作者: Martin Frey , Johannes C. Hunziker , James R. O'Neil , Hans W. Schwander
DOI: 10.1007/BF00372224
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摘要: Nine samples from the Monte Rosa Granite have been investigated by microscopic, X-ray, wet chemical, electron microprobe, stable isotope and Rb-Sr K-Ar methods. Two mineral assemblages distinguished optical methods dated as Permian mid-Tertiary means of age determinations. The assemblage comprises quartz, orthoclase, oligoclase, biotite, muscovite whereas Alpine microcline, albite+epidote or phengite.