在北中国-阿尔泰斯过渡期间对地构成架构的约束以及对克拉顿边缘改造的影响
Zhuo Ye1,2, Xiaomiao Tan3, Rui Gao3
1SinoProbe Center, Chinese Academy of Geological Sciences, Beijing 100037, China.
National science review
|June 10, 2024
概括
大陆地的演变是由北中国地 (NCC) 和Altaids的地震数据揭示的. NCC显示了进化的,重新加工的地,而Altaids则展示了一个年轻的,复杂的地,提供了对构造过渡的洞察力.
科学领域:
- 地质物理学 地质物理学
- 构造学 构造学 构造学 构造学
- 地质化学 地质化学
背景情况:
- 大陆进化难以量化,阻碍了对地分化和成熟的理解.
- 北中国克拉顿 (NCC) 到东南阿尔泰兹的边界区域代表了一个关键的构造过渡,从一个古老的克拉顿到一个Phanerozoic orogen.
研究的目的:
- 使用地震物理特性量化地的演化阶段.
- 为了划分NCC-Altaids构造过渡的组成架构.
主要方法:
- 集成的被动和主动源地震分析.
- 联合分析和反转来推导地震速度 (Vs) 和Vp/Vs模型.
- 与现有的同位素数据进行整合.
主要成果:
- 北部NCC边缘 (山-扬山带) 显示了具有分层均组成的进化地.
- 下层地的低Vs/高Vp/Vs特征表明,北方NCC边缘自古世中世后期以来发生了重大改造.
- 东南部的Altaids域显示出一个复杂的组成和结构复杂的地,表明青春期的Phanerozoic增殖.
结论:
- 地震成像为地演变提供了深刻的物理性质约束.
- 北部NCC边缘有一个经过重新处理的古老地地下室,由下层地过程和地地相互作用改变.
- 东南部的阿尔泰群岛代表了法内罗纪增殖原体内的青少年地领域.
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