High‐pressure micro‐inclusions and development of an inverted metamorphic gradient in the Santiago Schists (Ordenes Complex, NW Iberian Massif, Spain): evidence of subduction and syncollisional decompression
- 1 March 1995
- journal article
- Published by Wiley in Journal of Metamorphic Geology
- Vol. 13 (2), 141-164
- https://doi.org/10.1111/j.1525-1314.1995.tb00211.x
Abstract
No abstract availableKeywords
This publication has 60 references indexed in Scilit:
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