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Publications
Helmholtz Centre Potsdam
GFZ German Research Centre for Geosciences
(Co) Author: Emmermann, R.
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Robinson, P. T.; Trumbull, R. B.; Kostrowski, S.; Erzinger, J.; Schmitt, A.; Emmermann, R. (2007): Crustal contamination of the upper mantle: evidence from ophiolites. Geochimica et Cosmochimica Acta, 71, 15, Suppl. 1, A523.
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Merz, B.; Emmermann, R. (2006): Zum Umgang mit Naturgefahren in Deutschland: Vom Reagieren zum Risikomanagement. GAiA - Ecological Perspectives in Science Humanities and Economics, 15, 4, 265-274.
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Wigand, M.; Schmitt, A. K.; Trumbull, R. B.; Villa, I. W.; Emmermann, R. (2004): Short-lived magmatic activity in an anorogenic subvolcanic complex: 40Ar/39Ar and ion microprobe U-Pb zircon dating of the Erongo, Damaraland Province, Namibia. Journal of Volcanology and Geothermal Research, 130, 3-4, 285-305.
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Emmermann, R.; Donner, W. T. (2003): Naturwissenschaften - the long-standing official organ of the German Society of Natural Scientists and Physicians. Naturwissenschaften, 90, 1, 1-3.
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Robinson, P. T.; Erzinger, J.; Emmermann, R. (2002): The Composition and Origin of Igneous and Hydrothermal Veins in the Lower Ocean Crust - ODP Hole 735B, Southwest Indian Ridge. Proceedings of the Ocean Drilling Program : Scientific results, 176, 55.
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Lindsay, J. M.; Schmitt, A. K.; Trumbull, R. B.; de Silva, S. L.; Siebel, W.; Emmermann, R. (2001): Magmatic evolution of the La Pacana Caldera system, central Andes, Chile: compositional variation of two cogenetic, large-volume felsic ignimbrites and implications for contrasting eruption mechanisms. Journal of Petrology, 42, 3, 459-486.
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Schmitt, A. K.; de Silva, S. L.; Trumbull, R. B.; Emmermann, R. (2001): Magma evolution in the Purico ignimbrite complex, northern Chile: evidence for zoning of a dacitic magma by injection of rhyolitic melts following mafic recharge. Contributions to Mineralogy and Petrology, 140, 6, 680-700.
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Siebel, W.; Schnurr, W. B. W.; Hahne, K.; Kraemer, B.; Trumbull, R. B.; Bogaard, P.; Emmermann, R. (2001): Geochemistry and isotope systematics of small- to medium-volume Neogene-Quaternary ignimbrites in the southern central Andes: evidence for derivation from andesitic magma sources. Chemical Geology, 171, 3-4, 213-237.
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