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Neoproterozoic iron formation: An evaluation of its temporal, environmental and tectonic significance

Chemical geology, 2013-12, Vol.362, p.232-249

2013

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Geochemistry of Neoproterozoic black shales from Svalbard: Implications for oceanic redox conditions spanning Cryogenian glaciations

Chemical geology, 2015-12, Vol.417, p.383-393

2015

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Photophysics of dopamine-modified quantum dots and effects on biological systems

Nature materials, 2006-05, Vol.5 (5), p.409-417

2006

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Sulfur isotope and trace element data from ore sulfides in the Noranda district (Abitibi, Canada): implications for volcanogenic massive sulfide deposit genesis

Mineralium deposita, 2015-06, Vol.50 (5), p.591-606

2015

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The Magmatic Architecture of Taney Seamount-A, NE Pacific Ocean

Journal of petrology, 2015-06, Vol.56 (6), p.1037-1067

2015

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Metal ion levels in the blood of patients after hip resurfacing: a comparison between twenty-eight and thirty-six-millimeter-head metal-on-metal prostheses

Journal of bone and joint surgery. American volume, 2008-08, Vol.90 Suppl 3, p.142

2008

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Experimental partitioning of uranium between liquid iron sulfide and liquid silicate: Implications for radioactivity in the Earth’s core

Geochimica et cosmochimica acta, 2006-01, Vol.70 (6), p.1537-1547

2006

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Thermal History of the Bandelier Magmatic System: Evidence for Magmatic Injection and Recharge at 1.61 Ma as Revealed by Cathodoluminescence and Titanium Geothermometry

The Journal of geology, 2009-09, Vol.117 (5), p.469-485

2009

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A critical evaluation of pressure scales at high temperatures by in situ X-ray diffraction measurements

Physics of the earth and planetary interiors, 2004-06, Vol.143, p.515-526

2004

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Trace element partitioning between majoritic garnet and silicate melt at 10–17 GPa: Implications for deep mantle processes

Lithos, 2012-09, Vol.148, p.128-141

2012

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Evidence for lithium-aluminosilicate supersaturation of pegmatite-forming melts

Contributions to mineralogy and petrology, 2015-07, Vol.170 (1), p.255-16, Article 4

2015

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High-pressure experimental trace-element partitioning between clinopyroxene and basaltic melts

Chemical geology, 1994-11, Vol.117 (1), p.127-147

1994

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Textural Entrapment of Core-Forming Melts

Science (American Association for the Advancement of Science), 1996-04, Vol.272 (5261), p.530-533

1996

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Aluminum-dependent trace element partitioning in clinopyroxene

Contributions to mineralogy and petrology, 2008-10, Vol.156 (4), p.439-451

2008

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Melt-rock interaction near the Moho: Evidence from crystal cargo in lavas from near-ridge seamounts

Geochimica et cosmochimica acta, 2016-10, Vol.191, p.139-164

2016

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Precise water level measurements using low-cost GNSS antenna arrays

Earth surface dynamics, 2021-06, Vol.9 (3), p.673-685

2021

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Interconnectivity of carbonate melt at low melt fraction

Earth and planetary science letters, 1995-07, Vol.133 (3), p.423-437

1995

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Trace element partitioning between majoritic garnet and silicate melt at 10–17GPa: Implications for deep mantle processes

Lithos, 2012-09, Vol.148, p.128-141

2012

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Erratum to: “Trace element partitioning between majoritic garnet and silicate melt at 10–17 GPa: Implications for deep mantle processes” [Lithos 148 (2012) 128–141]

Lithos, 2012-12, Vol.154, p.406-406

2012

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A new capsule technique for hydrothermal experiments using the piston-cylinder apparatus

The American mineralogist, 1992-10, Vol.77 (9-10), p.1080-1086

1992

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Thermoelastic properties of (Mg 0.64Fe 0.36)O ferropericlase based on in situ X-ray diffraction to 26.7 GPa and 2173 K

Physics of the earth and planetary interiors, 2005-07, Vol.151 (1), p.163-176

2005

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Multicomponent diffusion and convection in molten MgO-Al2O3-SiO2

Geochimica et cosmochimica acta, 1998-06, Vol.62 (11), p.1985-1991

1998

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Thermoelastic properties of (Mg0.64Fe0.36)O ferropericlase based on in situ X-ray diffraction to 26.7GPa and 2173K

Physics of the earth and planetary interiors, 2005-07, Vol.151 (1-2), p.163-176

2005

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Multicomponent diffusion and convection in molten MgO-Al 2O 3-SiO 2

Geochimica et cosmochimica acta, 1998, Vol.62 (11), p.1985-1991

1998

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The interfacial energy properties of sodium carbonate and iron-nickel sulfide melts in a polycrystalline olivine matrix at high pressure and temperature

Minarik, William Grant

1994

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Neoproterozoic iron formation: An evaluation of its temporal, environmental and tectonic significance

Geochemistry of Neoproterozoic black shales from Svalbard: Implications for oceanic redox conditions spanning Cryogenian glaciations

Photophysics of dopamine-modified quantum dots and effects on biological systems

Sulfur isotope and trace element data from ore sulfides in the Noranda district (Abitibi, Canada): implications for volcanogenic massive sulfide deposit genesis

The Magmatic Architecture of Taney Seamount-A, NE Pacific Ocean

Metal ion levels in the blood of patients after hip resurfacing: a comparison between twenty-eight and thirty-six-millimeter-head metal-on-metal prostheses

Experimental partitioning of uranium between liquid iron sulfide and liquid silicate: Implications for radioactivity in the Earth’s core

Thermal History of the Bandelier Magmatic System: Evidence for Magmatic Injection and Recharge at 1.61 Ma as Revealed by Cathodoluminescence and Titanium Geothermometry

A critical evaluation of pressure scales at high temperatures by in situ X-ray diffraction measurements

Trace element partitioning between majoritic garnet and silicate melt at 10–17 GPa: Implications for deep mantle processes

Evidence for lithium-aluminosilicate supersaturation of pegmatite-forming melts

High-pressure experimental trace-element partitioning between clinopyroxene and basaltic melts

Textural Entrapment of Core-Forming Melts

Aluminum-dependent trace element partitioning in clinopyroxene

Melt-rock interaction near the Moho: Evidence from crystal cargo in lavas from near-ridge seamounts

Precise water level measurements using low-cost GNSS antenna arrays

Interconnectivity of carbonate melt at low melt fraction

Trace element partitioning between majoritic garnet and silicate melt at 10–17GPa: Implications for deep mantle processes

Erratum to: “Trace element partitioning between majoritic garnet and silicate melt at 10–17 GPa: Implications for deep mantle processes” [Lithos 148 (2012) 128–141]

A new capsule technique for hydrothermal experiments using the piston-cylinder apparatus

Thermoelastic properties of (Mg 0.64Fe 0.36)O ferropericlase based on in situ X-ray diffraction to 26.7 GPa and 2173 K

Multicomponent diffusion and convection in molten MgO-Al2O3-SiO2

Thermoelastic properties of (Mg0.64Fe0.36)O ferropericlase based on in situ X-ray diffraction to 26.7GPa and 2173K

Multicomponent diffusion and convection in molten MgO-Al 2O 3-SiO 2

The interfacial energy properties of sodium carbonate and iron-nickel sulfide melts in a polycrystalline olivine matrix at high pressure and temperature

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