大陆变形的热力学
Ajay Kumar1, Mauro Cacace2, Magdalena Scheck-Wenderoth2,3
1GFZ German Research Centre for Geosciences, Potsdam, Germany. kumar@gfz-potsdam.de.
Scientific reports
|November 14, 2023
概括
大陆变形是由构造力和岩层强度驱动的. 数据驱动的建模表明,高山喜马拉雅碰撞区的平衡偏差如何控制变形,导致稳定状态或失控的延伸.
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
- 热力学是一种热力学.
背景情况:
- 大陆的变形是由构造力和引力力造成的.
- 石质层强度受热放松的影响,决定了变形模式.
- 在这些力量的基础上,平衡或失控的延伸发生.
研究的目的:
- 为了证明平衡偏差如何控制大陆变形.
- 用数据驱动的热力学建模分析高山喜马拉雅碰撞区.
- 为了量化内部板块能量和构造力之间的平衡.
主要方法:
- 数据驱动的热力学建模.
- 对阿尔卑斯山和喜马拉雅山脉碰撞区的分析.
- 对关键地厚度的量化.
主要成果:
- 地幔动力学,板块边界力和石质层影响变形之间的平衡偏差.
- 较厚的地领域 (orogens) 削弱并将能量分散到更广的区域.
- 一个散热热力学反循环控制了orogenic石化层中的能量散散.
- 放射性热源减轻了失控的延伸,使原体达到平衡.
结论:
- 一个关键的地厚度平衡了内部能量和构造力.
- 源性减弱和能量消耗与厚厚的放射性地有关.
- 表明地的热化学状态和地球类行星上的构造进化之间存在联系.
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