Geology Reference
In-Depth Information
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Further reading: K201
•
Nonparallel oblique bedding that might indicate
cross-bedding structures.
•
Gravity-dependent mechanical deposition of grains
or ore detritus.
•
Vertically graded bedding.
•
Geopetal deposition of minerals within sedimentary
cavities or in intraskeletal pores, e.g. shells filled
with micrite at the base and ore at the top.
•
Repeated sequences exhibiting an increase and de-
crease in the abundance of ore minerals within indi-
vidual strata forming rhythmic graded beds.
•
Resediments that provide evidence of erosion of ore-
containing strata.
•
Mechanical deposition of mineralized grains within
an erosional bottom relief.
•
Syngenetic deformation of both ore bodies and host
carbonates due to sliding and slumping.
Basics: Carbonatehosted mineral deposits
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De Voto, R.H. (1988): Late Mississippian paleokarst and re-
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Fan, D., Hein, J.R., Jye, J. (1999): Ordovician reef-hosted
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Friedrich, G.H., Herzig, P.M. (eds., 1988): Base metal sul-
