作者:闫德宇;黄文辉;李昂;刘浩;刘翰林; 时间:2013-01-01 点击数:
闫德宇;黄文辉;李昂;刘浩;刘翰林;
1:中国地质大学(北京)能源学院
2:中国地质大学(北京)海相储层演化与油气富集机理教育部重点实验室
摘要(Abstract):
以鄂尔多斯盆地海陆过渡相富有机质泥页岩为研究对象,分析野外露头和岩心观察、采样、地化参数和物性参数等测试资料,研究富有机质泥页岩的沉积相、厚度及分布、有机质类型及含量、热成熟度、孔隙度等页岩气成藏条件.结果表明:鄂尔多斯盆地上古生界石炭—二叠系海陆过渡相富有机质泥页岩主要发育在沼泽相和三角洲相,常与煤层、灰岩、致密砂岩等互层,纵横向变化快,单层厚度小,累计厚度大,有机碳含量相对海相、陆相泥页岩较高.有机质类型以腐殖型为主,有机质热成熟度处在成气高峰阶段,有利于页岩气的形成.综合页岩气藏评价的各项指标信息,预测鄂尔多斯盆地石炭—二叠系海陆过渡相页岩气藏最有利发育区位于盆地东部神木—绥德—延长一带的山西组、盆地北部乌审旗—杭锦旗—东胜—神木与鄂托克旗—盐池一带的太原组及盆地东北部靖边—横山—榆林—神木一带的本溪组,虽然各组地层埋深较大,但多与煤层、致密砂岩层互层,形成页岩气、煤层气和致密砂岩气叠置成藏,具有较大的勘探与开发潜力.
关键词(KeyWords):页岩气;聚集条件;有利区预测;海陆过渡相;鄂尔多斯盆地
Abstract:
Keywords:
基金项目(Foundation):国家科技重大专项(2011ZX05042-001-002);; 国家自然科学基金项目(40972106);; 国土资源部全国油气资源战略选区调查与评价国家专项(2009GYXQ-15)
作者(Author):闫德宇;黄文辉;李昂;刘浩;刘翰林;
Email:
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