Joint geophysical and petrological models for the lithosphere structure of the Antarctic Peninsula continental margin
The Antarctic Peninsula (AP) is a composite magmatic arc terrane formed at the Pacific margin of Gondwana. Through the late Mesozoic and Cenozoic subduction has stopped progressively from southwest to northeast as a result of a series of ridge trench collisions. Subduction may be active today in the...
Published in: | Geophysical Journal International |
---|---|
Main Authors: | , , , |
Format: | Text |
Language: | English |
Published: |
Oxford University Press
2011
|
Subjects: | |
Online Access: | http://gji.oxfordjournals.org/cgi/content/short/184/1/90 https://doi.org/10.1111/j.1365-246X.2010.04867.x |