Breakdown mechanisms of titanclinohumite in antigorite serpentinite (Cerro del Almirez massif, S. Spain): A petrological and TEM study

Lithos

Volumn 107, Issue 3-4, 2009, Pages 216-226

  López Sánchez Vizcaíno, Vicente ^a   Gómez Pugnaire, María Teresa ^b,c   Garrido, Carlos J ^c   Padrón Navarta, José Alberto ^b   Mellini, Marcello ^d  

^a UNIVERSITY OF JAÉN   (Spain)

^b UNIVERSITY OF GRANADA   (Spain)

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

^d UNIVERSITY OF SIENA   (Italy)

Author keywords

Antigorite serpentinite; Breakdown; Dehydration; Titanclinohumite; Vein

Indexed keywords

ANTIGORITE; BRUCITE; CLINOHUMITE; DIOPSIDE; FORMATION MECHANISM; HYDRATION; P-T CONDITIONS; PHASE TRANSITION; SERPENTINITE; SUBDUCTION ZONE; TECTONIC SETTING; TITANIUM; TRANSMISSION ELECTRON MICROSCOPY; VEIN (GEOLOGY);

ANDALUCIA; BETIC CORDILLERA; EURASIA; EUROPE; SIERRA NEVADA [BETIC CORDILLERA]; SOUTHERN EUROPE; SPAIN;

EID: 58549112201     PISSN: 00244937     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.lithos.2008.10.008     Document Type: Article

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