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Dolomite Textures

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Dolomite (dolostone) is composed mainly of the mineral dolomite [CaMg(CO3)2]. [1] Unlike limestone, which is characterized by the presence of grains, micrite, and/or sparry cement, dolomite has a largely crystalline (granular) texture. [1]

Classification by Crystal Shape

On the basis of crystal shape, two kinds of dolomite are recognized. [1]

Planar (Idiotopic) Dolomite

Planar (or idiotopic) dolomite consists of rhombic, euhedral (well-formed) to anhedral (poorly formed) crystals. [1]

Nonplanar (Xenotopic) Dolomite

Nonplanar (or xenotopic) dolomite is made of nonplanar, commonly anhedral crystals. [1]

Subtypes

Each of these major kinds of dolomite can be divided into subtypes. [1]

Formation by Replacement

Many dolomites form by replacement of a precursor limestone. [1] Original limestone textures may be preserved in such dolomites to various degrees, ranging from virtually unreplaced to totally replaced. [1]

The replacing dolomite may preserve the original texture as a “ghost” (mimicking replacement) or the original texture may be completely destroyed (nonmimicking replacement). [1]

References & Citations

  • 1.
    Principles of Sedimentology and Stratigraphy Boggs
Dr. Jeev Jatan Sharma

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