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Big Bend Megafold or Broken River Triple Junction?

 

作者: H. J. Harrington,  

 

期刊: Journal of the Geological Society of Australia  （Taylor Available online 1981）
卷期: Volume 28, issue 3-4  

页码: 501-502

 

ISSN:0016-7614

 

年代: 1981

 

DOI:10.1080/00167618108729184

 

出版商: Taylor & Francis Group

 

数据来源: Taylor

 

摘要:

The Broken River Embayment is a major transverse structure in the Tasman Orogen in northern Queensland. Bell (1980) suggested that it is a hinge zone of an orocline, which he named the Big Bend Megafold. An alternative explanation, presented in this paper, involves a Silurian‐Devonian triple plate junction.

 

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