3-D density model of the crust of southern and central Finland obtained from joint interpretation of the SVEKALAPKO crustal P-wave velocity models and gravity data

Autor: M. Pirttijärvi, S. Elo, J. Yliniemi, S.E. Hjelt, Elena Kozlovskaya

Publikováno v: Geophysical Journal International. 158:827-848

3-D density model of the crust of southern and central Finland obtained from joint interpretation of the SVEKALAPKO crustal P-wave velocity models and gravity data

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::4999f55ac8e12e49ba6d1d2d339ee09f
https://doi.org/10.1111/j.1365-246x.2004.02363.x

Some characteristics of the conducting plate model in the inversion of geophysical electromagnetic data

Autor: S.E. Hjelt, Markku Pirttijärvi

Publikováno v: Inverse Problems. 16:1209-1223

A thin conducting plate has proven to be a versatile model in describing various relevant geologic features in crystalline bedrock. During the last few years we have developed several inversion codes for some commonly used electromagnetic (EM) measur

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::e718d54e0983676b01a0d17f4fe5df63
https://doi.org/10.1088/0266-5611/16/5/307

Electromagnetic studies in the Fennoscandian Shield—electrical conductivity of Precambrian crust

Autor: T. Korja, S.E. Hjelt

Publikováno v: Physics of the Earth and Planetary Interiors. 81:107-138

Electromagnetic (EM) investigations of the 1980s in the Fennoscandian (Baltic) Shield produced an unique and unified EM data set. Studies include regional investigations by the magnetovariational (MV) method with large lateral sampling distance, inve

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::5720707f2ea5de18912f1bc468ca4fe2
https://doi.org/10.1016/0031-9201(93)90127-u

Geoelectric studies and conductivity structures of the eastern and northern parts of the Baltic Shield

Autor: S.E. Hjelt

Publikováno v: Tectonophysics. 189:249-260

Large resistive regions (ideally having a horizontal size of about 200 km) are needed to study reliably the conductivity distribution of the lower crust of the Baltic (Scandinavian) Shield by deep electromagnetic (EM) methods. The overburden of the s

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::894a29667787ef1da40f225efa91ec52
https://doi.org/10.1016/0040-1951(91)90500-r

Complex lithospheric structure under the central Baltic Shield from surface wave tomography

Autor: Bruneton, M., H.A., Pedersen, Farra, V., N.T., Arndt, Vacher, P., Achauer, U., Alinaghi, A., Ansorge, J., Bock, G., Friederich, W., Grad, M., Guterch, A., Heikkinen, P., S.E., Hjelt, T.L., Hyvönen, J.P., Ikonen, Kissling, E., Korja, A., Kozlovskaya, E., M.V., Nevsky, Paulssen, H., N.I., Pavlenkova, Plomerovà, J., Raita, T., O.Y., Riznichenko, R.G., Roberts, Sandoval, S., I.A., Sanina, N.V., Sharov, Z.H., Shomali, Tiikkainen, J., Wielandt, E., Wilegalla, K., Yliniemi, J., Y.G., Yurov

Publikováno v: Journal of Geophysical Research
Journal of Geophysical Research, American Geophysical Union, 2004, 109 (B10), pp.B10303. ⟨10.1029/2003JB002947⟩

International audience

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::bc3dc67d31689b2069c9b681b9c3dca7
https://hal.archives-ouvertes.fr/hal-00118054/file/2003JB002947.pdf