Tectonic processes associated with supercontinent cycles result in a variety of basin types,
and the isotopic dating of detrital minerals within sedimentary sequences assists …

Extensional structures characterize significant parts of the North Atlantic Caledonides.
Silurian extensional deformation took place, particularly in the heated crust in the southern …

Abstract During the Mesoproterozoic, central Fennoscandia and Laurentia (Greenland) were
characterized by a weakly extensional stress regime, as evident from episodic rapakivi …

To better understand the past retreat patterns and chronologies of major marine-terminating
outlet glaciers, the Late Weichselian and Holocene glacial history of a NE Greenland fjord …

abstract Recent studies of structure, stratigraphy and isotope geochronology on Svalbard
and East Greenland have provided a foundation for reconstructing the Laurentian margin of …

Observations and modeling show that temperature controls crustal rheology and therefore
also the orogenic evolution of continent‐continent collision zones and the associated …

We argue there is no distinction between accretion and collision as a process, except when
accretion is used in the sense of incorporating small bodies of sedimentary and/or volcanic …

Arkose-dominated sequences exposed in the Lower and Middle Allochthons of the
Scandinavian Caledonides, known as the Sparagmites, are the product of sedimentation …

New detrital zircon sensitive high-resolution ion microprobe (SHRIMP) geochronology and
published framework geology of Neoproterozoic to Silurian strata are integrated to …

Siliciclastic sequences accumulated along the eastern margin of Laurentia during the late
Neoproterozoic to early Paleozoic as a result of the breakup of Rodinia and formation of the …