No unique temperature of equilibration for mantle peridotites – Thermal histories told by differently diffusing cations based on novel calibrations We generated novel thermometric formulae for cation exchange reactions between mantle minerals involving species of…Heinz-Gerd Röhling31. Mai 2023
Diffraction intensities of ordered omphacite, measured from precession electron diffraction Cation ordering in minerals at high temperatures is important for understanding the metamorphic processes in…Heinz-Gerd Röhling31. Mai 2023
Contaminant mobilization from an abandoned polymetallic sulfide mine, Mt. Bobija, Serbia On top of Mt. Bobija, located in Western Serbia and mainly composed of silt- and…Heinz-Gerd Röhling31. Mai 2023
No unique temperature of equilibration for mantle peridotites – Thermal histories told by differently diffusing cations based on novel calibrations We generated novel thermometric formulae for cation exchange reactions between mantle minerals involving species of…Heinz-Gerd Röhling31. Mai 2023
Application of U-Pb LA-ICP-MS dating to unravel climate evolution and surface processes Geochronological tools may play an important role in understanding the coupled evolution of biosphere and…Heinz-Gerd Röhling31. Mai 2023
“Heat In Place” assessments for Berlin/Brandenburg’s deep geothermal potential Geologically located in the Northeast German Basin, Berlin and most parts of Brandenburg are known…Heinz-Gerd Röhling31. Mai 2023
Neoflabellina reticulata (Reuss 1851) – The Fossil of the Year 2022 The Paläontologische Gesellschaft (Palaeontological Association) has been awarding the title Fossil of the Year since…Heinz-Gerd Röhling31. Mai 2023
Three years communicating geosciences in social networks: Divulgacion Terrologa Social networks have become important communication bridges between the scientific community and society. For this…Heinz-Gerd Röhling31. Mai 2023
Latest analytical developments of the SwissSIMS Lausanne The SwissSIMS is a national facility equipped with a Cameca 1280 HR2 installed at the…Heinz-Gerd Röhling31. Mai 2023
Timing and conditions for peak metamorphism in Isua (Western Greenland) We present a Lu-Hf-garnet-amphibole-whole rock age of 2.59 ± 0.11 Ga for a carbonaceous garnet-hornblende-mica…Heinz-Gerd Röhling31. Mai 2023