高级检索

    黔南-桂中地区泥盆系层序地层格架中的储集体特征研究

    康建威, 林小兵, 田景春, 张翔

    康建威, 林小兵, 田景春, 张翔. 黔南-桂中地区泥盆系层序地层格架中的储集体特征研究[J]. 沉积与特提斯地质, 2010, 30(3): 76-83.
    引用本文: 康建威, 林小兵, 田景春, 张翔. 黔南-桂中地区泥盆系层序地层格架中的储集体特征研究[J]. 沉积与特提斯地质, 2010, 30(3): 76-83.
    KANG Jian-wei, LIN Xiao-bing, TIAN Jing-chun, ZHANG Xiang. Reservoir characteristics within the Devonian sequence stratigraphic framework in the southern Guizhou-central Guangxi region[J]. Sedimentary Geology and Tethyan Geology, 2010, 30(3): 76-83.
    Citation: KANG Jian-wei, LIN Xiao-bing, TIAN Jing-chun, ZHANG Xiang. Reservoir characteristics within the Devonian sequence stratigraphic framework in the southern Guizhou-central Guangxi region[J]. Sedimentary Geology and Tethyan Geology, 2010, 30(3): 76-83.

    黔南-桂中地区泥盆系层序地层格架中的储集体特征研究

    基金项目: 

    中国地质调查局《中国岩相古地理编图》(基[2009]01-12-13)

    Reservoir characteristics within the Devonian sequence stratigraphic framework in the southern Guizhou-central Guangxi region

    • 摘要: 通过对黔南坳陷和桂中坳陷的地层对比和分析,识别出了8种层序界面标志,共划分两个超(二级)层序SS1和SS2,并讨论了各体系域特征。在层序格架中对研究区内的储集体类型进行了总结,主要包括生物礁(滩)储集体、白云岩储集体和缝洞型储集体等3种类型。对层序格架中储集体的成因类型进行了总结归纳:有利的储集体主要有TST礁滩灰岩储集体、HST礁滩灰岩、白云岩储集体。
      Abstract: Eight sequence boundaries are recognized for the South Guizhou depression and Central Guangxi depression,including two supersequences(second-order sequences) SS1 composed of lowstand systems tract(LST),transgressive systems tract(TST) and highstand systems tract(HST),and SS2 composed of transgressive systems tract(TST) and highstand systems tract(HST).The reservoir rocks within the above-mentioned sequence stratigraphic framework consist of organic reef(bank) reservoirs,dolostone reservoirs and fissure-type reservoirs.The favourable reservoir rocks include the organic reef(bank) limestone reservoirs in the transgressive systems tract,organic reef(bank) limestone reservoirs and dolostone reservoirs in the highstand systems tract.
    计量
    • 文章访问数:  113
    • HTML全文浏览量:  6
    • PDF下载量:  78
    • 被引次数: 0
    出版历程
    • 发布日期:  2010-09-29

    目录

      /

      返回文章
      返回