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,(3):76-83.[点击复制]
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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
0
(1. 成都地质矿产研究所;
2. 成都理工大学油气藏地质及开发工程国家重点实验室)
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。
关键词:  黔南凹陷  桂中凹陷  泥盆系  层序地层格架  储集体
DOI:
附件
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
KANG Jian-wei, LIN Xiao-bing, TIAN Jing-chun, ZHANG Xiang
(1. Chengdu Institute of Geology and Mineral Resources, Chengdu 610081, Sichuan, China;
2. State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation, Chengdu University of Technology, Chengdu 610059, Sichuan, China)
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.
Key words:  South Guizhou depression  Central Guangxi depression  Devonian  sequence stratigraphic framework  reservoir rock

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