阿尔泰山脉的内部板块推力产物由深度地震反射揭示出来
Lei Zhang1, Lianfeng Zhao1, Liang Zhao2
1Key Laboratory of Earth and Planetary Physics, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China.
Science bulletin
|March 24, 2024
概括
阿尔泰山脉的升起是由深层地结构驱动的,而不仅仅是板块收应变. 一个遗传的推力故障和反形控制变形,解释了显著的升起与低张力率.
科学领域:
- 地力学是什么?地力学是什么?
- 结构地质学 结构地质学
- 板块构造学是一种板块构造学.
背景情况:
- 中亚的阿尔泰河流产物经历了印度-欧亚板块汇聚的洲内变形.
- 尽管与天山山脉相比,它的变压率较低,但它显示出显著的提升.
研究的目的:
- 了解阿尔泰山脉在有限的压力下大幅上升背后的机制.
- 为了创建阿尔泰山脉的详细地图像.
主要方法:
- 一个166.8公里深的地震反射形状的建设.
- 阿尔泰地结构的普雷斯塔克迁移成像.
主要成果:
- 识别了埃尔基斯地的反形状和一个主要的向南倾斜的下层地推力.
- 在阿尔泰弧和东格尔地区之间~10公里的莫霍偏移,与推力联系在一起.
- 在阿尔泰山脉下方的下层地挤出,地加厚和莫霍深化的证据.
结论:
- 一个遗传的南向俯冲推力断层和埃尔基斯反形控制在阿尔泰山脉的代变形.
- 这些结构解释了该地区的显著升起和扩大变形区域,尽管延展率低.
- 一个新的地力学模型突出了遗传结构在板内部变形中的作用.
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