Zobrazeno 1 - 10
of 24
pro vyhledávání: '"I.P. Kosminskaya"'
Publikováno v:
Tectonophysics. 189:29-35
An inverse tomographic problem of the construction of a 3-D velocity structure has been solved for depths of 10, 20, 30, and 40 km using the P-wave arrivals registered by the seismic array in southern Finland and on the DSS lines Sveka (1981) and Bal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b038ca2584f43f829ba41595323de331
https://doi.org/10.1016/0040-1951(91)90485-b
https://doi.org/10.1016/0040-1951(91)90485-b
Autor:
V.T. Ionkis, I.P. Kosminskaya, H. Korhonen, A.F. Buyanov, V. Burmin, Timo Tiira, N.V. Sharov, I. Azbel, U. Luosto
Publikováno v:
Geophysical Journal International. 101:89-110
SUMMARY The 430 km long DSS Baltic profile in SE Finland runs through the Rapakivi intrusion, the Svecokarelian geosynclinal complex, including the Ladoga-Bothnian Bay zone, and the Archean basement complex. A brief description of field operations in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::724fb32d0a8c93f215b1513a224f6ad8
https://doi.org/10.1111/j.1365-246x.1990.tb00760.x
https://doi.org/10.1111/j.1365-246x.1990.tb00760.x
Publikováno v:
International Geology Review. 19:11-24
This paper presents the results of the seismic observations carried out in1972 under the international NASP (North Atlantic Seismic Project) along profilesrunning between Iceland, the Faeroe and Shetland islands, arid Scotland.The crustal structure i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ccb1b7c00c168f0e40e7e37371f5e3b
https://doi.org/10.1080/00206817709470991
https://doi.org/10.1080/00206817709470991
Autor:
I.P. Kosminskaya, N. I. Pavlenkova
Publikováno v:
Tectonophysics. 59:307-320
Analogies are drawn between continental and continental margin structures on the basis of seismic data on the crustal structure of Eurasia and its Atlantic margins. Crustal thinning from the inner parts of the continent to its margins is observed to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b7cfbe7680b8455e61e04a925b7659fb
https://doi.org/10.1016/0040-1951(79)90052-0
https://doi.org/10.1016/0040-1951(79)90052-0
Publikováno v:
Tectonophysics. 10:517-538
Many geophysical characteristics of the Caspian and Black Seas' deep basins are similar, having: suboceanic type of the crust, low average seismic velocity, absence of earthquakes and relatively small variation of magnetic anomalies. However, the sed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c471a03710590d988de643208c3899f9
https://doi.org/10.1016/0040-1951(70)90042-9
https://doi.org/10.1016/0040-1951(70)90042-9
Publikováno v:
Tectonophysics. 20:147-151
The main results of seismic investigations in the transition zone from the Asian continent to the Pacific Ocean and in several regions of the Pacific Ocean are reported briefly. One of the most surprising findings is the existence of a layer with a P
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4ad358fb080276aac887259d8298fb4d
https://doi.org/10.1016/0040-1951(73)90104-2
https://doi.org/10.1016/0040-1951(73)90104-2
Autor:
C.L. Drake, I.P. Kosminskaya
Publikováno v:
Tectonophysics. 7:363-384
A considerable body of data has been collected on the continental margins of the world but the greater part of these data are concentrated in a few areas and the remaining areas have received only limited attention. This is especially true of data de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::deda0f7163c051067bbe2007cc71e5e4
https://doi.org/10.1016/0040-1951(69)90007-9
https://doi.org/10.1016/0040-1951(69)90007-9
Publikováno v:
Tectonophysics. 10:561-571
Models are presented which illustrate the various methods used for the determination of the thickness and nature of deep seismic boundaries according to the observed amplitude and frequency of subcritical reflected waves. From this study it becomes c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::150688120d6632448f3df9ddecd1420a
https://doi.org/10.1016/0040-1951(70)90045-4
https://doi.org/10.1016/0040-1951(70)90045-4
Publikováno v:
Tectonophysics. 13:309-323
Progress in different aspects of explosion seismology during the Upper Mantle Project period is discussed. In the method of field operation new observational systems have been developed, including continuous seismic depth-profiling, separate sounding
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1026a63f6ac56497cbba1b98702a13d7
https://doi.org/10.1016/0040-1951(72)90025-x
https://doi.org/10.1016/0040-1951(72)90025-x
