金伯利特喷发是由板块流动和俯冲角度驱动的
Ben R Mather1, R Dietmar Müller2, Christopher P Alfonso2
1EarthByte Group, School of Geosciences, The University of Sydney, Sydney, 2006, Australia. ben.mather@sydney.edu.au.
Scientific reports
|June 6, 2023
概括
潜伏角度,而不仅仅是地幔羽毛,解释了金伯利特喷发. 这种新模型将板块动态与含有钻石的岩浮出水面联系起来,统一了喷发时间理论.
科学领域:
- 地质地质地质地质地质地
- 地质物理学 地质物理学
- 石化学 石化学是一门学科.
背景情况:
- 金伯石是钻石的主要来源,从地幔上游喷发出来.
- 之前的喷发时间模型 (板块速度,地幔羽毛) 并不能完全解释白纪金伯利特的俯冲特征.
研究的目的:
- 为了研究一个统一的俯冲过程,解释kimberlite喷发的时间.
- 开发一种新的配方来计算潜水角度及其与金伯石置位的联系.
主要方法:
- 使用沟迁移,收率,板块厚度和密度计算俯冲角度的制定.
- 计算的俯冲角和板块流量峰与金伯利特喷发脉冲的相关性.
主要成果:
- 引角度与板块流量峰相结合,可以准确预测金伯利特喷发脉冲.
- 较高的降温率刺激地幔回流,激活肥沃的水库.
- 较弱影响的融被运送到表面,喷发位置与潜水角度相关.
结论:
- 俯冲动态为了解金伯石喷发时间提供了一个统一的机制.
- 深度时间板块浸泡的配方对模拟地球深层循环和矿产沉积物形成有影响.
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