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H

Hans Kreuzer

Researcher at Institute for Geosciences and Natural Resources

Publications -  24
Citations -  1756

Hans Kreuzer is an academic researcher from Institute for Geosciences and Natural Resources. The author has contributed to research in topics: Metamorphism & Hornblende. The author has an hindex of 16, co-authored 24 publications receiving 1604 citations.

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High-potassium, calc-alkaline I-type plutonism in the European Variscides: northern Vosges (France) and northern Schwarzwald (Germany)

Rainer Altherr, +4 more
- 01 Jan 2000 - 
TL;DR: In this paper, the chemical and isotopic properties of early carboniferous high-K, calc-alkaline I-type plutonic rocks from the northern Vosges and Schwarzwald were studied for their chemical and Sr-Nd isotopic compositions.
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40Ar/39Ar and oxygen isotope studies of polymetamorphism from Tinos Island, Cycladic blueschist belt, Greece

Michael Bröcker, +3 more
- 01 Mar 1993 - 
TL;DR: Petrological, oxygen isotope and 40Ar/39Ar studies were used to constrain the Tertiary metamorphic evolution of the lower tectonic unit of the Cyclades on Tinos.
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Geochronology of high-pressure rocks on Sifnos (Cyclades, Greece)

Rainer Altherr, +8 more
- 01 Oct 1979 - 
TL;DR: K-Ar and Rb-Sr dates on phengites (predominantly 3T) of the best preserved high P/itTmetamorphic rocks from northern Sifnos gave concordant ages around 42 m.y..
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Isotopic dating of pre-Alpidic rocks from the island of Ios (Cyclades, Greece)

Friedhelm Henjes-Kunst, +1 more
- 03 Mar 1982 - 
TL;DR: The lower tectonic unit of Ios provides evidence of an at least four stage metamorphic and intrusive history which well might be generalized for large parts of the internal Pelagonian as mentioned in this paper.
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K-Ar geochronology of different tectonic units at the northwestern margin of the Bohemian Massif

Hans Kreuzer, +5 more
- 20 Jan 1989 - 
TL;DR: In this paper, the authors used K-Ar analysis of hornblendes and muscovites from the autochthonous units of the Saxothuringian and the Munchberg nappe pile (MM) to obtain dates around 380-320 Ma for the prasinite-phyllite series.