The part of a continent that is stable and forms the central mass of the continent; typically Precambrian.
Cratons contain the ancient crust of igneous rocks.
Ancient metamorphic and igneous rock, usually in the middle of continents.
The sequences of sedimentary rocks in cratons are typically thin and are relatively undeformed or gently warped. The sequences in mountain belts, meanwhile, are thick and extensively folded and faulted.
Areas of ancient continental interiors are called cratons.
According to Wikipedia, a craton is an "...old and stable part of the continental lithosphere" -- the earth's outermost rocky shell. Kimberlite pipes, where diamonds are commonly found, are sometimes rooted in cratons. You can read more by following the link, below.
Cratons, large geologically stable areas in continental interiors.
Platforms and shields together make up cratons. The shield is the part of the craton that is exposed at Earth's surface and the platform is the part of the craton that is covered by sedimentary strata.
Cratons contain the ancient crust of igneous rocks.
cratons
Old Continental cratons with diatremes or in sediments derived from such.
The sequences of sedimentary rocks in cratons are typically thin and are relatively undeformed or gently warped. The sequences in mountain belts, meanwhile, are thick and extensively folded and faulted.
The sequences of sedimentary rocks in cratons are typically thin and are relatively undeformed or gently warped. The sequences in mountain belts, meanwhile, are thick and extensively folded and faulted.
Areas of ancient continental interiors are called cratons.
According to Wikipedia, a craton is an "...old and stable part of the continental lithosphere" -- the earth's outermost rocky shell. Kimberlite pipes, where diamonds are commonly found, are sometimes rooted in cratons. You can read more by following the link, below.
Cratons, large geologically stable areas in continental interiors.
In old areas of continental crust called "cratons" in volcanic structures called "kimberlite pipes".
It was formed when cratons collided and welded together.I dont know if he is right but i think that he is really good I dont know what it means.
Since diamonds are most rare, indicator minerals are the only way to predict -- sometimes unsuccessfully -- where a miner might locate diamonds.The pipes are always required, since that's how diamonds are pushed up to the surface from earth's upper mantle, and kimberlite is not the only indicator mineral. (Link, below.)Diamond formation does not occur in the pipes: it occurs in cratons. From Wikipedia:"The correct combination of temperature and pressure is only found in the thick, ancient, and stable parts of continental plates where regions of lithosphere known as cratons exist. Long residence in the cratonic lithosphere allows diamond crystals to grow larger."You can read more about cratons, below.
Henry V. Lyatsky has written: 'Principles of practical tectonic analysis of cratonic regions' -- subject(s): Cratons, Structural Geology