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Such waters form two important classes of deposit.
They are the most numerous of all classes of deposit.
Together with the classes of deposit that they form, these agents are discussed below.
Rather, specific classes of deposit tend to be concentrated in particular areas or regions called metallogenic provinces.
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Because the central plains coincide closely with the drainage basin of the Mississippi River, this class of deposit has come to be called the Mississippi Valley type (MVT).
This class of deposit comprises compounds of iron or manganese and is known as a chemical sediment, because the mineral constituents are transported in solution and then precipitated to form a sediment as a result of chemical reaction.
Secondary enrichment can affect most classes of ore deposit, but it is notably important in three circumstances.
Metallogenic epochs are units of geologic time during which conditions were particularly favourable for the formation of specific classes of mineral deposit.
Each one of the four classes of the deposited tungsten oxides exhibits its own optical properties, which indicates that each class has its own electronic structure.
An especially important class of residual deposit is formed by both the removal of valueless material in solution and the solution and redeposition of valuable ore minerals.
The cover of sedimentary rocks, which have been little changed since they were deposited, contains numerous strata of limestone, and within the limestones near the bottom of the pile is found a distinctive class of mineral deposit.
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