The pressure-temperature-time (PTt) evolution of metamorphic rocks is directly related to geodynamics as different tectonic settings vary in their thermal architecture. The shapes of …
A total of 4344 magmatic U-Pb ages in the range 2300 to 800 Ma have been compiled from the Great Proterozoic Accretionary Orogen along the margin of the Columbia/Nuna …
Abstract The mid-Proterozoic (ca. 1850–850 Ma) is a peculiar period of Earth history in many respects: ophiolites and passive margins of this age are rare, whereas anorthosite and A …
The geological timescale before 720 Ma uses rounded absolute ages rather than specific events recorded in rocks to subdivide time. This has led increasingly to mismatches between …
Here we present new 40 Ar/39 Ar geochronology, rock magnetic, and paleomagnetic data obtained from rocks from three distinct domains of the Precambrian Sveconorwegian orogen …
Y Baykal, T Stevens, A Engström-Johansson… - Quaternary Science …, 2021 - Elsevier
Loess deposits along the northern fringe of the European loess belt potentially record past changes in dust emission from areas proximal to former ice sheets. Recent chronologies …
Abstract The Cretaceous-Paleogene Boundary (KPB), the only known global impact ejecta layer, resulted from the 66 million years ago Chicxulub Impact Event. KPB is well …
The role of Quaternary ice sheet fluctuations in driving meltwater pulses and ocean circulation perturbations is widely acknowledged. What is less clear is the role of these …
N Rosing-Schow, RL Romer, A Müller, F Corfu… - Precambrian …, 2023 - Elsevier
Most pegmatites of southern Norway seem to be derived from anatectic melting of metamorphic rocks during the Sveconorwegian orogeny rather than to be highly evolved …