Factors controlling the evolution of mineral assemblages and illite crystallinity in paleozoic to triassic sequences from the transition between maláguide and alpujárride complexes (betic cordillera, Spain): The significance of tobelite

Clays and Clay Minerals

Volumn 58, Issue 4, 2010, Pages 558-572

  Ruiz Cruz, M D ^a   Sanz de Galdeano, C ^b  

^a UNIVERSITY OF MÁLAGA   (Spain)

^b INSTITUTO ANDALUZ DE CIENCIAS DE LA TIERRA   (Spain)

Author keywords

Alpine metamorphism; Alpuj rride complex; Betic cordillera; Hercynian metamorphism; Mal guide complex; Tobelite; White k mica

Indexed keywords

ALPINE METAMORPHISM; BETIC CORDILLERA; HERCYNIAN METAMORPHISM; TOBELITE; WHITE K-MICA;

INFRARED SPECTROSCOPY; KAOLINITE; METAMORPHIC ROCKS; MICA; MINERALOGY; MINERALS; SCANNING ELECTRON MICROSCOPY; X RAY DIFFRACTION;

SILICATE MINERALS;

CRYSTALLINITY; GEOLOGICAL RECORD; HERCYNIAN OROGENY; ILLITE; LOW TEMPERATURE; METAMORPHIC ROCK; METAMORPHISM; MICA; PALEOZOIC; PARAGENESIS; TRIASSIC;

BETIC CORDILLERA; SPAIN;

EID: 78249266615     PISSN: 00098604     EISSN: None     Source Type: Journal    
DOI: 10.1346/CCMN.2010.0580410     Document Type: Article

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