Fault zone structure and fluid-rock interaction of a high angle normal fault in the Carrara marble (NW Tuscany, Italy);Caratteri strutturali e interazione fluido-roccia in una faglia normale ad alto angolo nei marmi di Carrara

Rendiconti Online Societa Geologica Italiana

Volumn 5, Issue , 2009, Pages 142-143

  Molli, Giancarlo ^a   Cortecci, Gianni ^b   Vaselli, Luca ^b   Ottria, Giuseppe ^b  

^a UNIVERSITY OF PISA   (Italy)

^b CNR   (Italy)

Author keywords

Brittle faulting; Calcite microstructures; Carrara marble; Cataclasite; Geochemistry

Indexed keywords

EID: 84863494585     PISSN: 20358008     EISSN: None     Source Type: Journal    
DOI: None     Document Type: Conference Paper

References (4)

1. CARMIGNANI L. & KLIGFIELD R. (1990) - Crustal extension in the Northern Apennines: The transition from compression to extension in the Alpi Apuane. Tectonics, 9, 1275-1303.
2. MOLLI G. (2008) - Northern Apennine-Corsica orogenic system: an updated overview. In: Siegesmund, S., Fugenschuh B., Froitzheim, N. (Eds). Geological Society of London, Special Pubblications, 298, 413-442.
3. MOLLI G., CORTECCI G., VASELLI L., OTTRIA G., G. B., CORTOPASSI A., DINELLI E., BARBIERI M. & MUSSI M. (2009) - Fault zone structure and fluid-rock interaction of a high angle normal fault. Journal of Structural Geology, in stampa.
4. OTTRIA G. & MOLLI G. (2000) - Superimposed brittle structures in the late orogenic extension of the Northern Apennine. Results from Carrara area (NW Tuscany, Italy) Terra Nova 12(2), 52-59.