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Thomas Ulrich
Thomas Ulrich
Verified email at geo.au.dk
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Year
metal fractionation between magmatic brine and vapor, determined by micro-analysis of fluid inclusions.
D Heinrich, C.A., Audétat, A., Ulrich, T., Frischknecht, R. and Günther
Geology 27, 755-758, 1999
6741999
Gold concentrations of magmatic brines and the metal budget of porphyry copper deposits
T Ulrich, D Guenther, CA Heinrich
Nature 399 (6737), 676-679, 1999
6491999
The evolution of a porphyry Cu-Au deposit, based on LA-ICP-MS analysis of fluid inclusions: Bajo de la Alumbrera, Argentina
T Ulrich, D Günther, CA Heinrich
Economic Geology 96 (8), 1743-1774, 2001
5852001
The evolution of a porphyry Cu-Au deposit, based on LA-ICP-MS analysis of fluid inclusions: Bajo de la Alumbrera, Argentina
T Ulrich, D Günther, CA Heinrich
Economic Geology 97 (8), 1889-1920, 2002
2412002
Geology and alteration geochemistry of the porphyry Cu-Au deposit at Bajo de la Alumbrera, Argentina
T Ulrich, CA Heinrich
Economic Geology 97 (8), 1865-1888, 2002
2262002
An experimental study of the solubility of molybdenum in H2O and KCl–H2O solutions from 500 C to 800 C, and 150 to 300 MPa
T Ulrich, J Mavrogenes
Geochimica et Cosmochimica Acta 72 (9), 2316-2330, 2008
2072008
Fluid evolution of the Yuchiling porphyry Mo deposit, East Qinling, China
N Li, T Ulrich, YJ Chen, TB Thomsen, V Pease, F Pirajno
Ore Geology Reviews 48, 442-459, 2012
1732012
Gold and metal enrichment in natural granitic melts during fractional crystallization
R Mustard, T Ulrich, VS Kamenetsky, T Mernagh
Geology 34 (2), 85-88, 2006
1472006
Imaging element-distribution patterns in minerals by laser ablation–inductively coupled plasma–mass spectrometry (LA–ICP–MS)
T Ulrich, BS Kamber, PJ Jugo, DK Tinkham
The Canadian Mineralogist 47 (5), 1001-1012, 2009
1202009
In situ trace element and sulfur isotope analysis of pyrite in a Paleoproterozoic gold placer deposit, Pardo and Clement Townships, Ontario, Canada
T Ulrich, DGF Long, BS Kamber, MJ Whitehouse
Economic Geology 106 (4), 667-686, 2011
1162011
Fluid inclusion study of the Wunugetu Cu–Mo deposit, Inner Mongolia, China
N Li, YJ Chen, T Ulrich, Y Lai
Mineralium Deposita 47 (5), 467-482, 2012
972012
Design and testing of a horizontal rock bed for high temperature thermal energy storage
KE Stefano Soprani, Fabrizio Marongiu, Ludvig Christensen, Ole Alm, Kenni ...
Applied Energy 251, 2019
722019
Different mineralization styles in a volcanic-hosted ore deposit: the fluid and isotopic signatures of the Mt Morgan Au–Cu deposit, Australia
T Ulrich, SD Golding, BS Kamber, K Zaw, A Taube
Ore Geology Reviews 22 (1-2), 61-90, 2003
642003
Geochemical modelling of a Zn–Pb skarn: Constraints from LA–ICP–MS analysis of fluid inclusions
M Bertelli, T Baker, JS Cleverley, T Ulrich
Journal of Geochemical Exploration 102 (1), 13-26, 2009
582009
Long‐Term Observations of Isotope Ratio Accuracy and Reproducibility Using Quadrupole ICP‐MS
T Ulrich, BS Kamber, JD Woodhead, LA Spencer
Geostandards and Geoanalytical Research 34 (2), 161-174, 2010
472010
Laterally extensive modified placer gold deposits in the Paleoproterozoic Mississagi Formation, Clement and Pardo Townships, Ontario
DGF Long, T Ulrich, BS Kamber
Canadian Journal of Earth Sciences 48 (5), 779-792, 2011
292011
A description of the world-class rare earth element deposit, Tanbreez, South Greenland
HK Schřnwandt, GB Barnes, T Ulrich
Rare Earths Industry, 73-85, 2016
282016
“Normal” to adakite-like arc magmatism associated with the El Abra porphyry copper deposit, Central Andes, Northern Chile
OM Rabbia, KJ Correa, LB Hernández, T Ulrich
International Journal of Earth Sciences 106 (8), 2687-2711, 2017
262017
Natural Obsidian Glass as an External Accuracy Reference Material in Laser Ablation‐Inductively Coupled Plasma‐Mass Spectrometry
T Ulrich, BS Kamber
Geostandards and Geoanalytical Research 37 (2), 169-188, 2013
222013
Metal fractionation between magmatic brine and vapour, and the link between porphyry-style and epithermal Cu-Au deposits
CA Heinrich, D Günther, A Audédat, T Ulrich, R Frischknecht
Geology 27, 755-758, 1999
211999
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