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表面侵蚀事件控制了地球上板块构造的演变
Stephan V Sobolev1,2, Michael Brown3
1GFZ German Research Centre for Geosciences, Section of Geodynamic Modeling, Potsdam, Germany. stephan@gfz-potsdam.de.
Nature
|June 7, 2019
概括
板块构造随着大陆的增长和沉积而演变,这滑了沉积区. 随着全球冰川的出现,主要的构造事件推动了超大陆的形成和现代板块活动.
科学领域:
- 地质学
- 地球科学
- 构造学
背景情况:
- 板块构造是地球的一个基本过程,但它的起源和演变尚未完全理解.
- 了解板块构造的发展是理解地球地质历史的关键.
研究的目的:
- 调查地球上板块构造的出现和演变.
- 提出由大陆和沉积物学变化驱动的板块构造学的发展模型.
主要方法:
- 当今板块构造模型的推断到过去的地质时期.
- 分析大陆上升和沉积物在潜水滑中的作用.
主要成果:
- 自30亿年前以来,大陆的增长和沉积物可能为沉积提供了滑,这对板块构造至关重要.
- 在休伦和雪球地球冰期之后发生了显著的表面侵蚀和滑事件,影响了超级大陆的形成 (例如,哥伦比亚).
结论:
- "无聊的十亿"时期的减少构造活动可能是沟沉积物短缺的结果.
- 新生代"雪球"地球冰期被认为重新启动了活跃的板块构造.
- 沉积和侵蚀动态是板块构造学长期演变的关键因素.
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