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科学通报  2015 

鄂尔多斯盆地渭北隆起抬升期次及过程的裂变径迹分析

DOI: 10.1360/N972014-00617, PP. 1298-1309

Keywords: 裂变径迹分析,镜质体反射率,热史模拟,抬升过程,渭北隆起,鄂尔多斯盆地,秦岭造山带

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Abstract:

渭北隆起处于活动带(秦岭造山带)与稳定地块(鄂尔多斯地块)的过渡地带,构造位置独特重要,该带抬升期次及过程的确定对盆山作用、盆地动力学演化及油气成藏研究具有重要意义.本文运用磷灰石、锆石裂变径迹分析方法及热史模拟方法对渭北隆起进行了低温热年代学研究,研究表明渭北隆起抬升冷却在南北方向上具有明显的差异性,具有南早北晚的特点.南部奥陶系-下二叠统抬升早,主要为早白垩世晚期102~107Ma以来,北部自新生代65Ma以来抬升,主要抬升时期为晚始新世40Ma以来.渭北隆起主要有早白垩世晚期(102~107Ma)及40Ma以来两期快速隆升,40Ma以来为渭北隆起的主要快速隆升时期.热演化史模拟曲线表明渭北隆起在约125~100Ma快速抬升,在100~40Ma为缓慢抬升,自古近纪晚始新世约40Ma以来,特别是5Ma以来发生快速抬升冷却.渭北隆起新生代40Ma以来的整体快速隆升与秦岭造山带北缘的隆升具有同时性,与渭河盆地的新生代以来快速沉降具有很好的耦合关系.

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