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塔里木盆地三叠纪前缘隆起迁移演化规律

DOI: 10.7605/gdlxb.2013.02.019, PP. 219-230

Keywords: 前缘隆起,隆后坳陷,前陆盆地,塔里木盆地,三叠系

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Abstract:

利用大量钻测井及地震资料,通过对邻近前缘隆起的隆后坳陷地层特征的分析以及与库车河露头的对比,探讨了塔里木盆地三叠纪前缘隆起的迁移演化规律。结果表明,三叠纪前缘隆起发生了3次往复迁移,隆后坳陷地区发育多期不整合面,且最大不整合面均发育于地层的底部。早三叠世,隆后坳陷地层南厚北薄,早期前缘隆起向天山方向迁移,隆后坳陷地层超覆其上,前陆坳陷变窄;晚期则向克拉通方向迁移隆升,邻近的隆后坳陷地层遭受强烈剥蚀。由于前缘隆起的遮挡作用,该时期前陆坳陷与隆后地区尚未贯通,山前发育冲积扇。中、晚三叠世前缘隆起又发生两次迁移,其迁移特征与早三叠世类似,但中三叠世前陆坳陷与隆后坳陷仍未相连,而晚三叠世两者相互连通。

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