- vergent
- ver|gent[v...]<aus lat. vergens, Gen. vergentis, Part. Präs. von vergere, vgl. ↑vergieren>gekippt (von Gesteinsfalten; Geol.).
Das große Fremdwörterbuch. 2013.
Das große Fremdwörterbuch. 2013.
vergent — ver|gẹnt <Adj.> [zu lat. vergens (Gen.: vergentis), 1. Part. zu: vergere = sich neigen] (Geol.): geneigt (von Falten 3) … Universal-Lexikon
Vergent — … Useful english dictionary
Maria Fold and Thrust Belt — The Maria Fold and Thrust Belt is a series of mountain ranges in southeastern California and western Arizona that is geologically characterized by geologic structures that trend differently than it the rest of the Cordillera and Basin and Range… … Wikipedia
Moldanubian Zone — Most important structures and zones of the Variscan or Hercynian Orogeny in Europe.[1] The Moldanubian Zone is in the regional geology of Europe a tectonic zone formed during the Variscan or Hercynian Orogeny (400 to 300 million ye … Wikipedia
End — (Roget s Thesaurus) < N PARAG:End >N GRP: N 1 Sgm: N 1 end end close termination Sgm: N 1 desinence desinence conclusion finis finale period term terminus endpoint last omega … English dictionary for students
Emily Ann and Maggie Hays nickel mines — The Emily Ann and Maggie Hays nickel deposits are situated approximately 150km west of the town of Norseman, Western Australia, within the Lake Johnston Greenstone Belt [Hill R.E.T, Barnes S.J., Gole M.J., and Dowling S.E., 1990. Physical… … Wikipedia
Superior craton — in the west. The western margin extends from northern Minnesota through eastern Manitoba to northwestern Ontario.The formation of the Superior craton is best explained within the context of 2.72 2.68 Ga accretion of small continental plates and… … Wikipedia
Michoud fault — The Michoud fault is a geological fault that runs through eastern New Orleans. [1] The Michoud fault is the subject of extensive scientific inquiry into why Louisiana is losing vast tracts of land … Wikipedia
Maria fold and thrust belt — Ranges, Plains Thrusted Forms Country United States States … Wikipedia
Massif Central (geology) — The Massif Central forms together with the Armorican Massif (Brittany and Normandy) one of the two big basement massifs in France. Its geological evolution started in the late Neoproterozoic and continues to this day. It has been shaped mainly by … Wikipedia