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Differential volumetric analysis combined with monitoring of differential ultra-sound travel time, an approach for tracing fine-structural compression behaviour of solids: a study on MgO / periclase and polyethylene / PE up to 1.5 GPa at room temperature

Physics and chemistry of minerals, 2020-06, Vol.47 (6), Article 26

2020

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Isobaric annealing of high-density amorphous ice between 0.3 and 1.9 GPa : in situ density values and structural changes

Physical chemistry chemical physics : PCCP, 2006, Vol.8 (3), p.386-397

2006

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An experimental investigation of Na incorporation in cordierite in low P/high T metapelites

Mineralogy and petrology, 2018-04, Vol.112 (2), p.199-217

2018

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Cordierite under hydrostatic compression: Anomalous elastic behavior as a precursor for a pressure-induced phase transition

The American mineralogist, 2014-02, Vol.99 (2-3), p.479-493

2014

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Initial stages of carbonate weathering: climate chamber studies under realistic pollution conditions

Environmental earth sciences, 2008-12, Vol.56 (3-4), p.507-519

2008

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Geothermobarometry of a stilpnomelane–garnet-bearing metapegmatite: P–T constraints on the Eo-Alpine metamorphic overprint of the Austroalpine nappes north of the Tauern Window

Mineralogy and petrology, 2009-05, Vol.96 (1-2), p.99-111

2009

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The fine-structure of the dehydration boundary of brucite (Mg(OH)2) up to 3.5 GPa - indication of anomalous PVT behaviour of supercritical H2O

European journal of mineralogy (Stuttgart), 2005-07, Vol.17 (4), p.537-542

Mirwald, Peter W.

2005

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Moisture sorption behaviour of salt mixtures in porous stone

Chemie der Erde, 2009-01, Vol.69 (1), p.91-98

2009

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Experimental study of the dehydration reactions gypsum-bassanite and bassanite-anhydrite at high pressure: indication of anomalous behavior of H(2)O at high pressure in the temperature range of 50-300 degrees C

The Journal of chemical physics, 2008-02, Vol.128 (7), p.074502-074502

Mirwald, Peter W

2008

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Experimental study of the dehydration reactions gypsum-bassanite and bassanite-anhydrite at high pressure: Indication of anomalous behavior of H2O at high pressure in the temperature range of 50–300°C

The Journal of chemical physics, 2008-02, Vol.128 (7)

Mirwald, Peter W.

2008

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Experimental study of the dehydration reactions gypsum-bassaniteand bassanite-anhydrite at high pressure: Indication of anomalous behavior of H 2 O at high pressure in the temperature range of 50 - 300 ° C

The Journal of chemical physics, 2008-02, Vol.128 (7), p.074502-074502-7

Mirwald, Peter W.

2008

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Pore and hygric properties of porous limestones: a case study from Bratislava, Slovakia

Geological Society special publication, 2010-01, Vol.333 (1), p.165-174

2010

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Petrophysical properties of selected Quaternary building stones in western Austria

Geological Society special publication, 2010-01, Vol.333 (1), p.143-152

2010

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The melting curve of gold, silver, and copper to 60-Kbar pressure: A reinvestigation

Journal of Geophysical Research: Solid Earth, 1979-11, Vol.84 (B12), p.6750-6756

1979

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A high-pressure phase transition in cordierite

The American mineralogist, 1982-04, Vol.67 (3-4), p.277-283

Mirwald, Peter W

1982

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The electrical conductivity of calcite between 300 and 1200 C at a CO2 pressure of 40 bars

Physics and chemistry of minerals, 1979, Vol.4 (4), p.291-297

Mirwald, Peter W.

1979

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A differential thermal analysis study of the high-temperature polymorphism of calcite at high pressure

Contributions to mineralogy and petrology, 1976, Vol.59 (1), p.33-40

Mirwald, Peter W.

1976

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Material properties, room-climate measurements and building history - an interdisciplinary project to set the conditions of restoration and re-use for the fortress of Kufstein, Tyrol, Austria

Building and environment, 2003-09, Vol.1 |t 17, p.1133-1141.

2003

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Low-friction cell for piston-cylinder high-pressure apparatus

Journal of Geophysical Research, 1975-04, Vol.80 (11), p.1519-1525

1975

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Lithologische Kartierung als Teil der Bauforschung Kapelle in der Burgruine Kropfsberg/Tirol

Zeitschrift der Deutschen Gesellschaft für Geowissenschaften, 2005-04, Vol.156 (1), p.197-203

2005

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The low-high quartz and quartz-coesite transition to 40 kbar between 600° and 1600°C and some reconnaissance data on the effect of NaAlO2 component on the low quartz-coesite transition

Journal of Geophysical Research: Solid Earth, 1980-12, Vol.85 (B12), p.6983-6990

1980

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Initial stages of carbonate weathering : climate chamber studies under realistic pollution conditions: Monument Future: Climate Change, Air Pollution, Decay and Conservation

Environmental geology (Berlin), 2008, Vol.56 (3-4), p.507-519

2008

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The low‐high quartz and quartz‐coesite transition to 40 kbar between 600° and 1600°C and some reconnaissance data on the effect of NaAlO 2 component on the low quartz‐coesite transition

Journal of Geophysical Research: Solid Earth, 1980-12, Vol.85 (B12), p.6983-6990

1980

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Phase relations for SrF2 TO 50 Kbars and 1900°C and its compression to 40Kbars at 25°C

The Journal of physics and chemistry of solids, 1980, Vol.41 (10), p.1157-1160

1980

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The phase relations of calcium fluoride (fluorite) to 60 kbars and 1800°C

The Journal of physics and chemistry of solids, 1978, Vol.39 (8), p.859-861

1978

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Differential volumetric analysis combined with monitoring of differential ultra-sound travel time, an approach for tracing fine-structural compression behaviour of solids: a study on MgO / periclase and polyethylene / PE up to 1.5 GPa at room temperature

Isobaric annealing of high-density amorphous ice between 0.3 and 1.9 GPa : in situ density values and structural changes

An experimental investigation of Na incorporation in cordierite in low P/high T metapelites

Cordierite under hydrostatic compression: Anomalous elastic behavior as a precursor for a pressure-induced phase transition

Initial stages of carbonate weathering: climate chamber studies under realistic pollution conditions

Geothermobarometry of a stilpnomelane–garnet-bearing metapegmatite: P–T constraints on the Eo-Alpine metamorphic overprint of the Austroalpine nappes north of the Tauern Window

The fine-structure of the dehydration boundary of brucite (Mg(OH)2) up to 3.5 GPa - indication of anomalous PVT behaviour of supercritical H2O

Moisture sorption behaviour of salt mixtures in porous stone

Experimental study of the dehydration reactions gypsum-bassanite and bassanite-anhydrite at high pressure: indication of anomalous behavior of H(2)O at high pressure in the temperature range of 50-300 degrees C

Experimental study of the dehydration reactions gypsum-bassanite and bassanite-anhydrite at high pressure: Indication of anomalous behavior of H2O at high pressure in the temperature range of 50–300°C

Experimental study of the dehydration reactions gypsum-bassaniteand bassanite-anhydrite at high pressure: Indication of anomalous behavior of H 2 O at high pressure in the temperature range of 50 - 300 ° C

Pore and hygric properties of porous limestones: a case study from Bratislava, Slovakia

Petrophysical properties of selected Quaternary building stones in western Austria

The melting curve of gold, silver, and copper to 60-Kbar pressure: A reinvestigation

A high-pressure phase transition in cordierite

The electrical conductivity of calcite between 300 and 1200 C at a CO2 pressure of 40 bars

A differential thermal analysis study of the high-temperature polymorphism of calcite at high pressure

Material properties, room-climate measurements and building history - an interdisciplinary project to set the conditions of restoration and re-use for the fortress of Kufstein, Tyrol, Austria

Low-friction cell for piston-cylinder high-pressure apparatus

Lithologische Kartierung als Teil der Bauforschung Kapelle in der Burgruine Kropfsberg/Tirol

The low-high quartz and quartz-coesite transition to 40 kbar between 600° and 1600°C and some reconnaissance data on the effect of NaAlO2 component on the low quartz-coesite transition

Initial stages of carbonate weathering : climate chamber studies under realistic pollution conditions: Monument Future: Climate Change, Air Pollution, Decay and Conservation

The low‐high quartz and quartz‐coesite transition to 40 kbar between 600° and 1600°C and some reconnaissance data on the effect of NaAlO 2 component on the low quartz‐coesite transition

Phase relations for SrF2 TO 50 Kbars and 1900°C and its compression to 40Kbars at 25°C

The phase relations of calcium fluoride (fluorite) to 60 kbars and 1800°C

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