压缩诱导的降温启动的位置由结构与热继承控制
Éva Oravecz1,2, Taras Gerya2, Attila Balázs2
1Department of Geology, Institute of Geography and Earth Sciences, Eötvös Loránd University, Pázmány Péter sétány 1/C, 1117 Budapest, Hungary.
概括
俯冲的启动取决于板块运动的反转速度和石质层遗传的弱点. 突如其来的变化会导致脊的反转,而较慢的过渡则利用先前存在的断层区域来启动俯冲.
科学领域:
- 地力学是什么?地力学是什么?
- 构造学 构造学 构造学 构造学
- 计算建模 计算建模
背景情况:
- 降温启动是威尔逊周期的一个关键但不太了解的阶段.
- 了解它的机制是解读板块构造学和地球演变的关键.
研究的目的:
- 调查控制压缩诱导的降温启动的因素.
- 分析板块运动逆转时间和石质层遗传的影响.
主要方法:
- 采用3D合热力学和表面工艺模型.
- 分析了石质层强度和应变分布.
主要成果:
- 突发的板块运动逆转触发了脊逆转驱动的降温,受热和融化减弱的影响.
- 渐进的过渡 (>几百万年) 沿着遗传的大陆石层弱区局部化应变,由粒径减小增强.
结论:
- 结构和热继承显著控制了潜伏启动位置.
- 这些发现与阿尔及利亚边缘和东日本海等自然例子一致.
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