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鄂尔多斯盆地白垩系沉积建造

杨友运 

摘 要:鄂尔多斯盆地在白垩纪时期与外围六盘山、河套盆地相隔,是独立的非均衡坳陷盆地.盆地以南北向为轴,盆缘斜坡东缓西陡,盆地轴面西倾,沉降中心位于西侧,沉降中心区沉积厚度明显大于周缘抬升区.不对称结构和沉积环境演化不仅控制了盆内岩性、沉积相及地层分布,导致盆缘以冲积扇、河流相和三角洲平原分流河道相砂砾岩和砂岩沉积为主,盆内为风成沙漠相、三角洲前缘相和湖泊相的砂岩和泥岩.下白垩统平面展布受盆地升降运动、剥蚀与残留变化规律影响,盆地东部和边缘剥蚀作用强,残留厚度小,腹部及西部坳陷区地层发育全,保留厚度大,以洛河组分布最广,其次是环河华池组,罗汉洞组及泾川组仅残留在西部和北部坳陷区.
关键词:沉积相;沉积建造;白垩系;鄂尔多斯盆地
分类号:TE111.3 文献标识码:A

文章编号:0253-9985(2006)02-0167-06

Cretaceous sedimentary formation in Ordos basin

Yang Youyun 

 

基金项目:国家重点基础研究发展规划(973)项目(2003CB2146007);国土资源部"十五"重大项目(1212010331302)
作者简介:杨友运(1959-),男,副教授,沉积学与石油地质
作者单位:杨友运(西安石油大学,陕西,西安,710065) 

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