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stylolite

   Also found in: Encyclopedia, Wikipedia 0.02 sec.
sty·lo·lite  (stl-lt)
n.
A secondary structure found along contacting surfaces of adjacent calcareous rock layers, the contact zone appearing in cross section as a series of jagged interlocking up-and-down projections that resemble a suture or the tracing of a stylus.

[Greek stlos, pillar; see stylite + -lite.]

stylolite [ˈstaɪləˌlaɪt]
n
(Earth Sciences / Palaeontology) any of the small striated columnar or irregular structures within the strata of some limestones
[from Greek stulos pillar + -lite]
stylolitic  [ˌstaɪləˈlɪtɪk] adj

stylolite  (stl-lt)
A contact surface usually found between two calcareous rock layers, marked by a series of jagged interlocking up-and-down projections that resemble a suture or the tracing of a stylus. Stylolites are found in rocks that have been subjected to pressure and are formed by a process, called pressure dissolution, whereby insoluble material, such as clay and hydrocarbons, becomes concentrated along a surface while other more soluble material, such as calcite, is carried away.


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Kaolincoating in stylolites, effect of quartz cementation and general implications for dissolution at mineral interfaces.
The Tennessee marble is characterized by well developed stylolites having two orientations.
In the limestones, pressure solution has resulted in the formation of stylolites (Figure 4D), while fenestral porosity (Figure 3C) formed as a result of the decay of organic material.
 
 
 
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