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四川盆地西南地区下三叠统嘉陵江组沉积相研究
引用本文:朱露,胡明毅,段健,侯慧敏.四川盆地西南地区下三叠统嘉陵江组沉积相研究[J].海洋地质译丛,2010(1):43-47.
作者姓名:朱露  胡明毅  段健  侯慧敏
作者单位:[1]长江大学油气资源与勘探技术教育部重点实验室,湖北荆州434023 [2]中国石油冀东油田分公司,河北唐山063200
摘    要:通过对钻井岩心和测井等资料的研究,认为川西南地区下三叠统嘉陵江组存在着混积潮坪、开阔台地、局限台地和蒸发台地4种沉积相类型。嘉一期主要发育混积潮坪相和开阔台地相,嘉三期主要发育开阔台地相,嘉二、嘉四、嘉五期主要发育局限台地和蒸发台地相。选取并研究地层厚度、灰岩厚度、白云岩厚度和颗粒岩厚度等四种能反映沉积环境和沉积相的地质因素,指出了每个层段的沉积相平面分布特征。

关 键 词:川西南地区  下三叠统  嘉陵江组  沉积相

Study on sedimentary facies of Jialingjiang Formation in southwest of Sichuan Basin
Authors:Zhu Lu  Hu Mingyi  Duan Jian  Hou Huimin
Institution:1. Key Laboratory of Exploration for Oil and Gas Resource ( Ministry of Education ), Yangtze University, Jingzhou 434023; 2, Jidong Oil field Branch Company, PetroChina , Tangshan 063200)
Abstract:According to the study of core and well logging data, it is recognized that the mixed tidal flat, the open platform, restricted platform and evaporative platform were developed in Jialingjiang Formation. Mixed tidal flat and open platform developed in the first Jialingjiang period, open platform developed in the third JialinKjiang period, restricted platform and evaporative platform developed in the second, the fourth and the fifth Jialingjiang periods. The facies distribution of four key formations were pointed out after thorough study of four geologic factors that could embody sedimentary environment and facies, which is the thickness of formation, limestone, dolostone and grainstone.
Keywords:southwest of Sichuan Basin  lower Triassic  Jialingjiang Formation  sedimentary facies
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