Our understanding of how global climatic changes are translated into ice-sheet fluctuations and sea-level change is currently limited by a lack of knowledge of the configuration of ice …
The Great Unconformity, a profound gap in Earth's stratigraphic record often evident below the base of the Cambrian system, has remained among the most enigmatic field …
Ice can sculpt extraordinary landscapes, yet the efficacy of, and controls governing, glacial erosion on geological timescales remain poorly understood and contended, particularly …
P Japsen, PF Green, JA Chalmers, JM Bonow - Earth-Science Reviews, 2024 - Elsevier
The forces that drive uplift of the continental lithosphere outside collision zones are a topic of considerable dispute. Here we review our studies of the post-Caledonian development of …
We introduce the first solution for simulating the formation and evolution of glaciers, together with their attendant erosive effects, for periods covering the combination of glacial and inter …
This paper introduces the Instructed Glacier Model (IGM)–a model that simulates ice dynamics, mass balance and its coupling to predict the evolution of glaciers, icefields or ice …
Ice-sheet responses to climate warming and associated sea-level rise depend sensitively on the form of the slip law that relates drag at the beds of glaciers to their slip velocity and basal …
We employ U–Pb calcite dating of structurally-controlled fracture fills within crystalline Caledonian basement in western Norway to reveal subtle large-scale tectonic events that …
The Cryogenian 'Sturtian'snowball Earth glaciation (c. 717–658 Ma) likely had a major role in shaping continental landscapes and biotic radiations of the late Neoproterozoic Era …