Petrologija in pogoji nastanka karavanškega tonalita : doktorska disertacija
Faninger, Ernest
Petrološko smo preiskali karavanško magmatsko cono, da bi ugotovili medsebojni odnos in genezo tamkajšnjih globočin, kakor tudi razmerje do vzhodneje ležeče pohorske globočine. Rezultati vseh ...dosedanjih raziskav je sledeč: ugotavljamo, da karavanški gnajsni tonalit genetsko ni povsem povezan z granitom odnosno z globočinami granitnega pasu. Oba pasova karavanške magmatske cone sta posledica dveh različnih in časovno ločenih magmatizomov. Po dosedanjih radometričnih določitvah absolutnih starosti so karavanški granit in z njim genetsko povezane globočine granitnega pasu sigurno variscične, gnajsni tonalit pa je po vsej verjetnosti alpidske starosti. Medtem ko imamo lahko magmo karavanškega tonalitnega gnajsa za diferenciat neke iz zemljskega plašča izvirajoče mafične magme, predstavlja magma pohorske globočnine produkt hibridizacije med daleč prevladujoče palingenetsko magmo in magmo, v zvezi s katero je prišlo tudi do nastanka karavanškega gnajsnega tonalita.
Type of material - dissertation
; adult, serious
Publication and manufacture - E. Faninger, 1975 ; Ljubljana
Central Technological Library of the University of Ljubljana
52047/252 Skladišče IN: 397600328
available - outside loan, loan period: 14 days
NTF, Department of Geology, Lj.
Geologija M FANINGER Ernest Petrologija IN: 000012852
available - outside loan, loan period: 14 days
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