Judith Hannah
Judith Hannah
Colorado State University & Universitetet i Oslo
Verified email at
Cited by
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Dating the rise of atmospheric oxygen
A Bekker, HD Holland, PL Wang, D Rumble Iii, HJ Stein, JL Hannah, ...
Nature 427 (6970), 117-120, 2004
The remarkable Re–Os chronometer in molybdenite: how and why it works
HJ Stein, RJ Markey, JW Morgan, JL Hannah, A ScherstÚn
Terra Nova 13 (6), 479-486, 2001
Subgrain-scale decoupling of Re and 187Os and assessment of laser ablation ICP-MS spot dating in molybdenite
H Stein, A ScherstÚn, J Hannah, R Markey
Geochimica et Cosmochimica Acta 67 (19), 3673-3686, 2003
Primitive Os and 2316 Ma age for marine shale: implications for Paleoproterozoic glacial events and the rise of atmospheric oxygen
JL Hannah, A Bekker, HJ Stein, RJ Markey, HD Holland
Earth and Planetary Science Letters 225 (1-2), 43-52, 2004
A 2.5 Ga porphyry Cu–Mo–Au deposit at Malanjkhand, central India: implications for Late Archean continental assembly
HJ Stein, JL Hannah, A Zimmerman, RJ Markey, SC Sarkar, AB Pal
Precambrian Research 134 (3-4), 189-226, 2004
Assessment of the 187Re decay constant by cross calibration of Re–Os molybdenite and U–Pb zircon chronometers in magmatic ore systems
D Selby, RA Creaser, HJ Stein, RJ Markey, JL Hannah
Geochimica et Cosmochimica Acta 71 (8), 1999-2013, 2007
Standardizing Re–Os geochronology: a new molybdenite reference material (Henderson, USA) and the stoichiometry of Os salts
R Markey, HJ Stein, JL Hannah, A Zimmerman, D Selby, RA Creaser
Chemical Geology 244 (1-2), 74-87, 2007
Tectonic configuration of the Apuseni–Banat—Timok–Srednogorie belt, Balkans-South Carpathians, constrained by high precision Re–Os molybdenite ages
A Zimmerman, HJ Stein, JL Hannah, D Koželj, K Bogdanov, T Berza
Mineralium Deposita 43, 1-21, 2008
Movement and origin of ore fluids in Climax-type systems
HJ Stein, JL Hannah
Geology 13 (7), 469-474, 1985
Re-Os study of Fe-Ti-V oxide and Fe-Cu-Ni sulfide deposits, Suwałki anorthosite massif, northeast Poland
JW Morgan, HJ Stein, JL Hannah, RJ Markey, J Wiszniewska
Mineralium Deposita 35, 391-401, 2000
Molybdenum isotope variations in molybdenite: Vapor transport and Rayleigh fractionation of Mo
JL Hannah, HJ Stein, ME Wieser, JR De Laeter, MD Varner
Geology 35 (8), 703-706, 2007
Hot acidic Late Permian seas stifle life in record time
S Georgiev, HJ Stein, JL Hannah, B Bingen, HM Weiss, S Piasecki
Earth and Planetary Science Letters 310 (3-4), 389-400, 2011
Cause of Upper Triassic climate crisis revealed by Re–Os geochemistry of Boreal black shales
G Xu, JL Hannah, HJ Stein, A M°rk, JO Vigran, B Bingen, DL Schutt, ...
Palaeogeography, Palaeoclimatology, Palaeoecology 395, 222-232, 2014
Digestion methods for trace element measurements in shales: Paleoredox proxies examined
G Xu, JL Hannah, B Bingen, S Georgiev, HJ Stein
Chemical Geology 324, 132-147, 2012
A double spike for osmium analysis of highly radiogenic samples
R Markey, JL Hannah, JW Morgan, HJ Stein
Chemical Geology 200 (3-4), 395-406, 2003
Re–Os geochronology of Arctic black shales to evaluate the Anisian–Ladinian boundary and global faunal correlations
G Xu, JL Hannah, HJ Stein, B Bingen, G Yang, A Zimmerman, ...
Earth and Planetary Science Letters 288 (3-4), 581-587, 2009
Age relationships and depositional environments of Paleozoic strata, northern Sierra Nevada, California
JL Hannah, EM Moores
Geological Society of America Bulletin 97 (7), 787-797, 1986
Cadmium-isotopic evidence for increasing primary productivity during the Late Permian anoxic event
SV Georgiev, TJ Horner, HJ Stein, JL Hannah, B Bingen, M Rehkńmper
Earth and Planetary Science Letters 410, 84-96, 2015
Re–Os depositional age for Archean carbonaceous slates from the southwestern Superior Province: challenges and insights
G Yang, JL Hannah, A Zimmerman, HJ Stein, A Bekker
Earth and Planetary Science Letters 280 (1-4), 83-92, 2009
Chemical signals for oxidative weathering predict Re–Os isochroneity in black shales, East Greenland
S Georgiev, HJ Stein, JL Hannah, HM Weiss, B Bingen, G Xu, E Rein, ...
Chemical Geology 324, 108-121, 2012
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