在北美底部重建法拉龙板沉降,追溯到白纪晚期
Lijun Liu1, Sonja Spasojevic, Michael Gurnis
1Seismological Laboratory, California Institute of Technology, Pasadena, CA 91125, USA. lijun@gps.caltech.edu
概括
研究人员使用地幔对流模型重建了法拉隆板块沉降. 证实了白纪晚期的平面沉降,揭示了延伸1000公里的更广的浅沉沉沉降区域.
科学领域:
- 地质物理学 地质物理学
- 板块构造学是一种板块构造学.
- 地幔动力学地幔动力学
背景情况:
- 了解过去的构造事件对于解释地球的动态过程至关重要.
- 法拉隆板块的沉降历史极大地影响了北美地质学.
- 之前的模型缺乏关于板块几何和地幔特性的详细约束.
研究的目的:
- 为了重建法拉隆板块的沉降历史,追溯到1亿年前.
- 使用地震数据和板块运动来限制地幔粘度和浮力.
- 为了研究平面俯冲的机制和程度.
主要方法:
- 利用了一个反向地幔对流模型.
- 同化地震结构和板块运动数据.
- 使用地质层级学的受限模型.
主要成果:
- 重建了法拉隆板块的沉降,证实了白纪晚期的一块平躺板块.
- 该模型表明浅沉沉沉积延伸到1000公里以外的平板板块.
- 海洋高原的沉降被认为是板块平整的原因.
结论:
- 地幔的地震图像为过去的构造事件提供了强大的约束.
- 费拉伦板块的潜水几何结构已经得到了改进.
- 地幔对流模型提供了对板块构造学和板块行为的动态的见解.
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