Granites of Edward VII Peninsula, Marie Byrd Land: anorogenic magmatism related to Antarctic-New Zealand rifting
Syenogranites and monzogranites of Edward VII Peninsula, Marie Byrd Land, represent magmatism associated with continental rifting and the separation of New Zealand from W Antarctica in the mid-Cretaceous. These coarse-grained, leucocratic, subsolvus biotite granites occur as five small plutons cutti...
Published in: | Earth and Environmental Science Transactions of the Royal Society of Edinburgh |
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Main Authors: | , , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Royal Society of Edinburgh
1992
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Subjects: | |
Online Access: | http://nora.nerc.ac.uk/id/eprint/519103/ https://doi.org/10.1017/S0263593300007963 |