Intragrain pinning strength depth dependence of 2223 (Bi,Pb)‐based high criticalTcsuperconducting ceramics made by a vitreous route

1995 ◽  
Vol 77 (7) ◽  
pp. 3560-3562 ◽  
Author(s):  
An Dang ◽  
P. A. Godelaine ◽  
Ph. Vanderbemden ◽  
R. Cloots ◽  
M. Ausloos
Keyword(s):  
Depth Dependence

Depth dependence of rupture velocity in deep earthquakes

2011 ◽  
Vol 38 (5) ◽  
pp. n/a-n/a ◽  
Author(s):  
Mitsuru Suzuki ◽  
Yuji Yagi
Keyword(s):  
Rupture Velocity ◽  
Depth Dependence ◽  
Deep Earthquakes

Depth dependence of 10Be and 26Al production rates in the iron meteorite grant

1987 ◽  
Vol 29 (1-2) ◽  
pp. 262-265 ◽  
Author(s):  
Thomas Graf ◽  
Stephan Vogt ◽  
Georges Bonani ◽  
Ulrich Herpers ◽  
Peter Signer ◽  
...  
Keyword(s):  
Iron Meteorite ◽  
Production Rates ◽  
Depth Dependence

Shear velocity from differential travel times of short-period ScS-P in New Hebrides, Fiji-Tonga, and Banda Sea regions

1975 ◽  
Vol 65 (6) ◽  
pp. 1787-1796
Author(s):  
Mansur A. Choudhury ◽  
Georges Poupinet ◽  
Guy Perrier
Keyword(s):  
Upper Mantle ◽  
Focal Depth ◽  
Shear Velocity ◽  
Mean Value ◽  
Travel Times ◽  
Velocity Models ◽  
Depth Dependence ◽  
Short Period ◽  
New Hebrides ◽  
The Antarctic

abstract Behavior of P, S and ScS residuals as well as those of differential travel times of ScS-P from the Jeffreys-Bullen tables are analyzed. The phases have been read from short-period records of the Antarctic station, Dumont d'Urville (DRV); the earthquakes originating in New Hebrides, Fiji-Tonga, and Banda Sea regions. P residuals from all regions show a mean value of about −1 sec. On the contrary, S and ScS residuals, well correlated among themselves, show important regional as well as focal-depth dependence. ScS-P residuals from shallow and intermediate shocks are largely positive for New Hebrides and largely negative for Banda Sea; those from intermediate shocks are moderately positive for Fiji-Tonga. The anomalies disappear at depths greater than about 200 km. Upper mantle shear velocity models are presented for the three regions. The models are discussed in relation to a sinking lithosphere.

scholarly journals Low‐frequency propagation across the East Greenland and Frontal Zone: Depth dependence of transmission loss

1987 ◽  
Vol 82 (S1) ◽  
pp. S31-S31
Author(s):  
Leonard E. Mellberg ◽  
D. N. Connors ◽  
D. G. Browning ◽  
G. Botseas ◽  
O. M. Johannessen
Keyword(s):  
Frontal Zone ◽  
Transmission Loss ◽  
Low Frequency ◽  
East Greenland ◽  
Depth Dependence ◽  
Zone Depth

Diameter to depth dependence of impact craters

1980 ◽  
Vol 28 (6) ◽  
pp. 567-573 ◽  
Author(s):  
K. Nagel ◽  
H. Fechtig
Keyword(s):  
Impact Craters ◽  
Depth Dependence

Equal-loudness contours in water and its depth dependence

1998 ◽  
Vol 55 (1) ◽  
pp. 1-12 ◽  
Author(s):  
Kensei Oimatsu ◽  
Kazuoki Kuramoto ◽  
Shin’ya Kuwahara ◽  
Shizuma Yamaguchi
Keyword(s):  
Depth Dependence

scholarly journals Measured depth-dependence of waveguide invariant in shallow water with a summer profile

2016 ◽  
Vol 139 (6) ◽  
pp. EL184-EL189 ◽  
Author(s):  
Altan Turgut ◽  
Laurie T. Fialkowski ◽  
Jeffrey A. Schindall
Keyword(s):  
Shallow Water ◽  
Depth Dependence ◽  
Waveguide Invariant
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