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The Geology from the Upper Rennick Glacier to the Coast, Northern Victoria Land, Antarctica

 

作者: H. S. Gair,  

 

期刊: New Zealand Journal of Geology and Geophysics  (Taylor Available online 1967)
卷期: Volume 10, issue 2  

页码: 309-344

 

ISSN:0028-8306

 

年代: 1967

 

DOI:10.1080/00288306.1967.10426742

 

出版商: Taylor & Francis Group

 

数据来源: Taylor

 

摘要:

The Polar Plateau in this area is a rock surface thinly veneered with ice and lies at a height 8,000 to 11,000 ft above sea level. Three major groups of rocks are present: (1) Volcanics of late Tertiary and Quaternary age including kenyte and related rock types; (2) Volcanics (mostly basalt) of Triassic-Jurassic age with minor sediments; and (3) A basement complex consisting mostly of granite and gneissic granite digesting regional biotite schist of probable Precambrian age.

 

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