Gary Stevens
Gary Stevens
Professor of Geology, Stellenbosch University
Email verificata su sun.ac.za - Home page
TitoloCitata daAnno
Diabetes self-management education and support in type 2 diabetes: a joint position statement of the American Diabetes Association, the American Association of Diabetes…
MA Powers, J Bardsley, M Cypress, P Duker, MM Funnell, AH Fischl, ...
The Diabetes Educator 43 (1), 40-53, 2017
832*2017
Melt production during granulite-facies anatexis: experimental data from “primitive” metasedimentary protoliths
G Stevens, JD Clemens, GTR Droop
Contributions to Mineralogy and Petrology 128 (4), 352-370, 1997
3401997
JAK2 p. V617F allele burden in myeloproliferative neoplasms one month after allogeneic stem cell transplantation significantly predicts outcome and risk of relapse
T Lange, A Edelmann, U Siebolts, R Krahl, C Nehring, N Jkel, M Cross, ...
Haematologica 98 (5), 722-728, 2013
260*2013
Experimental constraints on TTG petrogenesis: implications for Archean geodynamics
J Moyen, G Stevens
GEOPHYSICAL MONOGRAPH-AMERICAN GEOPHYSICAL UNION 164, 149, 2006
2432006
Oxidized BAL fluid proteins in patients with interstitial lung diseases
AG Lenz, U Costabel, KL Maier
European Respiratory Journal 9 (2), 307-312, 1996
234*1996
What controls chemical variation in granitic magmas?
JD Clemens, G Stevens
Lithos 134, 317-329, 2012
2212012
Selective peritectic garnet entrainment as the origin of geochemical diversity in S-type granites
G Stevens, A Villaros, JF Moyen
Geology 35 (1), 9-12, 2007
2042007
Record of mid-Archaean subduction from metamorphism in the Barberton terrain, South Africa
JF Moyen, G Stevens, A Kisters
Nature 442 (7102), 559, 2006
1962006
The enigmatic sources of I-type granites: the peritectic connexion
JD Clemens, G Stevens, F Farina
Lithos 126 (3-4), 174-181, 2011
1952011
Tectonic model for the evolution of the Limpopo Belt
C Roering, DD Van Reenen, CA Smit, JM Barton Jr, JH De Beer, ...
Precambrian Research 55 (1-4), 539-552, 1992
1801992
Fluid-absent melting and the roles of fluids in the lithosphere: a slanted summary?
G Stevens, JD Clemens
Chemical Geology 108 (1-4), 1-17, 1993
1461993
Diet and hepatic tumor formation
JA Miller, DL Miner, HP Rusch, CA Baumann
Cancer Research 1 (9), 699-708, 1941
118*1941
The trace element compositions of S-type granites: evidence for disequilibrium melting and accessory phase entrainment in the source
A Villaros, G Stevens, JF Moyen, IS Buick
Contributions to Mineralogy and Petrology 158 (4), 543-561, 2009
1122009
Metamorphism of the granite–greenstone terrane south of the Barberton greenstone belt, South Africa: an insight into the tectono-thermal evolution of the ‘lower’portions of the…
A Dziggel, G Stevens, M Poujol, CR Anhaeusser, RA Armstrong
Precambrian Research 114 (3-4), 221-247, 2002
1052002
Chemical structure in granitic magmas–a signal from the source?
JD Clemens, PA Helps, G Stevens
Earth and Environmental Science Transactions of the Royal Society of…, 2009
982009
Thermal-metamorphic signature of an impact event in the Vredefort dome, South Africa
RL Gibson, W Uwe Reimold, G Stevens
Geology 26 (9), 787-790, 1998
951998
Isotopic variations in S-type granites: an inheritance from a heterogeneous source?
A Villaros, IS Buick, G Stevens
Contributions to Mineralogy and Petrology 163 (2), 243-257, 2012
932012
Stabilization of the southern portion of the So Francisco craton, SE Brazil, through a long-lived period of potassic magmatism
R Romano, C Lana, FF Alkmim, G Stevens, R Armstrong
Precambrian Research 224, 143-159, 2013
892013
Metamorphism and exhumation of the basal parts of the Barberton greenstone belt, South Africa: Constraining the rates of Mesoarchaean tectonism
JFA Diener, G Stevens, AFM Kisters, M Poujol
Precambrian Research 143 (1-4), 87-112, 2005
882005
Barberton (South Africa) TTG magmas: geochemical and experimental constraints on source-rock petrology, pressure of formation and tectonic setting
JD Clemens, LM Yearron, G Stevens
Precambrian Research 151 (1-2), 53-78, 2006
872006
Il sistema al momento non pu eseguire l'operazione. Riprova pi tardi.
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