Field report on combined Anglo–Bulgarian geological studies in northern Alexander Island

The structural basement of Alexander Island consists of a wide belt of accretionary complex rocks, the LeMay Group (Bum 1984). This is overlain by ?Cretaceous-Tertiary calcalkalinevolcanic rocks (Bum 1981), and intruded by several slightly younger, but related, plutons (Care 1983). The Rouen Mountai...

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Bibliographic Details
Published in:Antarctic Science
Main Authors: Nell, P.A.R., Kamenov, B.K., Pimpirev, C.T.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1989
Subjects:
Alexander Island
Antarctic Science
Online Access:http://dx.doi.org/10.1017/s0954102089000258
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0954102089000258
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Summary:The structural basement of Alexander Island consists of a wide belt of accretionary complex rocks, the LeMay Group (Bum 1984). This is overlain by ?Cretaceous-Tertiary calcalkalinevolcanic rocks (Bum 1981), and intruded by several slightly younger, but related, plutons (Care 1983). The Rouen Mountains batholith is a large group of these plutons which occurs in the northern part of the island.

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