The role of crustal and mantle sources in the genesis of granitoids of the Antarctic Peninsula and adjacent crustal blocks
Magmatic rocks from the Antarctic Peninsula show marked variations in isotope composition, which reflect changes in the geodynamic evolution of the peninsula through time. Most Antarctic Peninsula granitoids formed as a result of subduction: they fall on well-defined trends on plots of Nd, Pb-207/Pb...
Main Authors: | , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Geological Society
2001
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Subjects: | |
Online Access: | https://eprints.gla.ac.uk/603/ https://eprints.gla.ac.uk/603/1/Journ_Geol_Soc_158%285%29_855-867.pdf http://www.ingentaconnect.com/content/geol/jgs;jsessionid=2c0c3b2lngepy.henrietta? |