A Two‐Part Framework for Depth to Bedrock Prediction and Uncertainty Assessment in Sweden
ABSTRACT Accurate mapping of depth to bedrock (DTB) in complex post‐glacial landscapes is challenging due to high spatial variability and the prevalence of bedrock outcrops, which introduce “structural zeros” that violate standard regression modelling assumptions.
Yiqi Lin +5 more
wiley +1 more source
Optimal configuration of a micro-earthquake network [PDF]
This study simulates automatic event detection and location performance of a micro-earthquake network centred around a future power plant site in Finland, Fennoscandian Shield.
O. Valtonen +4 more
doaj +1 more source
Evolution and Provenance of the Polish Rotliegend in the Southern Permian Basin
Abstract The Southern Permian Basin (SPB) has been extensively explored for ore deposits. However, a comprehensive evaluation of the remaining copper potential, specifically for sediment‐hosted stratiform copper system, remains lacking. This study applies goSPL, an open‐source landscape and stratigraphic evolution model, to reconstruct the Permian rift‐
Beatriz Hadler Boggiani +3 more
wiley +1 more source
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Tatiana N. Tatevossian +2 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
Multisheet modelling of the electrical conductivity structure in the Fennoscandian Shield [PDF]
Electromagnetic multisheet modelling is a powerful tool for large model areas, if they can be approximated by a multilayered heterogeneous conductivity structure of small vertical dimension in comparison with the penetration depth of electromagnetic fields. In this paper, thin sheet technique is applied to the whole Fennoscandian (Baltic) Shield, whose
Engels, Martin, Korja, Toivo
openaire +1 more source
Increased Glacier Melt Across Millennia to Hours Enhances Erosion and Sediment Export Processes
Abstract Glacial erosion and sediment evacuation are key in shaping polar and mountain landscapes and influencing downstream ecological and social systems. The glacier dynamics and hydrology responsible for these processes are closely linked to hydrological and climatic (hydro‐climatic) conditions.
Ian Delaney +11 more
wiley +1 more source
Ice Phenology and Thickness in Small Arctic Lakes: Field Observations and Mechanistic Controls
Abstract The Arctic is the fastest‐warming region globally. Lake ice is a sentinel indicator of Arctic change, with wide impacts on hydrological regimes, biodiversity, and ecosystem services. While small lakes are ubiquitous across northern boreal and tundra zones, ice observations remain biased toward large lakes with distinct freezing and melting ...
Ludwig Strötz +4 more
wiley +1 more source
Luminescence analysis of a postglacial landscape in northeastern Norway and northern Finland
Portable optically stimulated luminescence (pOSL) analysis allows rapid relative dating of sediments that potentially can be calibrated against known OSL ages to provide an age estimate for landforms across a large area. This study uses 186 pOSL measurements and 20 OSL ages to investigate the postglacial landscape evolution inside the Younger Dryas ...
Alastair Goodship +2 more
wiley +1 more source
Formation mechanism of the Vaasa Batholith in the Fennoscandian shield: Petrographic and geochemical constraints [PDF]
The ~1.88 Ga Vaasa Batholith in western Finland is a large granitoid area (8 000 km2) with gradational contacts against the garnet- and cordierite-bearing diatexite and metatexite migmatites of the Pohjanmaa Belt.
H. Mäkitie +4 more
doaj +1 more source

