在实验室中在高压和高温下记录的深焦地震类比
Alexandre Schubnel1, Fabrice Brunet, Nadège Hilairet
1Laboratoire de Géologie, CNRS UMR 8538, Ecole Normale Supérieure, 75005 Paris, France. aschubnel@geologie.ens.fr
概括
奥利文的相位转换可以触发深度焦点地震. 实验室实验表明,在橄石转变为尖石的过程中,骨折会产生模仿自然地震的地震信号.
科学领域:
- 地质物理学 地质物理学
- 矿物物理 矿物物理
背景情况:
- 深度焦点地震起源于400-700公里的深度,位于地下石化层内.
- 转移稳定的奥利文相变化是这些地震事件的假设触发因素.
研究的目的:
- 调查橄酸相转换作为深焦地震机制的可行性.
- 用实验来模拟与压板相关的条件.
主要方法:
- 实验室的变形实验是在橄 (Mg2GeO4) 上进行的.
- 实验是在高压 (2-5 GPa) 和特定温度 (1000-1250 K) 下进行的.
- 应用了差应力来诱导相变和变形.
主要成果:
- 在olivine-to-spinel过渡开始时观察到骨折核.
- 动态传播的断裂产生了强烈的声学辐射.
- 声学辐射表现出纯剪切源的特征,并遵循古登堡-里希特定律,类似于深度焦点地震.
结论:
- 从橄石转变为脊柱石,可以产生与深度焦点地震一致的地震信号.
- 动态减弱,可能涉及纳米晶体螺旋的超塑性,可能会在高应变速率下促进这些地震事件.
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