrecht， 2003：11-16.
[17] 张传恒，孙玉建，汪剑，等. 标定碰撞构造的地层学线索——欠补偿周缘前陆盆地结构与充填序列[J]. 地质科技情报，2003，22(1)：36-40.
[18] Jordan T E. Thrust loads and foreland basin evolution, Cretaceous, western United States[J]. AAPG Bulletin, 1981, 65：2 506-2 520.
[19] Karner G D, Watts A B. Gravity anomalies and flexure of the lithosphere at mountain ranges[J]. Journal of Geophysical Research, 1983，88：10 449-10 477.
[20] Heller P L, Angevine C L , Winslow N S, et al. Two-phase stratigraphic model of foreland-basin sequences[J]. Geology, 1988，16：501-504.
[21] Jordan T E, Flemings P B. Large-scale statigraphic architecure, eustatic variation, and unsteady tectonism: a theoretical evaluation[J]. Journal of Geophysical Research, 1991, 96：6 681-6 699.