Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Per Einar Tröften"'
Autor:
Christian Bronge, Nils-Axel Mörner, Alf Sidén, Ole Kvamsdal, Rabbe Sjöberg, Per Einar Tröften, Sue Dawson, Douglas Grant
Publikováno v:
Quaternary Science Reviews. 19:1461-1468
The Iggeesund event is an example of the high seismicity which occurred in Fennoscandia during deglaciation as a function of the high rate of glacial isostatic uplift. This event is dated to varve 9663 BP. The Iggesund–Hudiksvall area is represente
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::871fd2a1a73a18d23b8e3fdfed323c69
https://doi.org/10.1016/s0277-3791(00)00095-0
https://doi.org/10.1016/s0277-3791(00)00095-0
Autor:
Per-Einar Tröften
Publikováno v:
Sedimentary Geology. 130:167-181
Geological structures suggest that the Fennoscandian Shield was subjected to a higher seismicity at the end of the last glaciation than today. This article demonstrates the use of varved clay chronology for dating paleoseismic events. It is argued th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::14b7f9ec03b33cbf52b8d9b98f1ddc99
https://doi.org/10.1016/s0037-0738(99)00109-8
https://doi.org/10.1016/s0037-0738(99)00109-8
Autor:
Per-Einar Tröften, Nils-Axel Mörner
Publikováno v:
Journal of Geodynamics. 24:249-258
Structures in bedrock and sediments suggest that the Fennoscandian Shield was subjected to a higher seismicity at the end of the last glaciation than it is today. We suggest that the annual varves of the glacial clays document this seismicity. In the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9db992e0e0d3711f1af2dc2739628d37
https://doi.org/10.1016/s0264-3707(96)00031-2
https://doi.org/10.1016/s0264-3707(96)00031-2