Examples of 'facies' in a sentence
Meaning of "facies"
Facies (noun): In geology, facies refers to the overall characteristics of a rock unit, including its mineral composition, sedimentary structures, and fossil content, that help in identifying and interpreting the environment in which it was formed
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- General appearance.
- Facial features, like an expression or complexion, typical for patients having certain diseases or conditions.
- A body of rock with specified characteristics reflecting its formation, composition, age, and fossil content.
How to use "facies" in a sentence
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facies
Combining of facies groups to a smaller number of sets.
Inputting of individual descriptions for each facies.
These facies are thought to represent a lacustrine environment.
The reservoir contains a facies of constant porosity.
A foliated granite is locally developed as a marginal facies.
The dark facies is rich in green hornblende.
Indication of dominant facies for each zone.
Certain part of it only exhibits a flysch facies.
The proofs and the facies libri to review.
No rhythmic pattern is recognized in these subtidal facies.
Calculation of facies distribution percentage for each zone.
There can be lithologic and sedimentary facies.
Number of facies is determined by graphical selection of dendrogram cuts.
No measurable tilting accompanied this change of facies.
This facies is named for the mineral sanidine.
See also
These rocks are generally metamorphosed to the greenschist facies.
A facies thus corresponds to each simulated value in a grid.
These characteristics lead to mask facies.
Similar facies occur in adjoining eskers.
Seven architectural elements were recognized based on facies associations.
The facies realization is therefore converted to a continuous realization.
Lawsonite is a metamorphic mineral typical of the blueschist facies.
Microscopic observations of fracture facies validated these results.
Discrete seismic units are similarly referred to as seismic facies.
The essential characteristics of each facies are described in detail.
Principles of classification of volcanic rocks and volcanogenic facies.
Facies identification in an uncored borehole is a classic problem in formation evaluation.
The terrane displays amphibolite to granulite facies metamorphism.
This facies contains also micropegmatites and pegmatitic geodes.
Garnets are also useful in defining metamorphic facies of rocks.
These facies reflect deposition in adjacent and gradational paleoenvironments.
The dominant mineral in the carbonate facies is siderite.
Facies anterior corporis pancreatis.
Most fossils are from the siltstone facies.
Facies inferior corporis pancreatis.
The dominant mineral in the sulfide facies is pyrite.
Facies dorsalis ossis sacri.
Explosive volcanic activity and formation of pyroclastic facies.
Facies pelvica ossis sacri.
Estimating the regional distribution of the sedimentary facies.
Facies where bushes grow.
Each environment is represented by several facies.
These average facies proportions are calculated independently in each region.
Stratified sediments also occur in places in this facies.
We also observed an eclogitic facies at the base of thecontinental crust.
The thresholds define intervals of belonging to a lithologic facies.
Facies simulation can then be constrained by the computed bathymetry.
All the rocks are metamorphosed to the greenschist facies.
The facies are expressive and charming excluding all ferocity.
The dry heath may present various facies.
