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Center for Applied Geosciences, Eberhard Karls University of Tuebingen, Sigwartstrasse 10, D-72076 Tuebingen, Germany Present address: Helmholtz Centre for Environmental Research - UFZ, Department of Bioenergy, Permoserstrasse 15, D-04318 Leipzig, Germany.
Institut für Geowissenschaften, Sigwartstrasse 10, Abteilung Geophysik, 72076 Tübingen, Germany
Institute for Geosciences, University Tübingen, Sigwartstr. 10, D-72076 Tübingen, Germany für Geologie und Paläontologie, Universität Tübingen, Sigwartstrasse 10, D-72076 Tübingen, Germany
Institut für Geologie, Universität, D-7400 Tübingen, Germany
Institute for Applied Geosciences, University of Tuebingen, Sigwartstr 10, 72076 Tuebingen, Germany
Fachbereich Geowissenschaften, Universität Tübingen, Sigwartstr. 10, 72076 Tübingen, Germany
Institut für Geowissenschaften, Abteilung Geophysik, Sigwartstrasse 10, 72076 Tübingen, Germany
Institut für Geologie und Paläontologie, Universität Tübingen, Sigwartstrasse 10, 72076 Tübingen, Germany
Institut für Allgemeine und Angewandte Geophysik, Universität München, Theresienstrasse 41, D-8000 München 2 W. Germany
Institut für Geologie, Universität Tübingen, Sigwartstrasse 10, 72076, Tübingen, Germany
Institut für Geologie und Paläontologie, Arbeitsbereich Geophysik, Universität Tübingen, Sigwartstrasse 10, D-72076 Tübingen, Germany für Allgemeine und Angewandte Geophysik, Theresienstrasse 41, D-8000 München 2, Germany
A study of gyroremanent magnetisation (GRM) and rotational remanent magnetisation (RRM) carried by greigite from lake sediments
Comment on ``Paleomagnetic study of the Eocene Quxu pluton of the Gangdese Belt: Crustal deformation along the Indus-Zangbo suture zone in Southern Tibet'' by Y. Otofuji et al.
Dependence of microbial magnetite formation on humic substance and ferrihydrite concentrations
Detailed analysis of successive pTRMs carried by pyrrhotite in Himalayan metacarbonates: an example from Hidden Valley, Central Nepal
Domain structure of small synthetic titanomagnetite particles and experiments with IRM and TRM
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