相关实验视频
Updated: Jul 12, 2026

08:43
Calibration Procedures for Orthogonal Superposition Rheology
Published on: November 18, 2020
概括
地球上层地幔使用两种主要的流动机制:在热,浅的地区出现脱位爬行,在更冷或更深的地区出现扩散爬行. 这些流转会影响地幔动力学和岩石变形.
科学领域:
- 地质物理学 地质物理学
- 地质地质地质地质地质地
- 类风病学 类风病学 类风病学
背景情况:
- 地球上层地幔的浮力学特性对于理解石层和天层动态至关重要.
- 然而,控制地幔流动的主要机制仍然不完全理解.
研究的目的:
- 为了研究地球上层地幔中占主导地位的流动机制.
- 综合实验室数据与地质物理和地质观测,以解决地幔动态的基本问题.
主要方法:
- 基于实验室的风湿学研究的综合.
- 分析与地幔结构和动态相关的地球物理观测.
- 整合地质证据来推断过去的地幔行为.
主要成果:
- 有证据表明,在上层地幔中,扩散爬行和脱位爬行之间的过渡发生.
- 热,浅的上层地幔主要通过位爬行流动.
- 寒冷,浅或深的上层地幔可能会表现出扩散爬行.
结论:
- 增加的压力导致粒径减少,使地幔在爬行模式过渡附近变弱.
- 这种减弱导致局部变形和在特定深度上层地幔的机械解.
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