Mississippi Valley-Type lead-zinc district

E615931

The Mississippi Valley-Type lead-zinc district is a class of ore deposits characterized by stratabound concentrations of lead and zinc sulfides hosted in carbonate rocks, typically formed from low-temperature, basin-derived mineralizing fluids.

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Observed surface forms (1)

Statements (51)

Predicate Object
instanceOf mineral deposit model
ore deposit type
distinguishedFrom porphyry copper deposits
sedimentary exhalative deposits
volcanogenic massive sulfide deposits
fluidSource basinal brines
fluidTemperature low-temperature
geneticProcess basin dewatering
hydrothermal fluid flow
metal transport in chloride brines
sulfide precipitation
geochemicalEnvironment reduced sulfur-rich conditions
hasAlteration carbonate dissolution
dolomitization
sulfidization
hasCommodity lead
zinc
hasMineral barite
calcite
dolomite
fluorite
galena
marcasite
pyrite
sphalerite
hostRock carbonate rocks
dolostone
limestone
metalAssociation lead-zinc-barium-fluorine
oreBodyStyle replacement deposit
stratabound
vein and breccia fill
oreControl lithologic controls
stratigraphic controls
structural controls
precipitationMechanism cooling of fluids
mixing of fluids
reaction with carbonate host rocks
tectonicSetting foreland basins
passive margin basins
sedimentary basins
typicalAgeRange Mesozoic
Paleozoic
typicalOreTexture breccia cement
open-space filling
replacement textures
typicalStructure fault-controlled
fracture-controlled
karst-related
usedIn mineral exploration models
resource assessment studies

Referenced by (2)

Full triples — surface form annotated when it differs from this entity's canonical label.

Empire District of the Tri-State mining district geologicalType Mississippi Valley-Type lead-zinc district
Wisconsin Territory hasJurisdictionOver Mississippi Valley-Type lead-zinc district
this entity surface form: Lead mining region of Upper Mississippi Valley