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

1995 ◽  
Vol 13 (2) ◽  
pp. 141-164 ◽  
Author(s):  
R. ARENAS ◽  
F. J. RUBIO PASCUAL ◽  
F. DIAZ GARCIA ◽  
J. R. MARTINEZ CATALAN
Keyword(s):  
High Pressure ◽  
Iberian Massif ◽  
Metamorphic Gradient

Comment on “The Late Devonian Variscan suture of the Iberian Massif: A correlation of high-pressure belts in NW and SW Iberia. Tectonophysics 654, 96–100" by R. Fernández and R. Arenas

2016 ◽  
Vol 666 ◽  
pp. 281-284 ◽  
Author(s):  
J.F. Simancas ◽  
A. Azor ◽  
D.J. Martínez Poyatos ◽  
I. Expósito ◽  
I. Pérez-Cáceres ◽  
...  
Keyword(s):  
High Pressure ◽  
Late Devonian ◽  
Iberian Massif

Graphitization in a high-pressure, low-temperature metamorphic gradient: a Raman microspectroscopy and HRTEM study

2002 ◽  
Vol 143 (1) ◽  
pp. 19-31 ◽  
Author(s):  
Olivier Beyssac ◽  
Jean-Noël Rouzaud ◽  
Bruno Goffé ◽  
Fabrice Brunet ◽  
Christian Chopin
Keyword(s):  
High Pressure ◽  
Low Temperature ◽  
Raman Microspectroscopy ◽  
Metamorphic Gradient

High-pressure metamorphism in the Early Variscan subduction complex of the SW Iberian Massif

2013 ◽  
Vol 592 ◽  
pp. 187-199 ◽  
Author(s):  
Francisco J. Rubio Pascual ◽  
Jerónimo Matas ◽  
Luis M. Martín Parra
Keyword(s):  
High Pressure ◽  
Iberian Massif ◽  
High Pressure Metamorphism
Sign in / Sign up

Export Citation Format

Share Document