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The origin of tin deposits in the Mount Wells region, Pine Creek Geosyncline, Northern Territory

 

作者: M. Ahmad,  

 

期刊: Australian Journal of Earth Sciences  （Taylor Available online 1993）
卷期: Volume 40, issue 5  

页码: 427-443

 

ISSN:0812-0099

 

年代: 1993

 

DOI:10.1080/08120099308728094

 

出版商: Taylor & Francis Group

 

关键词: fluid inclusions;mineralogy;paragenesis;stable isotopes;tin deposits

 

数据来源: Taylor

 

摘要:

Tabular steeply dipping cassiterite‐bearing lodes in the Mount Wells region are hosted by lower greenschist fades metasediment of the Pine Creek Geosyncline within the contact aureole of late orogenic granitoids. The latter are predominantly I‐type, but S‐type phases are developed near the sediment‐granitoid contact.

 

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