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The mountain building process witnessed today at the Andes is a good modern example of oceanic-continental convergence, providing a modern-day analogue that can be used to interpret older converging mountain belts around the world. Paniri (22°03'34”S, 68°13'42”W) a Pleistocene age stratovolcano and...
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| Language: | English English |
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Department of Geological Sciences
2025
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