Evidence for Paleocene–Eocene evolution of the foot of the...

Evidence for Paleocene–Eocene evolution of the foot of the Eurasian margin (Kermanshah ophiolite, SW Iran) from back-arc to arc: Implications for regional geodynamics and obduction

Whitechurch, H., Omrani, J., Agard, P., Humbert, F., Montigny, R., Jolivet, L.
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Volume:
182-183
Language:
english
Journal:
Lithos
DOI:
10.1016/j.lithos.2013.07.017
Date:
December, 2013
File:
PDF, 4.28 MB
english, 2013
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