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Oxygen and carbon isotope composition of Gordon Group carbonates (Ordovician), Florentine Valley, Tasmania, Australia

 

作者: C.Prasada Rao,   B. Wang,  

 

期刊: Australian Journal of Earth Sciences  （Taylor Available online 1990）
卷期: Volume 37, issue 3  

页码: 305-316

 

ISSN:0812-0099

 

年代: 1990

 

DOI:10.1080/08120099008727929

 

出版商: Taylor & Francis Group

 

关键词: dolomite;Gordon Group;Ordovician carbonates;oxygen and carbon isotopes;Tasmania

 

数据来源: Taylor

 

摘要:

The Gordon Group carbonates consist of biota of the Chlorozoan assemblage, diverse non‐skeletal grains and abundant micrite and dolomite, similar to those of modern warm water carbonates. Cathodoluminescence studies indicate marine, meteoric and some burial cements. Dolomites replacing burrows, mudcracks and micrite formed during early diagenesis.

 

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