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The youngest Alpine magmatism (Miocene to Quaternary) in Western and Central Anatolia is represented by three coeval assemblages from West to East. They are the Western Anatolian Volcanic assemblage (...
In the past ten years the structures of bikitaite, chabazite, dachiardite, erionite, faujasite, gismondine, gmelinite,harmotome, levyne, mordenite, phillipsite and Linde A have been determined. In add...
Mineral layering is developed in the upper and marginal parts of two granite stocks intruding Precambrian gneisses north of Tigssaluk Fjord, southern Greenland. The layering consists of unusual concen...

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