Results 21 to 30 of about 3,972 (218)
Fault systems in multiply deformed regions of Eurasia
Russian Journal of Earth Sciences, 2023 We have studied the orogenic fragile deformation of the upper Earth’s crust of several areas of the Eurasian continent, where deformations have occurred many times – in the Tian Shan and Altai-Sayan regions of the Central Asian Paleozoic Fold Belt and in
Burtman V, Kolodyazhnyi S
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Vanadium Mineralization in the Kola Region, Fennoscandian Shield [PDF]
Minerals, 2018 In the northern Fennoscandian Shield, vanadium mineralization occurs in the Paleoproterozoic Pechenga–Imandra-Varzuga (PIV) riftogenic structure. It is localized in sulfide ores hosted by sheared basic and ultrabasic metavolcanics in the Pyrrhotite Ravine and Bragino areas and was formed at the latest stages of the Lapland–Kola orogeny 1.90–1.86 Ga ago.
Alena Kompanchenko +2 more
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Timing of syn-orogenic, high-grade transtensional shear zone formation in the West Uusimaa Complex, Finland [PDF]
Bulletin of the Geological Society of Finland, 2022 We present zircon and titanite U-Pb ages from granulite-facies transtensional shear zones and a greenschist facies strike-slip shear zone in the Karkkila-Vihti area, West Uusimaa. The zircon rim and titanite ages of c.
Taija Torvela, Matti Kurhila
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Геофизический журнал, 2012 The nature of geoacoustic waves is discussed, based on comparison of the results of seismic and acoustic studies in the Fennoscandian Shield with the drilling record of the Kola Superdeep Borehole: 12262 m (1970-1990), Russia; Gravberg 6337 m (1986-1987),
N. V. Sharov
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Transactions of the Karelian Research Centre of the Russian Academy of Sciences, 2017 Specific morphological structures corresponding to impulsive seismotectonic events were identified within the Onega structure of the Fennoscandian (Baltic) shield of the East European platform.
Андрей Алексеевич Никонов +5 more
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Crustal Architecture of the Inverted Central Lapland Rift Along the HUKKA 2007 Profile [PDF]
, 2013 Peer ...
Bruckl, Ewald +9 more
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Pressure, temperature and time constraints on tectonic models for southwestern Sweden [PDF]
, 2010 In this work, a number of key localities have been investigated in detail in order to provide precise constraints on models for the tectonic evolution of southern Sweden.
Austin Hegardt, Eric
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Some features of deformation structures in an esker on the southern margin of the Fennoscandian shield [PDF]
Bulletin of the Geological Society of Finland, 2018 As a result of melting of the last ice sheet in the southeastern edge of the Fennoscandian shield, ridge structures called eskers were formed. One of these eskers is the subject of our study.
A. Poleshchuk, D. Zykov, S. Shvarev
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The Present State of the Kola Peninsula Broadband Seismic Network
Russian Journal of Earth Sciences, 2023 This paper provides information about the main parameters of spatial broadband seismic network in the Kola region (the northeastern part of the Fennoscandian Shield). Since 2021 the seismic network has been expanded by five seismic stations and currently
Goev Andrey Georgievich +5 more
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Seismic situation in the northern parts of the Karelian craton (Fennoscandian Shield)
Transactions of the Karelian Research Centre of the Russian Academy of Sciences, 2018 The seismic situation in the northern parts of the Karelian craton (Fennoscandian Shield) was studied. The geological structure of the territory is briefly described. The events of natural and man-made genesis recorded by seismic stations of the Karelian
Ирина Александровна Зуева +3 more
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