Platform (geology)
(Redirected from
Continental platform
) Extended crust | Oceanic crust: 0–20 Ma 20–65 Ma >65 Ma |
In geology, a platform is a continental area covered by relatively flat or gently tilted, mainly
metamorphic rocks of an earlier deformation. Platforms, shields and the basement rocks together constitute cratons.[1] Platform sediments can be classified into the following groups: a "protoplatform" of metamorphosed sediments at the bottom, a "quasiplatform" of slightly deformed sediments, a "cataplatform", and an "orthoplatform" at the top. The Mesoproterozoic Jotnian sediments of the Baltic area are examples of a "quasiplatform".[2] The post-Ordovician rocks of the South American Platform are examples of an orthoplatform.[3]
See also
References
- ^ Parker, Sybil P. (Ed.). 1997. McGraw-Hill Dictionary of Geology and Mineralogy. New York: McGraw-Hill.
- .
- ^ de Almeida, F. F. M.; et al. (1976). "The Upper Precambrian of South America". Boletim IG-USP. 7. Archived from the original on 2015-10-01. Retrieved 2015-09-29.