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craton |
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Scientists got their first inklings that cratonic plates differ from plates under oceans and the younger, deformed parts of continents, called orogenic zones, in the 1960s. recognize and document the trend fairway as analogous to the Canadian Foothills and Arkoma Spiro/Wapanucka trends, both exhibiting prolific Cratonic Margin plays as is the case in the Val Verde Basin. EM1 may be delaminated Archean subcontinental lithosphere, given that the most extreme isotopic examples come from some Cenozoic, cratonic mafic magmas (Greenough and Kyser, 2003). |
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