WebWe propose that the cratonic keels of the eastern NCC (ENCC) and the western WC (WWC) utilized this weak MLDL layer to delaminate from overlying lithosphere. We … WebDescribe a " cratonic keel". a. Found on every continental craton a cratonic Keel extends 100-200 km. It is comprised of a thick layer of strong mantle which is a less dense material that counteracts the increased density of the lower temperature which moves along with the plates during continental drifting.
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WebMay 22, 2024 · The craton witnessed extensive lithospheric destruction with the removal of nearly 100–150 km of the cratonic root. The decratonization may be linked to subduction during the Paleo-Mesoproterozoic period, together with mantle plumes at different times, suggesting a combined mechanical, thermal and chemical erosion of the cratonic keel. WebJun 1, 2024 · Loss of keels in the North China and Wyoming cratons has been attributed to subduction of the Pacific plate in the Mesozoic ( 27, 28 ), in stark contrast to the tectonic setting around southern Africa that experienced no subduction in its recent geologic past. cbt supply furniture
Craton Destruction 1: Cratonic Keel Delamination Along a …
WebJul 29, 2024 · First, approximately 100 km of cratonic “keel” underlying a weak midlithospheric discontinuity layer (approximately 80–100 km) was rapidly removed in … WebDec 1, 2024 · During the Archean the plume impact focused in the cratonic keel (minimum of 150 km-thick for CMP, based on tomography data). Later, during the Paleoproterozoic, … WebAncient continental craton Younger orogenic zone Continental margins 0 km 100 200 300 400 500 600 700 Continental crust Depleted in basaltic contituents Cratonic keel Undepleted in basaltic contituents Zone of partial melting Oceanic crust Ocean basin Continental shelf Lower mantle Upper mantle 1300 ° C isotherm Structure profonde des ... cbt-s webテスト 70分