Hostname: page-component-586b7cd67f-2plfb Total loading time: 0 Render date: 2024-11-26T01:56:42.962Z Has data issue: false hasContentIssue false

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

Published online by Cambridge University Press:  14 May 2004

P.A.R. Nell
Affiliation:
British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge CB3 0ET, UK
B.K. Kamenov
Affiliation:
Sofia University ‘Kliment Ochridsky’, 1000 Sofia, 15 Russky Bd, Bulgaria
C.T. Pimpirev
Affiliation:
Sofia University ‘Kliment Ochridsky’, 1000 Sofia, 15 Russky Bd, Bulgaria

Extract

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.

Type
Short notes
Copyright
© Antarctic Science Ltd 1989

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)