THE GEOLOGICAL STRUCTURE OF THE XIEFENG MOUNTAINS-YUANMA BASIN AND ITS SIGNIFICANCE TO OIL EXPLORATION
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摘要: 山系、盆地、油气三者之间关系的研究,是油气盆地分析系统工程中的一个重要组成部分。沅麻盆地与雪峰山系,自中、新生代以来,受“板内形变”动力条件控制组成“盆山体系”.造山挤压作用控制了盆地的构造(沉积)格局与油气组合,使盆地发生“构造反转”,破坏或重新调整油气富集条件。作者相信,研究这一区域山系-盆地-油气三者构成的系统,对于南方陆相盆地群的油气评价与找油找气有重要意义。Abstract: To study the relationship among mountain system, basin and hydrocarbon is an important (element) in hydrocarbon-bearing basin analysis.The Xiefeng mountain system and the Yuanma basin have been controlled by "intraplate deformation" dynamic condition since the Meso-Cenozoic, and the‘basinmounfain sysfem' wes formed. The orogenic compressional activity controlled basional structural (sedimentary) pattern and petroleum system resulted in ‘structural reversion' of the basin and damage or re-organization of hydrocarbon accumulation. It is very important to study the ‘mountain system-basin-hydrcoarbon' system of the area to evaluate and explore for oil and gas in the continental basins of the South China.
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[1] 孙肇才等.板内形变与晚期次生成藏—扬子区海相油气总体形成规律的探讨.石油实验地质,1991,13(2) [2] 许靖华.弧后碰撞造山作用及其大地构造相.南京大学学报(地球科学),1994,6(1) [3] 黄汲清.中国主要地质构造单位.北京:地质出版社.1954 [4] 范小林等.江南古陆西南区段深部地质(构造)探讨.华东地质学院学报.1993.16(1) [5] 刘树辉.贵州东部志留系岩相展布及麻江古背斜油藏序列的油源.贵州石油地质,1983,8(2) [6] 马文璞等.雪峰隆起的构造性质及其对上扬子东南缘古生代盆地的改造.江南-雪峰地区的层滑作用及多期复合构造,北京:地质出版社,1993 [7] 谢湘雄等.试论湖南省莫霍面形态及地壳厚度特征.湖南地质,1990,9(2) [8] 秦葆瑚.台湾-黑水地学大断面所揭示的湖南深部构造.湖南地质,1991,10(2) [9] 蒋洪堪等.四川大足-福建泉州深部地电特征.地球物理学报,1992,35(2) [10] 范小林等.雪峰古陆地区深部地质构造探讨.西安地质学院学报,1994,16(1) [11] 关士聪.关士聪地质文选.北京:地质出版社,1988 [12] 陈海乱等.雪峰山大地构造的基本特征初探.地质科学,1993,28(3) [13] 孙肇才等主编.中国南方古、中生界海相油气勘查研究.北京:科学出版社,1993 [14] 陈彦华等.扬子区早古生代沉积演化及其对油气的控制.中国南方古、中生界海相油气勘查研究,北京:科学出版社,1993 [15] Ziegler P A. Inverted basins in the Alpine foreland, in Bally A. W. ed. Seismic Expression of strultural styles. AAPG,1983,3(15) [16] Prodor A. Petroleum systems: Models and applications. Journal of Petroleum Geoloay,1993,15(3) -
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