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新疆塔西河地区8Ma以来沉积环境演化及其构造意义

, PP. 243-252

Keywords: 沉积相,沉积环境演化,构造隆升,晚新生代,天山

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Abstract:

天山南北麓巨厚的新生代地层记录着天山构造隆升与沉积环境演化的历史。在对新疆塔西河剖面进行磁性地层研究的基础上,通过沉积学分析,确定自8.1Ma以来塔西河剖面存在4个沉积相组合,对应的沉积环境演化分为4个阶段:1)在8.105.75MaB.P.之前为浅湖沉积环境;2)在5.754.27MaB.P.为扇三角洲沉积环境;3)在4.273.44MaB.P.为滨浅湖沉积环境;4)在3.44MaB.P.之后为冲积扇沉积旋回期。塔西河剖面沉积环境演化、岩相与沉积速率的变化等共同揭示出天山自8.1MaB.P.以来先后经历了构造活动稳定期(>5.75MaB.P.)、过渡期(5.753.44MaB.P.)以及快速强烈间歇性隆升期(<3.44MaB.P.)等3个构造活动阶段,并且自3.44MaB.P.,构造活动有增强的趋势。

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