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
- ARENAS, R.
- PASCUAL, F.J.R.
- GARCIA, F.D.
- CATALAN, J.R.M.
ISSN: 1525-1314, 0263-4929
Year of publication: 1995
Volume: 13
Issue: 2
Pages: 141-164
Type: Article