Mossbauer spectroscopy of magnetic minerals in basalt on Earth and Mars

被引：10

作者：

Gunnlaugsson, H. P. ^{[1
]}

Rasmussen, H. ^{[2
]}

Kristjansson, L. ^{[3
]}

Steinthorsson, S. ^{[3
]}

Helgason, O. ^{[3
]}

Nornberg, P. ^{[2
]}

Madsen, M. B. ^{[4
]}

Morup, S. ^{[5
]}

机构：

[1] Aarhus Univ, Dept Phys & Astron, DK-8000 Aarhus C, Denmark

[2] Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark

[3] Univ Iceland, Inst Sci, IS-107 Reykjavik, Iceland

[4] Univ Copenhagen, Niels Bohr Inst, DK-2100 Copenhagen O, Denmark

[5] Tech Univ Denmark, Dept Phys, DK-2800 Lyngby, Denmark

来源：

HYPERFINE INTERACTIONS | 2008年 / 182卷 / 1-3期

关键词：

Basalt; Mossbauer spectroscopy; Titanomaghemite;

D O I：

10.1007/s10751-008-9714-9

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 of iron-titanium containing spinel phases is reviewed. New techniques are presented for determination of their composition using room-temperature Mossbauer spectroscopy. An example of thermal alteration processes is described. The speciality of olivine-containing basalt is briefly discussed with regard to its magnetic properties.

引用

页码：87 / 101

页数：15

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