Zobrazeno 1 - 10
of 48
pro vyhledávání: '"Hatten, S"'
Autor:
Perkins, J., Dundee, B., Obousy, R., Hatten, S., Kasper, E., Robinson, M., Sloan, C., Stone, K., Cleaver, G.
Publikováno v:
Phys.Rev.D75:026007,2007
For the weakly coupled heterotic string (WCHS) there is a well-known factor of twenty conflict between the minimum string coupling unification scale, Lambda_H ~5x10^(17) GeV, and the projected MSSM unification scale, Lambda_U ~ 2.5x10^(16) GeV, assum
Externí odkaz:
http://arxiv.org/abs/hep-ph/0510141
Autor:
Yoder, Hatten S.
Publikováno v:
Proceedings of the American Philosophical Society, 2002 Mar 01. 146(1), 37-55.
Externí odkaz:
https://www.jstor.org/stable/1558155
Autor:
Cody, George D., Boctor, Nabil Z., Filley, Timothy R., Hazen, Robert M., Scott, James H., Sharma, Anurag, Yoder, Hatten S.
Publikováno v:
Science, 2000 Aug . 289(5483), 1337-1340.
Externí odkaz:
https://www.jstor.org/stable/3077627
Autor:
Perkins, J., Dundee, B., Obousy, R., Hatten, S., Kasper, E., Robinson, M., Sloan, C., Stone, K., Cleaver, G.
Publikováno v:
ETSU Faculty Works.
For the weakly coupled heterotic string (WCHS) there is a well-known factor of 20 conflict between the minimum string coupling unification scale, ΛH∼5×1017GeV, and the projected minimal supersymmetric standard model (MSSM) gauge coupling unificat
Externí odkaz:
https://dc.etsu.edu/etsu-works/17882
Autor:
Yoder,, Hatten S.
Publikováno v:
Proceedings of the American Philosophical Society, 1982 Jun 01. 126(3), 229-241.
Externí odkaz:
https://www.jstor.org/stable/986509
Autor:
Yoder,, Hatten S.
Publikováno v:
Earth Sciences History, 1992 Jan 01. 11(1), 45-55.
Externí odkaz:
https://www.jstor.org/stable/24138588
Autor:
Yoder, Hatten S.
Publikováno v:
The Journal of Geology, 1952 Jul 01. 60(4), 364-374.
Externí odkaz:
https://www.jstor.org/stable/30058217
Autor:
Yoder, Hatten S.
Publikováno v:
The Journal of Geology, 1952 Nov 01. 60(6), 586-593.
Externí odkaz:
https://www.jstor.org/stable/30057029
Autor:
Yoder, Hatten S.
Publikováno v:
The Journal of Geology, 1950 May 01. 58(3), 221-253.
Externí odkaz:
https://www.jstor.org/stable/30068022
Publikováno v:
American Mineralogist. 80:534-548
Experiments have been carried out from 500 to 1200 °C, 1 atm to 10 kbar, and fH2from that of the IQF buffer to air, to quantify the variation of Fe oxy-component content in a titanian pargasite megacryst amphibole from Vulcan's Throne, Arizona. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::db20c05e6449435b221a1eaceaf1945e
https://doi.org/10.2138/am-1995-5-613
https://doi.org/10.2138/am-1995-5-613