Processes in geophysics studied by Mossbauer spectroscopy

被引：1
作者：
Helgason, Ö [1 ]
机构：
[1] Univ Iceland, Inst Sci, IS-107 Reykjavik, Iceland
来源：
HYPERFINE INTERACTIONS | 2004年 / 156卷 / 01期
关键词：
Mossbauer spectroscopy; mantle-derived magma; oxidation state; rock magnetism; titanomagnetite; geothermal alteration;
D O I：
10.1023/B:HYPE.0000043257.28606.14
中图分类号：
O64 [物理化学（理论化学）、化学物理学]; O56 [分子物理学、原子物理学];
学科分类号：
070203 ; 070304 ; 081704 ; 1406 ;
摘要：
Mossbauer spectroscopy has been appreciated in geoscience as a powerful tool to study magnetic and structural properties of a wide range of minerals and rocks. In this presentation the application of Mossbauer spectroscopy in different geophysical processes such as tracing the development of magma during volcanic eruptions and phase transitions of magnetic minerals due to thermal impact of dikes in earlier lava formation or hydrothermal alteration will be discussed.
引用
收藏
页码：379 / 388
页数：10
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