Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Rabbe Sjöberg"'
Autor:
Nils-Axel Mörner, Rabbe Sjöberg
Publikováno v:
International Journal of Speleology, Vol 47, Iss 3, Pp 393-405 (2018)
Sweden has thousands of caves cut into the bedrock, two thirds of which occur in the crystalline bedrock, and hence represent pseudokarst phenomena. The formation of these caves can only be understood in terms of paleoseismics. In this paper, we revi
Externí odkaz:
https://doaj.org/article/d26e575d37e24afab3ec0187f72f65ec
Autor:
Rabbe Sjöberg
Publikováno v:
International Journal of Speleology, Vol 49, Iss 3, Pp 271-272 (2020)
Externí odkaz:
https://doaj.org/article/51b5e704d33547159da2897b7250a4b2
Autor:
Therese Sallstedt, Magnus Ivarsson, Johannes Lundberg, Rabbe Sjöberg, Juan Ramón Vidal Romaní
Publikováno v:
International Journal of Speleology, Vol 43, Iss 3, Pp 305-313 (2014)
Tjuv-Antes grotta (Tjuv-Ante's Cave) located in northern Sweden is a round-abraded sea cave ('tunnel cave'), about 30 m in length, formed by rock-water abrasion in a dolerite dyke in granite gneiss. Abundant speleothems are restricted to the inner, m
Externí odkaz:
https://doaj.org/article/d86d946ed4f2492ba0ee6a4041c160b2
Autor:
Johannes Lundberg, Rabbe Sjöberg, Therese Sallstedt, Magnus Ivarsson, Juan Ramón Vidal Romaní
Publikováno v:
International Journal of Speleology, Vol 43, Iss 3, Pp 305-313 (2014)
Sallstedt, T, Ivarsson, M, Lundberg, J, Sjoberg, R & Romani, J R V 2014, ' Speleothem and biofilm formation in a granite/dolerite cave, Northern Sweden ', International Journal of Speleology, vol. 43, no. 3, pp. 305-313 . https://doi.org/10.5038/1827-806x.43.3.7
Sallstedt, T, Ivarsson, M, Lundberg, J, Sjoberg, R & Romani, J R V 2014, ' Speleothem and biofilm formation in a granite/dolerite cave, Northern Sweden ', International Journal of Speleology, vol. 43, no. 3, pp. 305-313 . https://doi.org/10.5038/1827-806x.43.3.7
Tjuv-Antes grotta (Tjuv-Ante’s Cave) located in northern Sweden is a round-abraded sea cave (‘tunnel cave’), about 30 m in length, formed by rock-water abrasion in a dolerite dyke in granite gneiss. Abundant speleothems are restricted to the in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6b48e33e1e61ddb37394c8e9ad98fe1a
http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-386
http://urn.kb.se/resolve?urn=urn:nbn:se:nrm:diva-386
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
Autor:
Rabbe Sjöberg, William C. Mahaney
Publikováno v:
Zeitschrift für Geomorphologie. 37:337-350
Autor:
Rabbe Sjöberg
Publikováno v:
Zeitschrift für Geomorphologie. 35:305-320