Li Cunyou, Shi Lida. THE REASON AND EXPLORING SIGNIFICANCE OF α β PEAK OF QUARTZ IN DECREPITATION TEST[J]. Geology and Resources, 1999, 8(1): 35-37. DOI: 10.13686/j.cnki.dzyzy.1999.01.007

Citation:

Li Cunyou, Shi Lida. THE REASON AND EXPLORING SIGNIFICANCE OF α β PEAK OF QUARTZ IN DECREPITATION TEST[J]. Geology and Resources, 1999, 8(1): 35-37. DOI: 10.13686/j.cnki.dzyzy.1999.01.007

Li Cunyou, Shi Lida. THE REASON AND EXPLORING SIGNIFICANCE OF α β PEAK OF QUARTZ IN DECREPITATION TEST[J]. Geology and Resources, 1999, 8(1): 35-37. DOI: 10.13686/j.cnki.dzyzy.1999.01.007

Citation:

Li Cunyou, Shi Lida. THE REASON AND EXPLORING SIGNIFICANCE OF α β PEAK OF QUARTZ IN DECREPITATION TEST[J]. Geology and Resources, 1999, 8(1): 35-37. DOI: 10.13686/j.cnki.dzyzy.1999.01.007

THE REASON AND EXPLORING SIGNIFICANCE OF α β PEAK OF QUARTZ IN DECREPITATION TEST

Li Cunyou,
Shi Lida

Graphical Abstract

Graphical Abstract

Abstract

In decrepitation test for quartz,α-β peaks frequently appear when the samples are heated to the temperature of 573℃.Study shows that the α-β peak is produced by the leaking(without decrepitating) of high temperature inclusions whose decrepitating temperature is higher than 573℃,the critical point when α quartz converts into β quartz This form of peak may be used to infer the denuded degree of lodes and decide the origin of deposits in gold ore exploring

FullText(HTML)

Related Articles

Turn off MathJax

Article Contents

/

DownLoad: Full-Size Img PowerPoint

Return