Abstract:<p>Breccia structure is a ubiquitous feature that is characterized by angular fragment in a matrix composed of smaller grain size, often associated to brittle tectonics or to specific sedimentary environment such as karst collapse. Many different studies across the world describe breccia related to dolomite geobodies, themselves associated to ore deposits occurring during major extensional events (Hungary, Spain, France, Canada, Poland, Canada). The mineralogical textures of these structures, i.e… Show more
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