塔里木盆地非构造圈闭特征 |
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引用本文: | 牟泽辉 杨克明. 塔里木盆地非构造圈闭特征[J]. 石油与天然气地质, 1995, 16(4): 348-353 |
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作者姓名: | 牟泽辉 杨克明 |
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作者单位: | 湖北荆沙地质矿产部石油地质综合大队 |
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摘 要: | 塔里木盆地非构造圈闭十分发育。有与不整合有关的起覆圈闭和削截圈闭;有与古隆起有关的潜山圈闭;有与河流、三角洲、滨浅湖等沉积作用有关的岩性圈闭。这些非构造圈闭的形成主控于古构造格局,主要分布于古隆起及古斜坡地带。海西期、印支-燕山期是塔里木盆地非构造同闭的主要形成期,构成以古隆起-潜山-岩性为主体的圈闭系列。
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关 键 词: | 塔里木盆地 非构造圈闭 特征 分布规律 |
CHARACTERISTICS OF NON-STRUCTURAL TRAPS IN TARIM BASIN |
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Abstract: | Non-structural traps are well developed in Tarim Basin and the types are various. The traps include: overlap traps and cut-blocking traps relating to unconformity;buried-hill traps relating to paleo-uplift; lithologic traps relating to the sedimentation of river, delta and shallow lake. The formation of the non-stractural traps was controlled by paleostructural framework. The traps formed primarily in the Hercynian, Indo-China and Yenshan Periods and were distributed in paleouplift and paleoslope belts,thus constituting a paleouplift-buried hill-lithologic trap series. |
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