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1.	Halliday, A, et al. (author) Status update and interim results from the asymptomatic carotid surgery trial-2 (ACST-2) 2013 In: European journal of vascular and endovascular surgery : the official journal of the European Society for Vascular Surgery. - : Elsevier BV. - 1532-2165. ; 46:5, s. 510-518 Journal article (peer-reviewed)
2.	Grad, I, et al. (author) NANOG priming before full reprogramming may generate germ cell tumours 2011 In: European cells & materials. - : European Cells and Materials. - 1473-2262. ; 22, s. 258-74 Journal article (peer-reviewed)
3.	Camnasio, S, et al. (author) The first reported generation of several induced pluripotent stem cell lines from homozygous and heterozygous Huntington's disease patients demonstrates mutation related enhanced lysosomal activity 2012 In: Neurobiology of disease. - : Elsevier BV. - 1095-953X .- 0969-9961. ; 46:1, s. 41-51 Journal article (peer-reviewed)
4.	Grad, M., et al. (author) Seismic lithosphere-asthenosphere boundary beneath the Baltic Shield 2014 In: GFF. - : Informa UK Limited. - 1103-5897 .- 2000-0863. ; 136:4, s. 581-598 Journal article (peer-reviewed)abstract The problem of the existence of the asthenosphere for old Precambrian cratons is still discussed. In order to study the seismic lithosphere-asthenosphere boundary (LAB) beneath the Baltic Shield, we used records of nine local earthquakes with magnitudes ranging from 2.7 to 5.9. To model the LAB, original data were corrected for topography and Moho depth using a reference model with a 46-km-thick crust. For two northern events at Spitsbergen and Novaya Zemlya, we observe a low-velocity layer, 60-70-km-thick asthenosphere, and the LAB beneath Barents Sea was found at depth of c. 200km. Sections for other events show continuous first arrivals of P-waves with no evidence for "shadow zone" in the whole range of registration, which could either be interpreted as the absence of the asthenosphere beneath the central part of the Baltic Shield, or that the LAB in this area occurs deeper (>200km). The relatively thin low-velocity layer found beneath southern Sweden, 15km below the Moho, could be interpreted as small-scale lithospheric heterogeneities, rather than asthenosphere. Differentiation of the lower lithosphere velocities beneath the Baltic Shield could be interpreted as regional heterogeneity or as anisotropy of the Baltic Shield lithosphere, with high velocities approximately in the east-west direction, and slow velocities approximately in the south-north direction.

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Type of publication: journal article (4)

Type of content: peer-reviewed (4)

Author/Editor: Hovatta, O (2); Resch, T. (2); Sonesson, B. (2); Acosta, S. (2); Lindblad, B (2); Brown, J. (1); show more...; Liu, B. (1); Werner, M. (1); White, R. (1); Nagy, E. (1); Smith, D. (1); Kobayashi, A (1); Jackson, R. (1); Brown, A. (1); Brown, E. (1); James, A. (1); Schneider, R. (1); Scott, P. (1); Jenkins, A. (1); Klein, G (1); Pereira, A (1); Smith, A (1); Mitchell, J. (1); Kundu, A. (1); Malek, A. (1); Mariotti, C. (1); Lambert, D. (1); Martin, P. (1); Kere, J (1); Holst, J. (1); Kristmundsson, T. (1); Clifton, A. (1); Clarke, M (1); Blanco, E (1); Hill, M (1); Labate, C (1); Szabo, A. (1); Mitsiadis, TA (1); Jones, S. (1); Caso, V. (1); Toni, D. (1); Inoue, T. (1); Gottsäter, Anders (1); Zdanowski, Z (1); Guerra, M (1); Varga, D. (1); Nair, R (1); Mitchell, D (1); Polydorou, A (1); Welsh, S (1); show less...

University: Karolinska Institutet (3); Uppsala University (1); Lund University (1)

Language: English (4)

Research subject (UKÄ/SCB): Natural sciences (1); Medical and Health Sciences (1)

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