短暂的orogenic周期和冷地的生态化由性热流体的生态化
Alfredo Camacho1, James K W Lee, Bastiaan J Hensen
1Geological Sciences and Geological Engineering, Queen's University, Kingston, Ontario K7L 3N6, Canada.
Nature
|July 1, 2005
概括
碰撞构造学迅速将大陆地转化为像生态岩石这样的高压岩石. 新的数据显示,变态事件发生在数千年内,热脉冲持续数十年,挑战现有的热模型.
科学领域:
- 地质地质地质地质地质地
- 构造学 构造学 构造学 构造学
- 变态石器学 变态石器学
背景情况:
- 碰撞构造学将大陆地转化为高压岩石 (生态岩石).
- 现有的地质热模型与这些岩石的岩石学同位素数据相冲突.
- 矛盾来自于厚化地的热平衡假设.
研究的目的:
- 为了协调构热模型与岩石学同位素数据之间的差异.
- 为了限制orogenic周期和相关的变形事件的持续时间.
- 开发一个非稳定状态模型,用于碰撞期间地的演变.
主要方法:
- 利用了40Ar-39Ar的地球时间学.
- 采用了热模拟技术.
- 综合地质年代数据与热模型来分析变态时间尺度.
主要成果:
- 被限制在<13 Myr 持续时间的产卵周期.
- 改变形状的事件被确定为 ~20 kyr.
- 个体热脉冲被确定为最短的10年.
- 有证据表明,在剪切区域沿着热流体通过快速的构造过程和短暂的热传递.
结论:
- 短的时间表表明了快速的构造过程,可能与地震事件有关.
- 剪切区中热流体的短暂热量转移解释了快速升温的原因.
- 非平衡状态的冷地模型比平衡模型更好地解释地质观测.
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