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diapir |
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diapir [ˈdaɪəˌpɪə] n (Earth Sciences / Geological Science) Geology an anticlinal fold in which the brittle overlying rock has been pierced by material, such as salt, from beneath [from Greek diapeirainein to make holes through, pierce]
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Many scientists think that hotspots mark locations where diapiric convection cells, called mantle "plumes", rise beneath lithospheric plates (Morgan, 1971; Wilson, 1973). Medium to low-grade, bulk mineable disseminated deposit-type, Greisen stockworks or disseminations associated with granite emplacement at depth or laterally, controlled by reactivated thrusts by the "pushing aside" effect observed in diapiric intrusions. Based on this Krasnodar analog, these stacked reservoirs should have substantially greater petroleum reserves than contained in the smaller anticlinal features, such as Aktash, formed on the top of these diapiric structures. |
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