3-D velocity distribution of amphibolites collected from various crustal depths

IF 2.1 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
T. Lokajíček , R. Přikryl , A. Aminzadeh , T. Svitek , M. Petružálek
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引用次数: 0

Abstract

The elastic properties of nineteen samples of crystalline rocks – amphibolites from different areas/boreholes were studied in order to elucidate possible depth effect on the elastic properties of these mineralogically relatively homogenous rocks. The samples were taken from three different crustal levels – shallow (tens of meters) Stařechov (Czech Republic), medium (first thousands of meters) KTB (Germany), and extreme crustal depths (up to 12 km) KSDB3 (Russia). The elastic properties were first determined experimentally using a high-pressure apparatus allowing for multidirectional (3D) ultrasonic sounding at various levels of confining pressure. The effect of main rock fabric components was evaluated using the method of inverse calculation from experimental data. The observed increase of elastic wave velocity and elastic constants with depth could be explained by the stress memory effect.

不同地壳深度角闪岩的三维速度分布
研究了来自不同区域/钻孔的19个结晶岩-角闪岩样品的弹性特性,以阐明深度对这些矿物相对均质岩石弹性特性的可能影响。样本取自三个不同的地壳水平——浅层(几十米)的Stařechov(捷克共和国)、中等(最初几千米)的KTB(德国)和极端地壳深度(高达12公里)的KSDB3(俄罗斯)。弹性特性首先使用高压设备进行实验测定,该设备允许在不同围压水平下进行多向(3D)超声探测。采用实验数据反演的方法,对岩石主要组分的作用进行了评价。观察到的弹性波速和弹性常数随深度的增加可以用应力记忆效应来解释。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Journal of Geodynamics
Journal of Geodynamics 地学-地球化学与地球物理
CiteScore
4.60
自引率
0.00%
发文量
21
审稿时长
6-12 weeks
期刊介绍: The Journal of Geodynamics is an international and interdisciplinary forum for the publication of results and discussions of solid earth research in geodetic, geophysical, geological and geochemical geodynamics, with special emphasis on the large scale processes involved.
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