Hot dolomites in a Variscan foreland belt: Hydrothermal flow in the Cantabrian Zone (NW Spain)

Journal of Geochemical Exploration

Volumn 78-79, Issue , 2003, Pages 501-507

  Gasparrini, M ^a   Bakker, R J ^b   Bechstadt Th ^a   Boni, M ^c  

^a UNIVERSITY OF HEIDELBERG   (Germany)

^b UNIVERSITY OF LEOBEN   (Austria)

^c UNIVERSITY OF NAPLES FEDERICO II   (Italy)

Author keywords

Dolomite; Fluid flow; Hydrothermal; Northern spain

Indexed keywords

CATHODOLUMINESCENCE; FLOW OF FLUIDS; ISOTOPES; PETROGRAPHY; RAMAN SPECTROSCOPY; TECTONICS; X RAY DIFFRACTION ANALYSIS;

DOLOMITES; FLUID INCLUSION MICROTHERMOMETRY; HYDROTHERMAL FLOW; PALAEOZOIC SEDIMENTS;

SEDIMENTS;

BASEMENT ROCK; CARBONATE; DIAGENESIS; DOLOMITE; DOLOMITIZATION; EXTENSIONAL TECTONICS; FLUID FLOW; FLUID INCLUSION; FORELAND BASIN; HERCYNIAN OROGENY; HIGH TEMPERATURE; HOST ROCK; HYDROTHERMAL ACTIVITY; HYDROTHERMAL FLUID; LIMESTONE; LINEAMENT; TECTONIC STRUCTURE;

CANTABRIAN MOUNTAINS; CENTRAL AMERICA; EURASIA; EUROPE; IBERIAN MASSIF; IBERIAN PENINSULA; LEON; NICARAGUA; SOUTHERN EUROPE; SPAIN;

EID: 33748310172     PISSN: 03756742     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0375-6742(03)00115-8     Document Type: Conference Paper

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