|
|||||
|
|
| 盆山耦合与前陆盆地成藏区带分析 | |
| 引用本文： | 刘和甫,李晓清,刘立群,李小军.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. |
| 作者姓名： | 刘和甫 李晓清 刘立群 李小军 |
| 作者单位： | 1. 中国地质大学,能源学院,北京,100083 2. 中国地质大学,能源学院,北京,100083;胜利油田,东胜精攻石油开发集团有限公司,山东,东营,257100 3. 中国石油化工股份有限公司,勘探开发研究院,北京,100083 4. 中国地质大学,能源学院,北京,100083;中国石油勘探研究院,廊坊分院,065007 |
| 基金项目： | 国土资源大调查项目(DKD21040110)。 |
| 摘 要： | 经济全球化导致油气勘探全球化,板块学说在理论上提供全球油气勘探基础,亚洲大陆与北美大陆盆山体系在实践上提供全球油气勘探经验。盆山耦合体系存在3类造山带与3类前陆盆地即:(1)俯冲造山带与弧后前陆盆地;(2)碰撞造山带与周缘前陆盆地;(3)陆内造山带与陆内前陆盆地。前陆盆地成藏区带勘探中,在空间上应将造山带前麓褶皱—冲断带层与前陆盆地作为统一应变场,在时间上应将前冲断作用沉积层序,同冲断作用沉积层序和后冲断作用沉积层序作为整体来进行勘探。 |
| 关 键 词： | 俯冲造山带 弧后前陆盆地 碰撞造山带 周缘前陆盆地 陆内造山带 陆内前陆 |
| 文章编号： | 1000-8527(2004)04-0389-15 |
| 修稿时间： | 2004年10月10 |
BASIN-MOUNTAIN COUPLING AND FORELAND BASIN PETROLEUM PLAY ANALYSIS |
|
| LIU He-fu,LI Xiao-qing.BASIN-MOUNTAIN COUPLING AND FORELAND BASIN PETROLEUM PLAY ANALYSIS[J].Geoscience——Journal of Graduate School,China University of Geosciences,2004,18(4):389-403. | |
| Authors: | LIU He-fu LI Xiao-qing |
| Institution: | LIU He-fu~1,LI Xiao-qing~ |
| Abstract: | Economic globalization leads naturally to the globalization of oil and gas exploration and development. On one hand, plate tectonic theory provides a solid base for hydrocarbon global exploration and development. On the other hand, the practice of hydrocarbon exploration and development in Asian and North American continental basins supplies a wealth of useful experience. According to a basin-mountain mechanical coupling scenario,there are three types of orogenic belts with their foreland basin counterparts: (1) oceanic subduction orogenic belts and retro-arc foreland basins; (2) continental collision orogenic belts and peripheral foreland basins; and (3) intracontinental orogenic belts and their associated foreland basins. There are two important guidelines for the exploration and development of foreland basin petroleum plays. Firstly, the deformations of the mountain front thrust belt and the foreland basin are spatially under the same strain conditions. Secondly, the pre-thrusting sedimentary sequence, the syn-thrusting sedimentary sequence, and the post-thrusting sedimentary sequence should be explored integrally. |
| Keywords: | oceanic subduction orogenic belt retro-arc foreland basin continental collision orogenic belt peripheral foreland basin intracontinental orogenic belt intracontinent foreland basin |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ | |