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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