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