本文選題：開(kāi)江-梁平海槽東南緣　切入點(diǎn)：長(zhǎng)興組　出處：《西南石油大學(xué)》2015年碩士論文

【摘要】：開(kāi)江-梁平地區(qū)上二疊統(tǒng)長(zhǎng)興組作為區(qū)域內(nèi)重要的天然氣產(chǎn)層,受到了國(guó)內(nèi)的廣泛關(guān)注,但針對(duì)長(zhǎng)興組沉積相和儲(chǔ)層的發(fā)育分布規(guī)律意見(jiàn)不一。本文以經(jīng)典層序地層學(xué)、沉積學(xué)及儲(chǔ)層地質(zhì)學(xué)等為理論指導(dǎo),以開(kāi)江-梁平海槽東南緣上二疊統(tǒng)長(zhǎng)興組為對(duì)象,通過(guò)分析區(qū)內(nèi)鉆測(cè)井、巖心薄片、地震剖面及鄰區(qū)露頭資料,對(duì)長(zhǎng)興組進(jìn)行地層劃分,建立層序地層格架,并在格架內(nèi)對(duì)長(zhǎng)興組沉積相及儲(chǔ)層展開(kāi)研究,厘清了長(zhǎng)興組儲(chǔ)層發(fā)育與層序、沉積相的關(guān)系,確定了長(zhǎng)興組儲(chǔ)層的發(fā)育分布規(guī)律。 根據(jù)巖石類(lèi)型組合、沉積旋回等特征,研究區(qū)長(zhǎng)興組自下而上可劃分為長(zhǎng)一段(P3chl)、長(zhǎng)二段(P3ch2)和長(zhǎng)三段(P3ch3)。同時(shí),通過(guò)巖心薄片、鉆錄測(cè)井和地震剖面等資料分析,長(zhǎng)興組可劃分為兩個(gè)均由海侵域(TST1)、TST2)和高位域(HST1、HST2)組成的Ⅱ型三級(jí)層序(SQ1、 SQ2),并建立三級(jí)層序地層格架。其中,TSTl、HST1、TST2-HST2分別與長(zhǎng)一段、長(zhǎng)二段、長(zhǎng)三段對(duì)應(yīng),區(qū)域可對(duì)比性好。 結(jié)合巖心薄片與鉆測(cè)井等資料對(duì)長(zhǎng)興組進(jìn)行沉積相分析,以體系域?yàn)閱卧?等時(shí)動(dòng)態(tài)地揭示了研究區(qū)長(zhǎng)興組沉積相(尤其礁灘相)的時(shí)空分布及演化。TST1時(shí)期,區(qū)內(nèi)以開(kāi)闊臺(tái)地沉積為主,局部發(fā)育生屑灘,其后期臺(tái)緣相帶雛形形成；HST1時(shí)期,礁灘相大規(guī)模分布,臺(tái)地邊緣迅速沉積增厚,臺(tái)緣相帶演化成熟,臺(tái)地內(nèi)以開(kāi)闊臺(tái)地為主,局部發(fā)育生屑灘；TST2時(shí)期,繼承了前期相帶分布格局,但臺(tái)緣礁灘相規(guī)模明顯縮小,臺(tái)地內(nèi)以開(kāi)闊臺(tái)地為主,局部發(fā)育生屑灘；HST2早期,臺(tái)緣礁僅五百梯地區(qū)有小規(guī)模分布,末期臺(tái)緣帶局部發(fā)育潮坪沉積,開(kāi)闊臺(tái)地演變?yōu)榫窒夼_(tái)地。 綜合巖心薄片、測(cè)錄井和物性資料等分析,長(zhǎng)興組主要發(fā)育生物礁相云巖或灰?guī)r類(lèi)、生屑灘相云巖或灰?guī)r類(lèi)、潮坪或礁坪或?yàn)┖笃壕ЯＴ茙r類(lèi)溶蝕孔隙(洞)型儲(chǔ)層,以云巖類(lèi)儲(chǔ)集性最佳,灰?guī)r類(lèi)次之。垂向上,長(zhǎng)興組儲(chǔ)層主要發(fā)育于高位域中后期,與生物礁灘相沉積體系關(guān)系密切,主要分布在向上水體變淺的單體礁灘相沉積體系的中上部,溶蝕、云化作用強(qiáng)烈,孔洞發(fā)育好；而海侵域時(shí)期或在向上水體變深的單體礁灘相沉積體系中,溶蝕、云化程度低,以灰?guī)r類(lèi)儲(chǔ)層為主,孔隙性較差。平面上,長(zhǎng)興組儲(chǔ)層主要分布在臺(tái)地邊緣相帶和臺(tái)地內(nèi)部,斜坡-海槽區(qū)儲(chǔ)層不發(fā)育。根據(jù)儲(chǔ)層類(lèi)型、溶蝕云化程度及規(guī)模、優(yōu)質(zhì)儲(chǔ)層數(shù)量及規(guī)模等指標(biāo),研究區(qū)可定性劃分為4類(lèi)長(zhǎng)興組儲(chǔ)層發(fā)育區(qū)：溶蝕、云化作用強(qiáng)烈且規(guī)模較大的臺(tái)緣礁灘相分布區(qū)屬于Ⅰ類(lèi)發(fā)育區(qū),溶蝕、云化作用較強(qiáng)的臺(tái)緣礁灘相或臺(tái)內(nèi)淺灘相分布區(qū)屬于Ⅱ類(lèi)發(fā)育區(qū),溶蝕、云化較弱的臺(tái)緣或臺(tái)內(nèi)淺灘相灰?guī)r沉積區(qū)屬于Ⅲ類(lèi)發(fā)育區(qū),而開(kāi)闊臺(tái)地或局限臺(tái)地內(nèi)非礁灘相灰?guī)r沉積區(qū)屬于Ⅳ類(lèi)發(fā)育區(qū)。
[Abstract]:The Changxing formation of Upper Permian in Kaijiang-Liangping area, as an important natural gas layer in the region, has received extensive attention in China, but there are different opinions on the development and distribution of sedimentary facies and reservoirs in Changxing formation.Based on the theory of classical sequence stratigraphy, sedimentology and reservoir geology, and taking the upper Permian Changxing formation in the southeast margin of Kaijiang-Liangping trough as the object, this paper analyzes the drilling log, core slice, seismic profile and outcrop data of adjacent areas.The stratigraphic division of Changxing formation, the establishment of sequence stratigraphic framework, the study of sedimentary facies and reservoir of Changxing formation in the framework, the relationship between reservoir development and sequence and sedimentary facies of Changxing formation, and the distribution law of reservoir development in Changxing formation are clarified.According to the characteristics of rock type assemblage and sedimentary cycle, the Changxing formation in the study area can be divided from the bottom to the top into long first member P3chlang, long second member P3ch2) and Chang3 member P3ch3.At the same time, the Changxing formation can be divided into two types: type 鈪，

本文編號(hào)：1713415