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Reply to discussion of "A refined genetic model for the Laisvall and Vassbo Mississippi Valley-type sandstone-hosted deposits, Sweden: constraints from paragenetic studies, organic geochemistry, and S, C, N, and Sr isotope data" by D. Sangster

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Published in Mineralium Deposita. 2018, vol. 53, no. 2, p. 295-297
Abstract The very MVT definition includes ore deposits hosted in sandstone. Owing to the fact that the sandstone-hosted Pb-Zn deposits at Laisvall and Vassbo are epigenetic, formed by basinal brines long after deposition of the host rock, and this by the same mechanisms as those recognized in many carbonate-hosted MVT deposits, we maintain that using the term MVT is appropriate, useful, and has implications for the conceptualization of exploration models.
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Article (Published version) (350 Kb) - document accessible for UNIGE members only Limited access to UNIGE
Other version: http://link.springer.com/10.1007/s00126-017-0785-x
Structures
Research group Mineral Resources and Geofluids
Project FNS: 146353
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FONTBOTÉ, Lluis, SAINTILAN, Nicolas. Reply to discussion of "A refined genetic model for the Laisvall and Vassbo Mississippi Valley-type sandstone-hosted deposits, Sweden: constraints from paragenetic studies, organic geochemistry, and S, C, N, and Sr isotope data" by D. Sangster. In: Mineralium Deposita, 2018, vol. 53, n° 2, p. 295-297. https://archive-ouverte.unige.ch/unige:101049

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Deposited on : 2018-01-02

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