[HTML][HTML] Layered intrusions in the Precambrian: Observations and perspectives
Layered intrusions are plutonic bodies of cumulates that form by the crystallization of mantle-
derived melts. These intrusions are characterized by igneous layering distinguishable by …
derived melts. These intrusions are characterized by igneous layering distinguishable by …
Differences in Sm/Nd ratios between early magmatic and late sulfides: The role of fluids and Nd mobility
PA Serov - Chemical Geology, 2025 - Elsevier
This paper presents the results of a Smsingle bondNd study of sulfide minerals and whole-
rock samples from Cu-Ni-PGE layered complexes of the Fennoscandian Shield. Syngenetic …
rock samples from Cu-Ni-PGE layered complexes of the Fennoscandian Shield. Syngenetic …
Sr isotope geochemistry of the Koillismaa Intrusion, Northern Finland
S Itani - 2023 - oulurepo.oulu.fi
Igneous activity during the early Palaeoproterozoic (2.4–2.5 Ga) led to the development of
layered intrusions, mafic dyke swarms, and volcanic rock in the Earth's cratonic regions. The …
layered intrusions, mafic dyke swarms, and volcanic rock in the Earth's cratonic regions. The …
[PDF][PDF] Mineral systems driven prospectivity modelling of orthomagmatic ore deposits
Nickel (Ni), cobalt (Co), platinum group metals (PGMs), chromium (Cr), vanadium (V), and
copper (Cu) are some of the metals that are considered critical or strategic raw materials by …
copper (Cu) are some of the metals that are considered critical or strategic raw materials by …
[PDF][PDF] RES TERRAE
F Guo - oulu.fi
Northeastern Fennoscandia contains multiple generations of extrusive and intrusive
maficultramafic magmatism in the Archaean greenstone belts and Palaeoproterozoic rift …
maficultramafic magmatism in the Archaean greenstone belts and Palaeoproterozoic rift …