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作 者:宋玉光[1] 赵路子[1] 贾国相[2] 颜自给[2] 阳翔[2]
机构地区:[1]四川石油管理局川西南矿区 [2]中国有色金属工业总公司矿产地质研究院
出 处:《矿产与地质》1998年第4期275-280,共6页Mineral Resources and Geology
摘 要:西昌盆地是攀西地区中,新生代陆相断陷坳陷盆地。盆地内断裂褶皱发育,岩浆活动频繁,对于盆地内油气保存条件的好坏一直无法定论。通过盆地七里坝构造油气化探工作,发现了油气化探弱异常,进行了化探异常特征、存在形式以及与油气的关系的研究,结果表明,七里坝构造地表的各类异常是客观存在的,该构造内存在有异常源,但异常源的烃量可能已有相当部分逸散掉了。Xichang Basin is a continental faultsubsidence basin formed during MesozoicCenozoic Eons in Panxi region. In the basin,there exist many folds and faults and frequent magmatic activities.Which leaves the storage of oilgas in the basin open to question.Through the oilgas geochemical prospecting in Qiliba Basin,weak geochemical anomalies of oilgas were found and their features, existing forms and relation with oilgas are studied. It is shown that various anomalies objectively exist in the surface of Qiliba structure,indicating the existence of anomaly sources in the structure, from which considerable amount of hydrocarbons might have escaped.
分 类 号:P618.130.8[天文地球—矿床学]
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