From Surf Wiki (app.surf) — the open knowledge base
Fabric (geology)
Spatial and geometric configuration of all the elements that make up a rock
Spatial and geometric configuration of all the elements that make up a rock
the geological term
In geology, a rock's fabric describes the spatial and geometric configuration of all the elements that make it up. In sedimentary rocks, the fabric developed depends on the depositional environment and can provide information on current directions at the time of deposition. In structural geology, fabrics may provide information on both the orientation and magnitude of the strains that have affected a particular piece of deformed rock.
Types of fabric
- Primary fabric — a fabric created during the original formation of the rock, e.g. a preferred orientation of clast long axes in a conglomerate, parallel to the flow direction, deposited by a fast waning current.
- Shape fabric — a fabric that is defined by the preferred orientation of inequant elements within the rock, such as platy- or needle-like mineral grains. It may also be formed by the deformation of originally equant elements such as mineral grains.
- Crystallographic preferred orientation — in plastically deformed rocks, the constituent minerals commonly display a preferred orientation of their crystal axes as a result of dislocation processes.
- S-fabric — a planar fabric such as cleavage or foliation; when it forms the dominant fabric in a rock, it may be called an S-tectonite.
- L-fabric — a linear fabric such as mineral stretching lineation where aggregates of recrystallised grains are stretched out into the long axis of the finite strain ellipsoid, where it forms the dominant fabric in a rock, it may be called an L-tectonite.
- Penetrative fabric — a fabric that is present throughout the rock, generally down to the grain scale, although this does also depend on the scale at which the observations take place.
- Magnetic fabric — orientation of magnetic particles within a rock sample or in soils to determine paleomagnetic history or to quantify tectonic strain.
References
References
- Hobbs BE, Means WD, & Williams PF. (1976). ''An outline of structural geology''. John Wiley & sons, p.73.
- Twiss RJ and Moores EM. (2007). ''Structural Geology'', 2nd Edition, WH Freeman and Co., p.497.
- Park, R.G.. (2004). "Foundation of Structural Geology". Routledge.
- (2005). "Microtectonics". Springer.
- Butler, Robert F.. (1992). "Paleomagnetism : magnetic domains to geologic terranes". Blackwell Scientific Publications.
- Borradaile, Graham John. (December 1988). "Magnetic susceptibility, petrofabrics and strain". Tectonophysics.
This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.
Ask Mako anything about Fabric (geology) — get instant answers, deeper analysis, and related topics.
Research with MakoFree with your Surf account
Create a free account to save articles, ask Mako questions, and organize your research.
Sign up freeThis content may have been generated or modified by AI. CloudSurf Software LLC is not responsible for the accuracy, completeness, or reliability of AI-generated content. Always verify important information from primary sources.
Report