本文選題：奧陶系 + 志留系��； 參考：《海相油氣地質(zhì)》2017年03期

【摘要】：通過野外地質(zhì)調(diào)查資料及樣品測試分析,結(jié)合前人研究的結(jié)果,對川東南武隆地區(qū)五峰組—龍馬溪組頁巖氣形成的基礎(chǔ)地質(zhì)條件進行了研究,指出五峰組與龍馬溪組底部富有機質(zhì)頁巖形成于深水陸棚環(huán)境,富有機質(zhì)頁巖厚度大,分布廣,埋深適中(300~3 500 m),脆性礦物含量較高,TOC主要分布于2%~5%之間,熱演化程度處于高成熟—過成熟早期階段,發(fā)育溶蝕(微)孔、粒間微孔、粒內(nèi)微孔、有機質(zhì)孔及微裂縫等,并通過綜合信息疊合分析,提出了5個頁巖氣富集區(qū)。
[Abstract]:Through the field geological survey data and sample test analysis, combined with the results of previous studies, the basic geological conditions for formation of shale gas in the five peak group of Wulong area, the Long Maxi formation, are studied. It is pointed out that the five peak group and the bottom of the Long Maxi formation are rich in the deep-water shelf environment, and the rich shale is thick and widely distributed. The buried depth is moderate (300~3 500 m), the content of brittle minerals is high, and TOC is mainly distributed between 2%~5%. The thermal evolution is in the early stage of high maturity and over maturity, and the dissolution (micro) pores, intergranular micropores, micropores, organic pores and micro cracks are developed, and 5 shale gas enrichment areas have been put forward through comprehensive information overlap analysis.

【作者單位】： 中國地質(zhì)調(diào)查局成都地質(zhì)調(diào)查中心;國土資源部沉積盆地與油氣資源重點實驗室;
【基金】：中國地質(zhì)調(diào)查局“四川盆地頁巖氣基礎(chǔ)地質(zhì)調(diào)查”項目(編號:[2015]01-04-09-001)資助
【分類號】：P618.13

【參考文獻】

相關(guān)期刊論文 前10條

1 王亮;陳云燕;劉玉霞;;川東南彭水地區(qū)龍馬溪組頁巖孔隙結(jié)構(gòu)特征[J];中國石油勘探;2014年05期

2 劉樹根;王世玉;孫瑋;冉波;楊迪;羅超;葉sズ，

本文編號：1889857