Results 61 to 70 of about 343 (176)
Revisit of the Fennoscandian Shield along the UPPLAND seismic profile: competitive velocity models [PDF]
This paper presents a comprehensive re-analysis of seismic data collected along the UPPLAND profile in the Fennoscandian Shield, focusing on the competitive velocity models for P-wave (Vp) and S-wave (Vs) velocities and the Vp/Vs ratio.
T. Janik +4 more
doaj +1 more source
New evidence of the Vuoksi River origin by geodynamic cataclysm [PDF]
The territory of investigations is located in the SE periphery of the Fennoscandian Shield. It served as an arena of periodic significant restructuring of the hydrographic network associated with the filling and discharge of large late-glacial and ...
D.A. Subetto +5 more
doaj +1 more source
Radioisotopic age constraints of the Cambrian Ritland impact structure, Norway
Abstract Secondary ion mass spectrometry U‐Pb geochronology has been performed on zircon grains separated from impact melt rock from the 2.7 km‐in‐diameter Ritland impact structure, southwestern Norway. Scanning electron microscope‐based imaging techniques, including electron backscatter diffraction analysis, reveal various zircon grain microtextures ...
William R. Hyde +6 more
wiley +1 more source
Multi‐million‐year evolution of the Greenland Ice Sheet in Inglefield Land, North Greenland
ABSTRACT Information on past sensitivity of the Greenland Ice Sheet to climate change is of importance for optimizing models simulating the future evolution of ice mass loss. While the ice‐sheet change during the Lateglacial and Holocene is relatively well constrained, the long‐term (multi‐million‐year) evolution of the Greenland Ice Sheet remains ...
Anne Sofie Søndergaard +6 more
wiley +1 more source
Abstract We aim to isolate predominantly solar modulated (multi‐decadal to centennial) production changes in a 10Be record from Black Sea sediments covering Termination 2. In addition to the effects of varying climate and sedimentation, sea level rise and tephra‐driven Be relocation introduced non‐production biases into our 10Be (and 9Be) records ...
Markus Czymzik +2 more
wiley +1 more source
ABSTRACT Fluid–rock interactions play a key role in the formation, evolution and recycling of the Earth's crust. For fluids to infiltrate rocks and enable and sustain fluid‐mediated mineral transformations, fluid pathways are required. In this study, we examined the potential mechanisms of formation of such pathways via detailed mineralogical ...
Saskia Grund +4 more
wiley +1 more source
Our recent studies of metamorphism within the Fennoscandian (or Baltic) Shield area with representative sites of orogenic gold mineralization based on the scheme of mineral facies of metamorphic rocks introduced earlier inspired thorough revision of that
Сергей Алексеевич Бушмин +3 more
doaj +1 more source
Thiobacillus as a key player for biofilm formation in oligotrophic groundwaters of the Fennoscandian Shield. [PDF]
Lopez-Fernandez M +6 more
europepmc +1 more source
Mineralogical, petrographic and geochemical features of fenitization halos of circular (ring) and linear carbonatite complexes, Alno (Sweden) and Chernigovka (Ukraine), respectively, have been investigated.
Yu. Ye. Nykanorova +3 more
doaj
The results of detailed study of the Urosozero greenstone structure (northwestern part of the Vodlozero domain) of the Fennoscandian Shield are presented. The composition and the U-Pb zircon age of the volcanic rocks were studied. The Urosozero structure
Наталия Александровна Арестова +11 more
doaj +1 more source

