Browsing by Author "Dachs E."
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Browsing by Author "Dachs E."
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Dachs E. (1994)In P - T - logfO2 space, the stability of annite (ideally KFe 32+(OH)2AlSi3O10) at high fO2 (low fH2) is limited by the reaction: annite = sanidine + magnetite + H2. Using the hydrogen-sensor technique, the equilibrium fH2 ...
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Bertoldi C.; Garbe-Schönberg D.; Dachs E.; Proyer A.; Behrens H. (2004)Cordierite samples from pegmatites and metamorphic rocks have been analysed for major [electron microprobe analysis (EMPA)] and trace elements [inductively coupled plasma mass spectrometry (ICP-MS), secondary ion mass ...
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Dachs E.; Geiger C.A. (2006)The low-temperature heat capacities for a series of synthetic garnets along the pyrope-grossular (Py-Gr) join were measured with the heat capacity option of the Physical Properties Measurement System (PPMS) produced by ...
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Benisek A.; Dachs E.; Cemic L. (1999)Six members of the annite-siderophyllite join were synthesized in a three step process - crystallization of biotite from gels, decomposition of the fine-grained biotite under oxidizing conditions and resynthesis of Fe-Al ...
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Yong W.; Essene E.J.; Dachs E.; Withers A.C. (2006)The low-temperature heat capacity (Cp) of KAlSi3O8 with a hollandite structure was measured over the range of 5-303 K with a physical properties measurement system. The standard entropy of KAlSi3O8 hollandite is 166.2±0.2 ...
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Cemič L.; Dachs E. (2006)The heat capacity of synthetic ferrosilite, Fe2Si2O6, was measured between 2 and 820 K. The physical properties measurement system (PPMS, Quantum Design®) was used in the low-temperature region between 2 and 303 K. In the ...
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Bertoldi C.; Benisek A.; Cemic L.; Dachs E. (2001)The heat capacity of natural chamosite (XFe=0.889) and clinochlore (XFe=0.116) were measured by differential scanning calorimetry (DSC). The samples were characterised by X-ray diffraction, microprobe analysis and Mössbauer ...
Now showing items 1-7 of 7