Platform (geology)
From Wikipedia, the free encyclopedia
Please help improve this article or section by expanding it. Further information might be found on the talk page or at requests for expansion. (December 2007) |
In geology, a platform is a continental area covered by relatively flat or gently tilted, mainly sedimentary strata, which overlie a basement of consolidated igneous or metamorphic rocks of an earlier deformation. Platforms, shields and the basement rocks together constitute cratons.
[edit] See also
[edit] References
Parker, Sybil P. (Ed.). 1997. McGraw-Hill Dictionary of Geology and Mineralogy. New York: McGraw-Hill.