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High Pressure Research
An International Journal
Volume 26, 2006 - Issue 3
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Original Articles

Effect of gasketing and assembly design: a novel 10/3.5 mm multi-anvil assembly reaching perovskite pressures

A. J. Stewart Institute for Mineralogy and Petrology, Clausiusstrasse 25, ETH Zurich, CH 8092, Zurich, SwitzerlandCorrespondence[email protected]
,
W. Van Westrenen Faculty of Earth and Life Sciences, De Boelelaan 1085, Vrije Universiteit, 1081 HV, Amsterdam, The Netherlands
,
M. W. Schmidt Institute for Mineralogy and Petrology, Clausiusstrasse 25, ETH Zurich, CH 8092, Zurich, Switzerland
&
E. Melekhova Institute for Mineralogy and Petrology, Clausiusstrasse 25, ETH Zurich, CH 8092, Zurich, Switzerland
Pages 293-299 | Received 05 Apr 2006, Published online: 26 Jan 2007

Citations (15)

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Emil Stoyanov, Ulrich Häussermann & Kurt Leinenweber. (2010) Large-volume multianvil cells designed for chemical synthesis at high pressures. High Pressure Research 30:1, pages 175-189.
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Articles from other publishers (14)

Tobias Grützner, Stephan Klemme, Arno Rohrbach, Fernanda Gervasoni & Jasper Berndt. (2018) The effect of fluorine on the stability of wadsleyite: Implications for the nature and depths of the transition zone in the Earth's mantle. Earth and Planetary Science Letters 482, pages 236-244.
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Nathan Kang, Max W. Schmidt, Stefano Poli, James A. D. Connolly & Ettore Franzolin. (2016) Melting relations in the system FeCO3–MgCO3 and thermodynamic modelling of Fe–Mg carbonate melts. Contributions to Mineralogy and Petrology 171:8-9.
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C. H. Wijbrans, A. Rohrbach & S. Klemme. (2016) An experimental investigation of the stability of majoritic garnet in the Earth’s mantle and an improved majorite geobarometer. Contributions to Mineralogy and Petrology 171:5.
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Angelika D. Rosa, Carmen Sanchez-Valle, Jingyun Wang & Ashima Saikia. (2015) Elasticity of superhydrous phase B, seismic anomalies in cold slabs and implications for deep water transport. Physics of the Earth and Planetary Interiors 243, pages 30-43.
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Nathan Kang, Max W. Schmidt, Stefano Poli, Ettore Franzolin & James A.D. Connolly. (2015) Melting of siderite to 20GPa and thermodynamic properties of FeCO3-melt. Chemical Geology 400, pages 34-43.
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Sujoy Ghosh & Max W. Schmidt. (2014) Melting of phase D in the lower mantle and implications for recycling and storage of H 2 O in the deep mantle. Geochimica et Cosmochimica Acta 145, pages 72-88.
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A. D. Rosa, M. Mezouar, G. Garbarino, P. Bouvier, S. Ghosh, A. Rohrbach & C. Sanchez-Valle. (2013) Single-crystal equation of state of phase D to lower mantle pressures and the effect of hydration on the buoyancy of deep subducted slabs. Journal of Geophysical Research: Solid Earth 118:12, pages 6124-6133.
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Angelika D. Rosa, Carmen Sanchez-Valle, Carole Nisr, Shaun R. Evans, Regis Debord & Sébastien Merkel. (2013) Shear wave anisotropy in textured phase D and constraints on deep water recycling in subduction zones. Earth and Planetary Science Letters 377-378, pages 13-22.
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Daniele Grassi, Max W. Schmidt & Detlef Günther. (2012) Element partitioning during carbonated pelite melting at 8, 13 and 22GPa and the sediment signature in the EM mantle components. Earth and Planetary Science Letters 327-328, pages 84-96.
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A. Shatskiy, T. Katsura, K.D. Litasov, A.V. Shcherbakova, Y.M. Borzdov, D. Yamazaki, A. Yoneda, E. Ohtani & E. Ito. (2011) High pressure generation using scaled-up Kawai-cell. Physics of the Earth and Planetary Interiors 189:1-2, pages 92-108.
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Daniele Grassi & Max W. Schmidt. (2011) The Melting of Carbonated Pelites from 70 to 700 km Depth. Journal of Petrology 52:4, pages 765-789.
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Arno Rohrbach & Max W. Schmidt. (2011) Redox freezing and melting in the Earth’s deep mantle resulting from carbon–iron redox coupling. Nature 472:7342, pages 209-212.
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Andrew J. Stewart, Wim van Westrenen, Max W. Schmidt & D. Günther. (2009) Minor element partitioning between fcc Fe metal and Fe–S liquid at high pressure: The role of crystal lattice strain. Earth and Planetary Science Letters 284:3-4, pages 302-309.
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A. J. Stewart & M. W. Schmidt. (2007) Sulfur and phosphorus in the Earth's core: The Fe‐P‐S system at 23 GPa. Geophysical Research Letters 34:13.
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