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地质学报  2010 

柴达木盆地阿尔金斜坡带构造特征与阿尔金断裂形成时间讨论――以月牙山地区为例

, PP. 1275-1283

Keywords: 构造特征,断层相关褶皱,生长地层,形成时间,阿尔金断裂,阿尔金斜坡带,柴达木盆地

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Abstract:

研究区位于柴达木盆地阿尔金斜坡带的中段,跨越柴达木盆地、阿尔金断裂和索尔库里盆地三个构造单元,阿尔金斜坡带总体上表现为大致向南倾斜的斜坡,是一个在三位空间上变化的曲面,其包络面的走向与阿尔金断裂的走向基本一致。阿尔金斜坡带由与阿尔金断裂伴生的轴向近东西、靠近断裂逐渐向其收敛的背斜构成,在阿尔金山前表现为一系列斜列鼻状构造,在空间上呈宽缓的、隆拗相间的有规律性变化,在大部分地段表现为由堆垛式双重构造自北向南的逆冲作用形成的大型背斜的前翼。根据背斜前翼生长地层确定阿尔金断裂自下干柴沟组上段沉积时期(38Ma)开始形成,至今一直处于持续的活动状态。在下干柴沟组上段至上油砂山组沉积时期(38~8.1Ma),断裂的活动强度较小,自狮子沟组沉积开始(8.1Ma),断裂的活动强度明显增大。

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