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

Journal of Metamorphic Geology

Volumn 13, Issue 2, 1995, Pages 141-164

  ARENAS, R ^a   PASCUAL, F J RUBIO ^a   GARCIA, F DIAZ ^b   CATALAN, J R MARTINEZ ^c  

^a UNIVERSIDAD COMPLUTENSE DE MADRID   (Spain)

^b UNIVERSITY OF OVIEDO   (Spain)

^c UNIVERSITY OF SALAMANCA   (Spain)

Author keywords

eo Hercynian metamorphism; high P evolution; NW Spain; Ordenes Complex; Santiago Schists

Indexed keywords

HERCYNIAN; INVERTED METAMORPHIC GRADIENT; ORDENES COMPLEX; SANTIAGO SCHIST; SUBDUCTION; TECTONOTHERMAL EVOLUTION;

SPAIN, IBERIAN MASSIF;

EID: 0028852220     PISSN: 02634929     EISSN: 15251314     Source Type: Journal    
DOI: 10.1111/j.1525-1314.1995.tb00211.x     Document Type: Article

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