四川盆地棲霞組—茅口組巖相古地理與天然氣有利勘探區(qū)帶
[Abstract]:The middle Permian marine carbonate formation is an important natural gas producing layer in Sichuan basin, and the exploration potential is great. However, the understanding of the facies belt and its distribution of the stratified dolomite reservoir is not clear, which affects the process of natural gas exploration. Therefore, based on the sedimentary background of Sichuan Basin and taking the favorable reservoir section under sequence stratigraphic framework as the key research unit, the field outcrop profile, drilling data and seismic data are comprehensively analyzed. In lithofacies and paleogeography, the following results have been obtained: (1) the Middle Permian Qixia formation was deposited in a gentle slope background of high southwest and low north east, while the middle Permian Maokou formation superimposed a series of platform rifts distributed in the NW direction on this background. It has evolved into a paleogeographic pattern between Longwa and north east: (2) the transgression area of Qixia formation is an open platform environment, the high level area is a marginal platform, and the platform marginal beach of Jiango-Yaan area is a favorable reservoir facies zone; (3) the transgressive area of Maokou formation is carbonate shelf environment, and the high level area evolves into a rimmed platform, and the terrace marginal (reef) beach and the Taiwa marginal beach of Yanting-Guangan area are favorable reservoir facies zones. It is concluded that the two high-energy granular beach zones in Jiango-Yaan area and Yanting-Guang 'an area are favorable zones for the development of stratified dolomite reservoirs in the middle Permian of the basin and are the main direction of natural gas exploration in the next step.
【作者單位】: 中國(guó)石油杭州地質(zhì)研究院;中國(guó)石油天然氣集團(tuán)公司碳酸鹽巖儲(chǔ)層重點(diǎn)實(shí)驗(yàn)室;中國(guó)石油西南油氣田公司勘探開(kāi)發(fā)研究院;中國(guó)石油勘探開(kāi)發(fā)研究院;
【基金】:國(guó)家科技重大專(zhuān)項(xiàng)(編號(hào):2011ZX05004-002) 中國(guó)石油重大科技專(zhuān)項(xiàng)(編號(hào):2014E-32)
【分類(lèi)號(hào)】:P618.13
【相似文獻(xiàn)】
相關(guān)期刊論文 前5條
1 李君;吳曉東;楊柏松;楊慎;劉艷;林世國(guó);;中國(guó)天然氣聚集與分布新認(rèn)識(shí)及有利勘探區(qū)帶預(yù)測(cè)[J];新疆石油地質(zhì);2014年02期
2 吳世祥,汪澤成,張林,沈玨紅,羅啟后;川西坳陷T_3成藏主控因素與有利勘探區(qū)帶分析[J];中國(guó)礦業(yè)大學(xué)學(xué)報(bào);2002年01期
3 周慧;趙宗舉;劉燁;羅忠;張寶民;劉玉娥;張興陽(yáng);江青春;李秋芬;高志勇;楊雨;劉銀河;;四川盆地及鄰區(qū)早三疊世印度期層序巖相古地理及有利勘探區(qū)帶[J];石油學(xué)報(bào);2012年S2期
4 張可寶;張紅斌;趙玉光;何曉松;孫志華;;均方根振幅與巖性[J];石油地球物理勘探;2007年S1期
5 ;[J];;年期
相關(guān)會(huì)議論文 前2條
1 廖遠(yuǎn)濤;王華;王家豪;侯宇光;夏存銀;;板橋凹陷古近系沉積體系特征及有利勘探區(qū)帶預(yù)測(cè)[A];中國(guó)礦物巖石地球化學(xué)學(xué)會(huì)第12屆學(xué)術(shù)年會(huì)論文集[C];2009年
2 汪立群;張曉寶;徐子遠(yuǎn);姜桂鳳;馬素萍;譚彥虎;劉志強(qiáng);;柴北緣深層氣藏形成的地質(zhì)條件及有利勘探區(qū)帶[A];第十屆全國(guó)有機(jī)地球化學(xué)學(xué)術(shù)會(huì)議論文摘要匯編[C];2005年
,本文編號(hào):2333456
本文鏈接:http://sikaile.net/kejilunwen/diqiudizhi/2333456.html