Fluid flow vs. scale of shear zones in the lower continental crust and the granulite paradox

Geology

Volumn 25, Issue 1, 1997, Pages 15-18

  Pili, Eric ^a   Sheppard, Simon M F ^a   Lardeaux, Jean Marc ^b   Martelat, Jean Emmanuel ^c   Nicollet, Christian ^c  

^a UNIVERSITÉ DE LYON   (France)

^b UNIVERSITÉ LYON 1   (France)

^c UNIVERSITÉ CLERMONT AUVERGNE   (France)

Author keywords

[No Author keywords available]

Indexed keywords

CARBON; FLOW OF FLUIDS; ISOTOPES; MARBLE;

CONTINENTAL CRUSTS; DEVOLATILIZATION; HETEROGENEOUS DEFORMATION; HETEROGENEOUS DISTRIBUTIONS; ISOTOPIC COMPOSITION; ISOTOPIC VARIATIONS; STRUCTURAL RELATIONSHIP; STRUCTURAL SETTING; CRUSTAL SOURCES;

SHEAR FLOW;

CONTINENTAL CRUST; FLUID FLOW; GRANULITE; MARBLE; METABASITE; PETROLOGY; PROTOLITH; SHEAR ZONE; CARBON DIOXIDE; PETROGENESIS;

EID: 0030857262     PISSN: 00917613     EISSN: None     Source Type: Journal    
DOI: 10.1130/0091-7613(1997)025<0015:FFVSOS>2.3.CO;2     Document Type: Article

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