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  • noun

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the part of a continent that is stable and forms the central mass of the continent

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References in periodicals archive ?
Peter Sandstone--A record of eolian and fluvial sedimentation of early Paleozoic cratonic sheet sand: Journal of Sedimentary Research, v.
They cover non-volcanic and transform passive margins, cratonic basins on pre-Cambrian and Paleozoic basements, and world maps.
Geochemistry and mineralogy of sediments from the Ventersdorp and Transvaal Supergroups, South Africa: Cratonic evolution during the early Proterozoic: Geochimica et Cosmochimica Acta, 54(2), 343-354.
What lies below Cratonic crust is cooler and stronger than oceanic crust.
During the post-Tremadocian, from the Hunneberg time of the early Ordovician to the end of the Silurian, Estonia was a part of the northern flank of a shallow cratonic sea (Fig.
These areas were identified based upon the geological history of Madagascar and presence of the cratonic core, as well as historic discoveries of alluvial diamonds and other kimberlitic indicator minerals.
It has been written to provide you with a detailed overview of geologic rift systems, passive margins, and cratonic basins, it features the basic principles necessary to grasping the conceptual approaches to hydrocarbon exploration in a broad range of geological settings globally.
Structure and tectonic evolution of the transitional region between the central Appalachian foreland and interior cratonic basins.
Better understanding of earthquakes in stable cratonic regions, particularly levels of activity and maximum magnitudes (Mazzotti and Adams 2005; Fenton et al.
The mudstone organic matter is extremely fine and moves easily with water across the comparatively flat cratonic surface.
2000) that assignees crustal thickness to the Guiana Craton taken data from other cratonic areas of the world.
Most of Finland lies on the so-called Baltic Shield- the ancient cratonic mass
Belton DX, Brown RW, Kohn BP, Fink D, Farley KA (2004) Quantitative resolution of the debate over antiquity of the central Australian landscape: implications for the tectonic and geomorphic stability of cratonic interiors.
The Hirnantian glaciation, accompanied by a marked sea level fall, introduced favourable conditions for coral evolution on many subequatorial cratonic shelves, which helped corals to survive the severe conditions of the glacial period dominating at low latitudes.