兰坪盆地古近系宝相寺组层序地层分析
Sequence Stratigraphy Analysis of Paleogene Baoxiangsi Formation in Lanping Basin
运用层序地层学原理,对兰坪盆地中部古近系宝相寺组进行深入研究,划分出一个Ⅰ型层序及三个Ⅱ型层序界面。阐述了兰坪盆地中部古近系宝相寺组层序格架及砂体结构特征,建立层序地层格架演化模式图,反应了湖平面变化对砂体沉积结构具有重要影响。低位体系域早期河流侵蚀强烈,多以中粒为主,晚期发育复合状砂体;湖侵体系域砂体多为细粒砂泥岩,呈孤立状形态;高位体系域砂体以席状砂体为主,主要由滨浅湖、半深湖和湖泊三角洲沉积体系构成。
ccording to the theory and approach of the sequence Stratigraphy,we have investigated the Paleogene Baoxiangsi Formation outcrops in Lanping Basin,and identified four sequence boundaries(oneⅠtype and threeⅡtype).Sequence stratigraphy framework model and sandbody architecture have been illustrated, furthermore ,evolutionary model of sequence strata have been established and lacustrine level change on sand body sedimentary structure have an important influence in Lanping Basin;the sand body may have eroded in early LST, and many in grain of sandstone primarily,amalgamed channel filled sand body was espected in late LST;Sand body more for fine-grained mudstone, show isolation shape form in TST;Sand body in table form sand body is given priority to, mainly by the littoral and shallow lake, half a deep lake and lake delta depositional system formed in HST.
阮林森、冯志强、郭建秋
地质学
层序地层相对湖平面变化砂体结构宝相寺组兰坪盆地
sequence stratarelative lacustrine level changsandbody architectureBaoxiangsi FormationLanping Basin
阮林森,冯志强,郭建秋.兰坪盆地古近系宝相寺组层序地层分析[EB/OL].(2011-03-14)[2025-08-16].http://www.paper.edu.cn/releasepaper/content/201103-598.点此复制
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