辽宁工程技术大学学报(自然科学版)
遼寧工程技術大學學報(自然科學版)
료녕공정기술대학학보(자연과학판)
JOURNAL OF LIAONING TECHNICAL UNIVERSITY(NATURAL SCIENCE)
2013年
7期
896-900
,共5页
赵群%王红岩%刘大锰%姚艳斌%杨慎%刘德勋
趙群%王紅巖%劉大錳%姚豔斌%楊慎%劉德勛
조군%왕홍암%류대맹%요염빈%양신%류덕훈
页岩气%压力系数%超压%含气量%脆性矿物%构造%储层%海相
頁巖氣%壓力繫數%超壓%含氣量%脆性礦物%構造%儲層%海相
혈암기%압력계수%초압%함기량%취성광물%구조%저층%해상
shale gas%pressure factor%over pressure%gas content%brittle mineral%tectonic%reservoir%marine
为解中国南方海相页岩气成藏的基本特征,厘清成藏要素,建立符合中国复杂构造背景下页岩气储层选区评价指标等问题,借鉴美国页岩气储层评价指标,结合目前页岩气勘探评价成果,分析得出:中上扬子地区龙马溪组底部富有机质页岩储层分布连续、埋深适中、构造稳定,富有机质页岩在区域上分布连续,但含气性在局部表现为不连续;根据构造改造的程度,将中上扬子地区龙马溪组页岩分为构造改造区、靠近剥蚀区和构造稳定区三种类型。其中构造稳定区页岩储层表现为超压、含气量高,气井试采初期产量高,是中国中上扬子地区海相页岩气成藏的最有利区。
為解中國南方海相頁巖氣成藏的基本特徵,釐清成藏要素,建立符閤中國複雜構造揹景下頁巖氣儲層選區評價指標等問題,藉鑒美國頁巖氣儲層評價指標,結閤目前頁巖氣勘探評價成果,分析得齣:中上颺子地區龍馬溪組底部富有機質頁巖儲層分佈連續、埋深適中、構造穩定,富有機質頁巖在區域上分佈連續,但含氣性在跼部錶現為不連續;根據構造改造的程度,將中上颺子地區龍馬溪組頁巖分為構造改造區、靠近剝蝕區和構造穩定區三種類型。其中構造穩定區頁巖儲層錶現為超壓、含氣量高,氣井試採初期產量高,是中國中上颺子地區海相頁巖氣成藏的最有利區。
위해중국남방해상혈암기성장적기본특정,전청성장요소,건립부합중국복잡구조배경하혈암기저층선구평개지표등문제,차감미국혈암기저층평개지표,결합목전혈암기감탐평개성과,분석득출:중상양자지구룡마계조저부부유궤질혈암저층분포련속、매심괄중、구조은정,부유궤질혈암재구역상분포련속,단함기성재국부표현위불련속;근거구조개조적정도,장중상양자지구룡마계조혈암분위구조개조구、고근박식구화구조은정구삼충류형。기중구조은정구혈암저층표현위초압、함기량고,기정시채초기산량고,시중국중상양자지구해상혈암기성장적최유리구。
To understand the characteristic of shale gas reservoir in the southern China, clarify the accumulation elements and build the shale gas screening parameters for China’s complex tectonic background with the combination of the shale gas exploration evaluation results, the study concludes that the organic-rich marine shale at the bottom Longmaxi distributes continually, with moderate buried depth and stable tectonic setting. The Longmaxi organic-rich shale spreads continuously in space, but the gas content is discontinuous in some region. According to the tectonic reworking characteristic, the Middle-Upper Yangtze region with Longmaxi shale is divided into the tectonic damage area, close to the denuded area and tectonic stable area. Shale reservoir in the tectonic damage area is overpressure and high gas content, and high initial gas rate was acquired in exploration. So the tectonic stable area is the most favorable area for shale gas accumulation.