Excited Nuclear States for K-41 (Potassium)

2016 ◽  
pp. 1245-1271
Author(s):  
S. I. Sukhoruchkin ◽  
Z. N. Soroko
Keyword(s):  
1978 ◽  
Vol 63 ◽  
pp. 323-326 ◽  
Author(s):  
Gérard Chambat ◽  
Jean-Paul Joseleau ◽  
Marielle Lapeyre ◽  
Andrée Lefebvre
Keyword(s):  

2019 ◽  
Author(s):  
Gaëtan Mertens ◽  
Iris Engelhard

Whether fear conditioning can take place without contingency awareness is a topic of continuing debate and conflicting findings have been reported in the literature. This systematic review provides a critical assessment of the available evidence. Specifically, a search was conducted to identify articles reporting fear conditioning studies in which the contingency between conditioned stimuli (CS) and the unconditioned stimulus (US) was masked, and in which CS-US contingency awareness was assessed. A systematic assessment of the methodological quality of the included studies (k = 41) indicated that most studies suffered from methodological limitations (i.e., poor masking procedures, poor awareness measures, researcher degrees of freedom, and trial-order effects), and that higher quality predicted lower odds of studies concluding in favor of contingency unaware fear conditioning. Furthermore, meta-analytic moderation analyses indicated no evidence for a specific set of conditions under which contingency unaware fear conditioning can be observed. Finally, funnel plot asymmetry and p-curve analysis indicated evidence for publication bias. We conclude that there is no convincing evidence for contingency unaware fear conditioning.


2015 ◽  
pp. 901-924
Author(s):  
S. I. Sukhoruchkin ◽  
Z. N. Soroko
Keyword(s):  

ChemInform ◽  
2010 ◽  
Vol 28 (50) ◽  
pp. no-no
Author(s):  
M. HOSHI ◽  
K. W. SHIMOTOHNO ◽  
T. ENDO ◽  
K. FURIHATA ◽  
H. SETO

1990 ◽  
Vol 27 (6) ◽  
pp. 811-817 ◽  
Author(s):  
E. Irving ◽  
M. T. Brandon

The Eocene Flores volcanics of the Insular Belt of southwestern Vancouver Island have U–Pb zircon ages of 51–50 Ma and a mean direction of magnetization (D, I) of 349.8°, 69.6 °(12 collecting sites, k = 41, α95 = 7.0°). The paleopole (81.1°N, 188.0°E, K = 20, A95 = 9.9°) agrees well with Early to Middle Eocene (54–48 Ma) paleopoles from cratonic North America and with two Early to Middle Eocene paleopoles (49 and 52 Ma) from the Intermontane Belt of the Canadian Cordillera. This shows that both the Vancouver Island section of the Insular Belt and the Intermontane Belt were in their present positions with respect to ancestral North America at that time. The data can be used as a reference for estimating tilts in bodies that themselves contain no geological evidence of paleohorizontal; as an illustration, tilts of two Eocene intrusions on Vancouver Island are estimated.


2015 ◽  
pp. 314-332
Author(s):  
S. I. Sukhoruchkin ◽  
Z. N. Soroko

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