Results 71 to 80 of about 343 (176)
Decoupling of scandium and rare earth elements in organic (nano)particle-rich boreal rivers draining the Fennoscandian Shield. [PDF]
Klimpel F, Bau M.
europepmc +1 more source
Glaciation and regional groundwater flow in the Fennoscandian shield
AbstractRegional‐scale groundwater flow modeling of the Fennoscandian shield suggests that groundwater flow can be strongly affected by future climate change and glaciation. We considered variable‐density groundwater flow in a 1500‐km‐long and approximately 10‐km‐deep cross‐section through southern Sweden. Groundwater flow and shield brine transport in
A. M. PROVOST, C. I. VOSS, C. E. NEUZIL
openaire +1 more source
Comparative analysis of the crustal evolution of the Early Precambrian Belomorian and Trans-North China orogens (Fig. 1) has shown [Slabunov et al., 2015] that: Both belts were formed by the superposition of two Precambrian orogenies.
A. I. Slabunov +4 more
doaj +1 more source
The crystalline basement of Estonia: rock complexes of the Palaeoproterozoic Orosirian and Statherian and Mesoproterozoic Calymmian periods, and regional correlations [PDF]
New data on the Fennoscandian Shield and the Baltic area suggest a need for reinterpretation of the stratigraphy of Estonian Precambrian rock complexes.
Kirs, Juho +7 more
doaj
Journal of Quaternary Science, Volume 40, Issue 5, Page 916-921, July 2025.
Bernd Zolitschka +3 more
wiley +1 more source
The application of inductively coupled plasma mass spectrometry (ICP-MS) is discussed in the case study of Precambrian mafic and ultramafic rocks of easternFennoscandian shield and their mineral components.
Сергей Анатольевич Светов +17 more
doaj +1 more source
Connectivity to the surface determines diversity patterns in subsurface aquifers of the Fennoscandian shield. [PDF]
Hubalek V +7 more
europepmc +2 more sources
Thermochronologic perspectives on the deep-time evolution of the deep biosphere. [PDF]
Drake H, Reiners PW.
europepmc +1 more source
Advances in Defining Ecosystem Functions of the Terrestrial Subsurface Biosphere. [PDF]
Meyer-Dombard DR, Malas J.
europepmc +1 more source
Ancient crystalline basement cratons are traditionally considered challenging geothermal targets due to their low heat flow, limited porosity, and low matrix permeability.
Nicklas Nordbäck +8 more
doaj +1 more source

