Mélange within subduction–accretion complex rocks of Fredriksen Island, South Orkney Islands

Summary . A m´lange on Fredriksen Island, South Orkney Islands, is part of a Mesozoic subduction- accretion complex which formed along the western, Pacific side of Gondwana. It consists of a chaotic arrangement of irregular sized blocks, up to 8 m across, of basic pillow lava, chert, felsite and epi...

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Bibliographic Details
Published in:Geological Magazine
Main Authors: Storey, B. C., Meneilly, A. W.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1983
Subjects:
Online Access:http://dx.doi.org/10.1017/s0016756800027710
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800027710