概括
在低压下,岩石变形而没有不稳定. 然而,在高压 (7-10千巴) 下,某些岩石表现出不稳定的断层,这可能解释了深度地震.
科学领域:
- 地质物理学 地质物理学
- 岩石机械学 岩石机械学
- 地震学 地震学
背景情况:
- 沉积物,改变的岩石,多孔的火山岩石和沙子通常在低限压下柔性地变形.
- 柔性变形的特点是没有像可听的弹性冲击这样的不稳定性.
研究的目的:
- 为了研究各种岩石类型在高限制压力下的变形行为.
- 为了确定高压条件是否可以诱导不稳定的断裂和粘滑行为.
主要方法:
- 岩石样本在从几千巴到7-10千巴的限制压力下进行实验变形.
- 观察变形模式,重点关注不稳定的存在或不存在.
主要成果:
- 在低限压下,在所有测试的岩石类型中,变形是可变的.
- 在7到10千巴的压力下,在特定的岩石样本中观察到不稳定的断层和粘滑行为.
- 这种从柔性转变为不稳定的变形是压力依赖的.
结论:
- 高限压可以诱导脆性失效机制,如不稳定的断层,在岩石中,在较低的压力下柔性变形.
- 这种高压,低温的不稳定性可能是地震发生在深埋的地质形成的关键机制.
- 了解这些依赖压力的转变对于深层地环境的地震危险评估至关重要.
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