Neogene Patagonian plateau lavas: Continental magmas associated with ridge collision at the Chile Triple Junction
Extensive Neogene Patagonian plateau lavas (46.5° to 49.5°S) southeast of the modern Chile Triple Junction can be related to opening of asthenospheric “slab windows” associated with collisions of Chile Rise segments with the Chile Trench at ≈ 12 Ma and 6 Ma. Support comes from 26 new total‐fusion, w...
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Published in: | Tectonics (Washington, D.C.) Vol. 16; no. 1; pp. 1 - 17 |
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Main Authors: | , , , , , , |
Format: | Journal Article |
Language: | English |
Published: |
Blackwell Publishing Ltd
01-02-1997
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Subjects: | |
Online Access: | Get full text |
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