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...

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Bibliographic Details
Main Authors: Millar, I.L., Willan, R.C.R., Wareham, C.D., Boyce, A.J.
Format: Article in Journal/Newspaper
Language:English
Published: Geological Society 2001
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?