TEXTURE TYPES
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on terms in blue below to see captioned photo examples.
Mudstone:
Muddy carbonate rock containing less than 10 percent grains (Dunham,
1962). Generally indicates calm water and apparent inhibition
of grain-producing organisms (low-energy depositional setting).
Wackestone:
Mud-supported carbonate rock containing more than 10 percent grains
(Dunham, 1962). Generally indicates calm water and restriction
of grain-producing organisms (low-energy depositional setting).
In cases where grains are exceptionally large, Embry and Klovan
(1971) designated these carbonates “floatstones.”
Packstone:
Grain-supported muddy carbonate rock (Dunham, 1962). Lucia (1999)
divided packstones into mud-dominated (pore spaces totally filled
with mud) and grain-dominated (some intergrain pore space is free
of mud) packstones. This division is important in understanding
reservoir quality because mud plugs interparticle pore spaces.
Packstones indicate a range of depositional properties. Mud suggests
lower-energy processes, whereas the abundance of grains suggests
higher-energy processes. Dunham (1962) provided several scenarios
for the origin of packstones: (1) they may be a product of compacted
wackestones, (2) they may result from early or late mud infiltration
of previously deposited mud-free sediments, (3) they may result
from the prolific production of grains in calm water, or (4) they
may record the mixing by burrowers of different layers of sediment.
In cases where the grains are exceptionally large, Embry and Klovan
(1971) designated these carbonates “rudstones.”
Grainstone:
Mud-free carbonate rocks, which are grain supported (Dunham, 1962).
They generally are deposited in moderate- to high-energy environments,
but their hydraulic significance can vary. Dunham (1962) provided
several suggestions for their origin: (1) they may be produced
in high-energy, grain-productive environments where mud cannot
accumulate, (2) they may be deposited by currents that drop out
the grains and bypass mud to another area, or (3) they may be
a product of winnowing of previously deposited muddy sediments.
In cases where the grains are exceptionally large, Embry and Klovan
(1971) designated these carbonates “rudstones.”
Boundstone:
Carbonate rocks showing signs of being bound during deposition
(Dunham, 1962). Embry and Klovan (1972) further expanded the boundstone
classification on the basis of the fabric of the boundstone. They
have three subdivisions:
(1)
framestone: the organisms build a rigid framework,
(2) bindstone:
the organisms encrust and bind loose sediment together, and
(3) bafflestone:
the organisms do not form a framework or bind the sediments
together but provide protected areas for the sediment to accumulate
by baffling the currents.
Boundstones
generally are deposited in higher energy environments, where currents
can provide nutrients to the organisms that form the boundstone,
as well as carry away waste products.
Crystalline
carbonates: Carbonate rocks that lack enough evidence
of depositional texture to be classified. Extensive dolomitization
commonly obliterates the original depositional texture.
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