| 黔北道真地区上奥陶统五峰组—下志留统龙马溪组沉积微相研究 |
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| 引用本文： | 盘应娟,杨忠琴,安亚运,贺永忠,陈厚国,卢树藩,龙建喜.黔北道真地区上奥陶统五峰组—下志留统龙马溪组沉积微相研究[J].中国岩溶,2021,40(5):739-749. |
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| 作者姓名： | 盘应娟 杨忠琴 安亚运 贺永忠 陈厚国 卢树藩 龙建喜 |
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| 作者单位： | 贵州省地质调查院，贵州 贵阳550081 |
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| 基金项目： | 黔北地区石牛栏组岩相古地理与页岩气有利储集相带研究（黔地矿科合[2019]24） |
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| 摘 要： | 上奥陶统五峰组—下志留统龙马溪组是我国南方地区页岩气勘探开发的主要目标层系之一，但对其沉积微相的研究较为薄弱。文章以黔北道真地区为例，通过多条野外剖面和钻孔资料对比研究，结果显示上奥陶统五峰组—下志留统龙马溪组整体属于陆棚相，分属深水陆棚、半深水陆棚两个亚相。其中五峰组及龙马溪组下部属于粉砂质碳泥棚微相，龙马溪组中部属含粉砂质碳泥棚微相，龙马溪组上部属含钙质粉砂质碳泥棚微相。该认识对于黔北地区页岩气有利区的优选具有指示意义。
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| 关 键 词： | 沉积微相 页岩气勘探 道真地区 五峰组 龙马溪组 |
| 收稿时间： | 2021-03-30 |
A sedimentary microfacies study on Wufeng formation-lower Silurian Longmaxi formation of upper Ordovician in Daozhen area, northern Guizhou Province |
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| PAN Yingjuan,YANG Zhongqin,AN Yayun,HE Yongzhong,CHEN Houguo,LU Shufan,LONG Jianxi.A sedimentary microfacies study on Wufeng formation-lower Silurian Longmaxi formation of upper Ordovician in Daozhen area, northern Guizhou Province[J].Carsologica Sinica,2021,40(5):739-749. |
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| Authors: | PAN Yingjuan YANG Zhongqin AN Yayun HE Yongzhong CHEN Houguo LU Shufan LONG Jianxi |
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| Institution: | Guizhou Geological Survey，Guiyang，Guizhou550081，China |
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| Abstract: | The upper Ordovician Wufeng formation to the lower Silurian Longmaxi formation is one of the main target strata for shale gas exploration and development in southern China， however，the research on its sedimentary microfacies is relatively weak. In this study， the comparative study by several field sections and borehole data shows that the upper Ordovician Wufeng formation and lower Silurian Longmaxi formation belong to the continental shelf facies as a whole， which can be subdivided into deep water shelf and shallow water shelf subfacies.The Wufeng formation and the lower part of Longmaxi formation belong to silty carbon mud shack microfacies； the middle part of Longmaxi formation belongs to silty carbon mud shack microfacies， and the upper part of Longmaxi formation belongs to calcareous silty carbon mud shack microfacies. This study is of indicative significance for the optimization of favorable shale gas areas in the northern Guizhou area. |
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