A Mossbauer effect study of Fe-site occupancy in Australasian tektites

被引：16

作者：

Dunlap, RA ^{[1
]}

Sibley, ADE

机构：

[1] Dalhousie Univ, Dept Phys & Atmospher Sci, Halifax, NS B3H 3J5, Canada

[2] Dalhousie Univ, Mat Res Inst, Halifax, NS B3H 3J5, Canada

来源：

JOURNAL OF NON-CRYSTALLINE SOLIDS | 2004年 / 337卷 / 01期

基金：

加拿大自然科学与工程研究理事会;

关键词：

D O I：

10.1016/j.jnoncrysol.2004.03.113

中图分类号：

TQ174 [陶瓷工业]; TB3 [工程材料学];

学科分类号：

0805 ; 080502 ;

摘要：

A number of different splash-form Australasian tektites and one Muong Nong tektite from Laos have been investigated by room temperature Fe-57 Mossbauer effect spectroscopy. Multiple spectra of thailandite samples have been obtained in order to establish uncertainties in fitted parameters. Results indicate that most of the samples investigated have Fe3+/Fe-2divided by ratios that are close to zero. The Muong Nong tektite shows the largest Fe3+/Fe-2divided by ratio and this is interpreted in terms of proposed mechanisms for the formation of this class of tektite that have been presented in the literature. (C) 2004 Elsevier B.V. All rights reserved.

引用

页码：36 / 41

页数：6

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