Facies

For other uses, see facies (disambiguation).
Eolianite carbonate facies (Holocene) on Long Island, Bahamas.

In geology, a facies (pronounced variously as /ˈfeɪʃiːz/, /ˈfeɪsiːz/ or /ˈfæʃiːz/ ['faysheez', 'fayseez' or 'fash-eez']; plural also 'facies') is a body of rock with specified characteristics.[1] Ideally, a facies is a distinctive rock unit that forms under certain conditions of sedimentation, reflecting a particular process or environment.

The term facies was introduced by the Swiss geologist Amanz Gressly in 1838 and was part of his significant contribution to the foundations of modern stratigraphy,[2] which replaced the earlier notions of Neptunism.

Types of facies

Sedimentary facies

Middle Triassic marginal marine siltstone and sandstone facies exposed in southern Utah.

Sedimentary facies are bodies of sediment recognizably different from adjacent sediment deposited in a different depositional environment. Generally, facies are distinguished by what aspect of the rock or sediment is being studied. Thus, facies based on petrological characters such as grain size and mineralogy are called lithofacies, whereas facies based on fossil content are called biofacies.

These facies types are usually further subdivided, for example, you might refer to a "tan, cross-bedded oolitic limestone facies" or a "shale facies". The characteristics of the rock unit come from the depositional environment and original composition. Sedimentary facies reflect depositional environment, each facies being a distinct kind of sediment for that area or environment.

Since its inception, the facies concept has been extended to related geological concepts. For example, characteristic associations of organic microfossils, and particulate organic material, in rocks or sediments, are called palynofacies. Discrete seismic units are similarly referred to as seismic facies.

Walther's Law of Facies

Stratigraphic column on north shore of Isfjord, Svalbard, Norway. The vertical succession of rock types (representing sedimentary facies) reflects lateral changes in paleoenvironment.

Walther's Law of Facies, or simply Walther's Law, named after the geologist Johannes Walther, states that the vertical succession of facies reflects lateral changes in environment. Conversely, it states that when a depositional environment "migrates" laterally, sediments of one depositional environment come to lie on top of another.[3] In Russia the law is known as Golovkinsky-Walther’s Law honoring also Nikolai A. Golovkinsky.[4] A classic example of this law is the vertical stratigraphic succession that typifies marine transgressions and regressions.

Metamorphic facies

Main article: metamorphic facies

The sequence of minerals that develop during progressive metamorphism (that is, metamorphism at progressively higher temperatures and/or pressures) define a facies series.

Seismic facies

Seismic Facies are mappable three dimensional seismic units composed of reflections units whose parameters different from adjacent facies units.

See also

References

The Wikibook Historical Geology has a page on the topic of: Walther's principle
  1. ↑ Reading, H. G. (1996). Sedimentary Environments and Facies. Blackwell Scientific Publications. ISBN 0-632-03627-3.
  2. ↑ Cross, T. A.; Homewood, P. W. (1997). "Amanz Gressly's role in founding modern stratigraphy". Geological Society of America Bulletin (Geological Society of America) 109 (12): 1617–1630. doi:10.1130/0016-7606(1997)109<1617:agsrif>2.3.co;2.
  3. ↑ Stanley, Steven M. (1999). Earth System History. New York: W.H. Freeman and Company. p. 134. ISBN 0-7167-2882-6.
  4. ↑ Nurgalieva, N. G.; Vinokurov, V. M.; Nurgaliev, D. K. (2007). "The Golovkinsky strata formation model, basic facies law and sequence stratigraphy concept: Historical sources and relations". Russian Journal of Earth Sciences 9.
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