Fault zone structure and fluid–rock interaction of a high angle normal fault in Carrara marble (NW Tuscany, Italy)
- 30 September 2010
- journal article
- Published by Elsevier BV in Journal of Structural Geology
- Vol. 32 (9), 1334-1348
- https://doi.org/10.1016/j.jsg.2009.04.021
Abstract
No abstract availableKeywords
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