Multi-stage metal enrichment and formation of gold mineralization in black shales: the role of high heat flow in a rift setting

0571422 - GLÚ 2024 RIV DE eng J - Článek v odborném periodiku
Pašava, J. - Ackerman, Lukáš - Žák, J. - Svojtka, Martin - Magna, T. - Pour, O. - Trubač, J. - Veselovský, F.
Multi-stage metal enrichment and formation of gold mineralization in black shales: the role of high heat flow in a rift setting.
Mineralium deposita. Roč. 58, č. 6 (2013), s. 1051-1073. ISSN 0026-4598. E-ISSN 1432-1866
Institucionální podpora: RVO:67985831
Klíčová slova: Cadomian orogeny * Gold mineralization * Black shale * Cambro–Ordovician rifting * Quartz hydrothermal veins * Polyphase deformation
Obor OECD: Geology
Impakt faktor: 2.667, rok: 2013
Způsob publikování: Open access
https://link.springer.com/article/10.1007/s00126-023-01169-9

Black shales may serve as an important source of metals such as Co, Ni, or As, largely due to anoxic to euxinic conditions in association with high concentrations of sulfur leading to efficient scavenging and transport of metals from seawater into the seafloor sediment. We report on an unusual type of Au mineralization newly discovered in Ediacaran trench-slope black shales in the Bohemian Massif, Czech Republic. The Au enrichment is related to the formation of a quartz–sulfide vein system and a progressive evolution of ore-forming fluids with decreasing temperature, from Sb- to As-rich to final precipitation of native gold from silica and Au-bearing low-temperature hydrothermal colloidal solutions. The hydrothermal nature of these solutions is also documented by Li contents and isotope compositions which differ markedly between barren black shales and those carrying significant late-stage quartz-rich veins. The structural relationships and orientation of the associated quartz veins point to a close connection between vein emplacement and high heat flow in response to Ordovician rifting, and breakup of the northern margin of Gondwana, and opening of the Rheic Ocean. This triggered metal and sulfur remobilization, including Au, from the associated Neoproterozoic–Cambrian volcanosedimentary successions. The documented Au mineralization and its association with the Ordovician rift-related magmatic activity is different from the widespread Variscan Au occurrences in the Bohemian Massif. Our study thus provides a new genetic model potentially important for future exploration of Au also in other terrains underlain by a rifted Cadomian basement.
Trvalý link: https://hdl.handle.net/11104/0344837