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    胡忠贵, 郑荣才, 胡明毅, 胡九珍, 郑超. 川东邻水—渝北地区石炭系层序-岩相古地理特征[J]. 中国地质, 2010, 37(5): 1383-1392.
    引用本文: 胡忠贵, 郑荣才, 胡明毅, 胡九珍, 郑超. 川东邻水—渝北地区石炭系层序-岩相古地理特征[J]. 中国地质, 2010, 37(5): 1383-1392.
    HU Zhong-gui, ZHENG Rong-cai, HU Ming-yi, HU Jiu-zhen, ZHENG Chao. Sequence-based lithofacies and paleogeography of Carboniferous Huanglong Formation in Linshui (eastern Sichuan)-northern Chongqing area[J]. GEOLOGY IN CHINA, 2010, 37(5): 1383-1392.
    Citation: HU Zhong-gui, ZHENG Rong-cai, HU Ming-yi, HU Jiu-zhen, ZHENG Chao. Sequence-based lithofacies and paleogeography of Carboniferous Huanglong Formation in Linshui (eastern Sichuan)-northern Chongqing area[J]. GEOLOGY IN CHINA, 2010, 37(5): 1383-1392.

    川东邻水—渝北地区石炭系层序-岩相古地理特征

    Sequence-based lithofacies and paleogeography of Carboniferous Huanglong Formation in Linshui (eastern Sichuan)-northern Chongqing area

    • 摘要: 提要:川东邻水—渝北地区由于受海西早期强烈构造隆升和侵蚀作用影响,仅残存不完整的上石炭统黄龙组,为川东地区天然气藏主要产层,也是邻区寻找新气源最有利层位之一。本文根据岩心观察和室内镜下岩石薄片鉴定分析,并结合岩石学、古生物及测井等沉积相标志研究,确定该区黄龙组发育萨勃哈、有障壁海岸和海湾陆棚等沉积相带,进一步划分出若干亚相和微相。应用Vail为代表的经典层序地层学原理及其技术方法将黄龙组划分为1个Ⅰ型三级层序,细分为LST、TST和HST 3个体系域。在详尽沉积相和层序地层研究的基础上,以体系域为单位进行了层序-岩相古地理编图并对其演化特征进行了描述。结合各相带储层物性特征,认为障壁滩和滨外浅滩为最有利储集相带。

       

      Abstract: Abstract:The Linshui (eastern Sichuan)-northern Chongqing area only keeps unsound Upper Carboniferous Huanglong Formation because of intense structural uplift and erosion in early Hercynian period,and the Huanglong Formation of the study area is one of the most important natural gas reservoirs in eastern Sichuan area and one of the most favorable horizons in search for new gas sources. Based on core description and thin section analysis,combined with sedimentary lithologic marks,palaeontology and logging analysis,the authors have divided the Huanglong Formation into three main sedimentary facies, i.e., sabkha,gulf shelf and shore,and further divided these facies into many subfacies and microfacies. Using the classic sequence stratigraphy principle and technology represented by Vail,the authors have divided the Huanglong Formation into one sequence of Ⅰtype and three system tracts:LST,TST and HST. On the basis of a detailed analysis of sedimentary facies and sequence stratigraphy,the authors have compiled and described the sequence-paleogeographic maps which take the system tracts as the mapping units. Combined with the reservoir characteristics of all sorts of sedimentary facies,the barrier grain beach and the offshore grain beach are thought to be the most favorable reservoir facies.

       

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