Author: Göran EricssonPublisher:
ISBN:
Category :
Languages : en
Pages : 170
Book Description
Production of heavy hypernuclei in antiproton annihilation:study of their decay in the fission channel
Author: Göran EricssonThe Reaction Pp [producing] Pp [ʻeta]
![The Reaction Pp [producing] Pp [ʻeta] PDF](https://books.google.com/books/content/images/frontcover/h9nqFHznuoEC?fife=w80-h100)
Author: Ulf SchuberthPublisher:
ISBN:
Category : Hadrons
Languages : en
Pages : 100
Book Description
Two Studies of the Galactic Chemical Evolution
Author: Sofia FeltzingPublisher: Coronet Books
ISBN:
Category : Science
Languages : en
Pages : 124
Book Description
The Geopotential
Author: Fang PengPublisher: Coronet Books
ISBN:
Category : Science
Languages : en
Pages : 170
Book Description
Abstract.
Hydrogeophysics of Tropical Africa
Author: Elónio MuiuanePublisher:
ISBN:
Category : Geophysics
Languages : en
Pages : 148
Book Description
Designing Space-time Codes Using Orthogonal Designs
Author: Girish GanesanPublisher:
ISBN:
Category : Radio
Languages : en
Pages : 172
Book Description
Seismic Attenuation, Shear Wave Anisotropy and Some Aspects of Fracturing in the Crystalline Rock of the Siljan Ring Area, Central Sweden
Author: Christopher JuhlinPublisher:
ISBN:
Category : Crystalline rocks
Languages : en
Pages : 170
Book Description
Holocene Environmental Change of Southern Öland, Sweden
Author: Kerstin Alm KüblerPublisher:
ISBN:
Category : Nature
Languages : en
Pages : 248
Book Description
Seismic Refraction Studies in the Baltic Shield Along the Fennolora Profile
Author: Md. Anowar HossainPublisher: Coronet Books
ISBN:
Category : Science
Languages : en
Pages : 152
Book Description
The crustal structure of the Baltic Shield has been studied based on travel-time analysis of P and S-wave data recorded from the Fennolora deep seismic sounding profile. The derived velocity-depth models show several low-velocity zones in the upper crust along the profile. The velocity reduction in these zones is to be less than 7%. crust with varying thicknesses of about 13, 11 and 19-26 km, respectively. The velocity gradient is lower in the middle crust compared to that in the upper and lower crust. The P velocity increases from about 6 km/s at the surface to 6.4 km/s in the middle crust. In the lower crust, velocity varies from about 6.7 km/s to 7.3 km/s. The Moho velocity, below the crust, is to be higher than 8 km/s. The depth to the Moho varies considerably, variations on the order of about 10 km. as high as 0.28 close to the surface and decreased to below 0.25 at about 2 km depth. In the deeper part of the upper crust and in the middle crust, o appears to be about 0.24 and increases slightly to about 0.25 in the lower crust. At the Moho boundary, o increases to about 0.26 and decreases to 0.25 beneath the Moho.
Digital Differentiating Filters and Model Based Fault Detection
Author: Bengt CarlssonPublisher:
ISBN:
Category : Electric fault location
Languages : en
Pages : 232
Book Description