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六盘山盆地与酒西盆地中新生代构造对比
引用本文:张柏桥,胡望水,舒志国,罗忠辉,陆亚秋,巴秀娥.六盘山盆地与酒西盆地中新生代构造对比[J].石油天然气学报,2004,26(1):11-14.
作者姓名:张柏桥  胡望水  舒志国  罗忠辉  陆亚秋  巴秀娥
作者单位:1. 中国地质大学(武汉)资源学院,湖北 武汉 430074;江汉油田分公司,湖北 潜江 433124
2. 长江大学地球科学学院,湖北 荆州 434023
3. 江汉油田分公司,湖北 潜江 433124
4. 中国地质大学(武汉)资源学院,湖北 武汉 430074
基金项目:中国石油化工股份有限公司攻关项目 (XBKY0 1 13 )
摘    要:六盘山盆地与酒西盆地中新生代构造具有很好的相似性。中生代盆地为走滑拉分盆地,发育张扭伸展断层系(边界走滑断裂.盆内伸展正断层)。一级构造单元为断陷、断隆;新生代盆地是陆内前陆盆地,发育扭压逆冲断裂系,盆地一侧发育逆冲推覆体,一级构造单元为逆掩冲断褶皱区、坳陷、斜坡。因此,可以利用酒西盆地的资料和勘探成果认识六盘山盆地.借助酒西盆地的勘探经验指导六盘山盆地的下一步勘探。

关 键 词:中生代  新生代  含油气盆地  构造  对比  六盘山盆地  酒西盆地
文章编号:1000-9752(2004)01-0011-04

Mesozoic and Cenozoic Structural Comparison in Liupanshan Basin and Jiuxi Basin
ZHANG Bo-qiao.Mesozoic and Cenozoic Structural Comparison in Liupanshan Basin and Jiuxi Basin[J].Journal of Oil and Gas Technology,2004,26(1):11-14.
Authors:ZHANG Bo-qiao
Abstract:Mesozoic-Cenozoic structures in Liupanshan Basin and Jiuxi Basin have a good compatibility. The Mesozoic basin is a slide and pull apart one, where tenso-shear and extension fault system (its boundary is slide fault, the interior is extension fault )is developed. Primary structural units are faulted depression and faulted uplift. The Cenozoic basin is an intracontinental foreland basin, where transpressional and thrust fault systems are developed, thrust nappes are developed on one side of the basin, its primary structural units are thrust fold region, depression and slopes. Data from Jiuxi Basin and its exploration result could be used to comprehend Liupanshan Basin and to guide next exploration in the basin with the help of exploration experience in Jiuxi Basin.
Keywords:Mesozoic  Cenozoic  oil and gas bearing basin  structure  comparison  Liupanshan Basin  Jiuxi Basin
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