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Jörg A. Pfänder

Researcher at Freiberg University of Mining and Technology

Publications -  77
Citations -  3913

Jörg A. Pfänder is an academic researcher from Freiberg University of Mining and Technology. The author has contributed to research in topics: Basalt & Metamorphism. The author has an hindex of 26, co-authored 72 publications receiving 3250 citations. Previous affiliations of Jörg A. Pfänder include University of Mainz & Max Planck Society.

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MPI-DING reference glasses for in situ microanalysis: New reference values for element concentrations and isotope ratios

Klaus Peter Jochum, +60 more
TL;DR: In this paper, the authors present new analytical data of major and trace elements for the geological MPI-DING glasses KL2-G, ML3B-G and ATHO-G.
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Evolution of planetary cores and the Earth-Moon system from Nb/Ta systematics.

TL;DR: High-precision measurements of Nb/Ta and Zr/Hf reveal that Nb is moderately siderophile at high pressures, and can be linked in time with the final core-mantle equilibration on Earth 4.533 billion years ago.
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Nb/Ta and Zr/Hf in ocean island basalts — Implications for crust–mantle differentiation and the fate of Niobium

TL;DR: In this paper, high-precision Nb, Ta, Zr, Hf and Lu measurements for a variety of ocean island basalts determined by isotope dilution MC-ICPMS together with Hf isotope compositions are presented to constrain OIB source characteristics and HFSE fractionation during mantle melting and crystal fractionation.
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MPI-DING glasses: New geological reference materials for in situ Pb isotope analysis

TL;DR: In this paper, high-precision Pb isotope analyses by TIMS and MC-ICPMS techniques on seven geological MPI-DING glasses were performed by using a single-collector sector-field ICP mass spectrometer.
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Source composition and melting temperatures of orogenic granitoids: constraints from CaO/Na2O, Al2O3/TiO2 and accessory mineral saturation thermometry

TL;DR: In this article, a comparison of temperatures from melting experiments with corresponding Al2O3/TiO2 values indicate a reasonably good correlation ( r 2: 0.70-0.91), demonstrating the usefulness of temperature estimates in granitoid rocks based on Al2 o3/ti o2 systematics.