Results 41 to 50 of about 105,826 (191)
Zur letzten Eiszeit im alpinen und nordeuropäischen Raum [PDF]
Geographica HelveticaOn the last Glaciation of the Alps and Fennoscandia. During the Pleistocene the Alps and the Fennoscandian Shield were covered several times with extensive ice caps. During the last Ice Age.
G. Glückert
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Stratigraphical section through Lower Cambrian at Söderfjärden, Vaasa, western Finland [PDF]
Bulletin of the Geological Society of Finland, 1982 The Lower Cambrian sedimentary rocks form a doughnut-shaped deposit on the bottom of the Söderfjärden depression. The sedimentary pile was first established and has now been penetrated by drilling.
J.J. Lehtovaara
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, 2000 The current research report covers over 20 papers presented at the 2nd annual GEODE-Fennoscandian shield field workshop on Palaeoproterozoic and Archaean greenstone belts and VMS districts in the Fennoscandian Shield, 28 August to 1 September 2000 ...
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FAULT SYSTEMS IN THE UPPER CRUST OF THE FENNOSCANDIAN SHIELD, THE EAST EUROPEAN PLATFORM
Геодинамика и тектонофизика, 2020 Directions of 683 faults located in the southeastern part of the Fennoscandian (Baltic) shield were statistically analyzed, and three orthogonal associations of fault systems were identified in the study area.
V. S. Burtman, S. Yu. Kolodyazhny
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Helium in Porewater and Rocks of Crystalline Bedrock from the Fennoscandian Shield, Olkiluoto (Finland) [PDF]
, 2017 Dissolved noble gases in matrix porewaters of low-permeable crystalline rocks are useful tracers for investigating porewater migration and interactions between porewater and groundwater.
Eichinger, Florian +3 more
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Dynamic features of “Petrozavodsk” seismic station
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, 2016 The paper is devoted to the estimability and recordability of seismic events, namely the research of the noise power spectral density (PSD) and its diurnal variation around “Petrozavodsk” seismic station (PTRZ), located within the Onega structure of the ...
Александр Валерьевич Климовский +5 more
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Геодинамика и тектонофизика, 2020 A critical discussion of competing models of the geodynamic nature (oceanic or continental subduction) and age (Meso-Neoarchean or Late Paleoproterozoic) of the eclogite facies metamorphism in the Belomorian eclogite province (BEP) is based on the ...
M. V. Mints, K. A. Dokukina
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A seismic study of the mid- and lower-crust beneath the sea of Bothnia: BABEL line 1 [PDF]
, 1994 In the Autumn of 1989, Durham University took part in the BABEL Project, a collaboration of scientists from five nations recording wide angle and normal incidence seismic data in the Baltic Shield.
Graham, Daniel P.
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Numerical lithospheric modelling: rheology, stress and deformation in the central Fennoscandian Shield [PDF]
, 2005 This thesis deals with the analysis of the rheological structure and tectonic modelling of the Fennoscandian Shield. First, a short introduction to the geology and geophysics of the Fennoscandian Shield is presented followed by a description of ...
Moisio, K. (Kari)
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Geological-geophysical models of the crust for the White Sea region
Геодинамика и тектонофизика, 2020 The study of the White Sea region and the adjacent area aimed to model the structure of the crystalline portion of the crust at the contact of the northeastern slope of the Fennoscandian Shield and the Russian Plate.
N. V. Sharov +4 more
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