Mississippi Valley-type sulfide mineralization and relationships to carbonate diagenesis: Introductory remarks

Mazzullo, S. J.; Gregg, Jay M.

doi:10.1007/bf03175103

Cited by 5 publications

(5 citation statements)

References 18 publications

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“…Recent studies on typical MVT ore deposits of North America give evidence for an intimate relation of shallow depth ore emplacement by saline basinal fluids to be derived from adjoining dewatering basins (Sverjenski, 1986;Mazzullo and Gregg, 1989;Gregg and Shelton, 1989).…”

Section: Resultsmentioning

confidence: 99%

“…(2) Diagenetic-epigenetic Fe, Zn, Pb ore deposits hosted in carbonate rocks (Beishan) originated by the interplay of dic Gregg and Shelton (1989) agenetic compaction fluids and thermal brines from adjacent basins (Garven, 1985;Mazzullo and Gregg, 1989).…”

Section: Diagenetic and Hydrothermal History And Processesmentioning

confidence: 99%

“…(3) Epigenetic Fe, Zn, Pb ore deposits hosted mainly in dolomites and reefs (Siding) and related to saline basinal brines (Garven, 1985;Mazzullo and Gregg, 1989).…”

Section: Diagenetic and Hydrothermal History And Processesmentioning

confidence: 99%

“…Stratigraphic, tectonic, diagenetic, mineralogic and geochemical studies (Unpubl, Reports) have led to the conclusion that the SidingGudan lead-zinc mineralizations represent carbonate hosted, hydrothermal, strata-bound ore deposits similar to classic MVT sulfide mineral deposits (e.g. Anderson, 1975;Anderson and Macqueen, 1982;Sverjensky, 1986;Mazzullo and Gregg, 1989;and Gregg and Shelton, J989). Wu et al .. 1987).…”

Section: Introductionmentioning

confidence: 99%

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Diagenesis and mineralization processes in Devonian carbonate rocks of the Siding-Gudan lead-zinc mineral subdistrict, Guangxi, Southwest China

Schneider

Geng

Xiaozeng

1991

Carbonates Evaporites

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The lead-zinc ore deposits of the Siding-Gudan mineral subdistrict Guangxi are part of the large Nanling district of South China, and hosted in Devonian carbonate rocks. The ore bodies occur significantly along main faults and fault zones, and concentrate up to 300 meters above the Cambrian/Devonian unconformity. Connected with hydrothermal karst, size and volume of the ore bodies increase in proximity to this unconformity.Moving from the unaffected host rocks to the center of the ore bodies, four zones can be discriminated by the mineral assemblage (pyrite. sphalerite. galena) as well as by the degree of ordering. Ca/Mg, and Fe/Mn ratios of different dolomites. Homogenization temperatures range from 80-100°C (Presqu'Ile dolomite) to 230-260°C (massive sphalerite). The sulfides reveal

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Section: Resultsmentioning

confidence: 99%

Section: Diagenetic and Hydrothermal History And Processesmentioning

confidence: 99%

“…(3) Epigenetic Fe, Zn, Pb ore deposits hosted mainly in dolomites and reefs (Siding) and related to saline basinal brines (Garven, 1985;Mazzullo and Gregg, 1989).…”

Section: Diagenetic and Hydrothermal History And Processesmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

See 2 more Smart Citations

Diagenesis and mineralization processes in Devonian carbonate rocks of the Siding-Gudan lead-zinc mineral subdistrict, Guangxi, Southwest China

Schneider

Geng

Xiaozeng

1991

Carbonates Evaporites

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“…manganese mineralizations (Maynard 1990 Mazzullo and Gregg 1989;Cemy 1989;Bechstädt and Boni 1994;Zeeh et al 1995;Dejonghe 1998;Sass-Gustkiewicz and Dzulynski.1999;Zeeh et al 1999;Liaghat et al 2000). manganese mineralizations (Maynard 1990 Mazzullo and Gregg 1989;Cemy 1989;Bechstädt and Boni 1994;Zeeh et al 1995;Dejonghe 1998;Sass-Gustkiewicz and Dzulynski.1999;Zeeh et al 1999;Liaghat et al 2000).…”

Section: Ore Depositsand Carbonate Settingsmentioning

confidence: 99%

Reservoir Rocks and Host Rocks

Flügel

2004

Microfacies of Carbonate Rocks

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The third part of the book provides insights into applied aspects of microfacies studies. Chapter 17 considers the role of microfacies in reservoir rock analyses of hydrocarbon reservoirs and carbonate-hosted base metal deposits. Chapter 18 deals with carbonate resources and rock properties and their depositional and diagenetic controls. Chapter 19 emphasizes a very promising approach, the use of microfacies in archaeology. Reservoir Rocks and Host RocksReservoir rocks are characterized by petrophysical properties favoring the capacity for the migration and storage offluids, gas and minerals. Microfacies analysis has been strongly triggered by the exploration and development of hydrocarbon reservoirs and source rocks in Iimestone and dolomites and is still of interest in understanding depositional controls, facies heterogeneities and reservoir property distribution.Carbonates can also be host rocks for ore deposits. Patterns of syn-and epigenetic mineralizations become more understandable from the use of microfacies data. E. Flügel, Microfacies of Carbonate Rocks

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Practical use of microfacies: Reservoir Rocks and Host Rocks

Flügel

2009

Microfacies of Carbonate Rocks

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Mississippi Valley-type sulfide mineralization and relationships to carbonate diagenesis: Introductory remarks

Cited by 5 publications

References 18 publications

Diagenesis and mineralization processes in Devonian carbonate rocks of the Siding-Gudan lead-zinc mineral subdistrict, Guangxi, Southwest China

Diagenesis and mineralization processes in Devonian carbonate rocks of the Siding-Gudan lead-zinc mineral subdistrict, Guangxi, Southwest China

Reservoir Rocks and Host Rocks

Practical use of microfacies: Reservoir Rocks and Host Rocks

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