Pre-existing structures within crystalline basement may exert a significant influence over the
evolution of rifts. However, the exact manner in which these structures reactivate and thus …

The deformation of the middle to lower crust in collisional settings occurs via deformation
mechanisms that vary with rock composition, fluid content, pressure, and temperature. These …

The International Geo Sample Number (IGSN) is a globally unique persistent identifier (PID)
for physical samples that provides discovery functionality of digital sample descriptions via …

Nappes of continental outer and outermost margin affinities (Middle Allochthon) were
transported from locations west of the present Norwegian coast and thrust eastwards onto …

Numerous studies have investigated the geodynamic history and lithological composition of
the Proterozoic basement, Caledonian nappes, and Devonian extensional basins and shear …

Scientific drilling expeditions offer a unique opportunity to characterize microbial
communities in the subsurface that have long been isolated from the surface. With …

The evolution of Fennoscandia following the early Devonian collapse of the Caledonian
mountains is a matter of debate, due largely to the scarcity of post-Caledonian cover rocks …

The 2.5 km deep scientific COSC-1 borehole (ICDP 5054-1-A) was successfully drilled with
nearly complete core recovery during spring and summer of 2014. Downhole and on-core …

We present a novel 2‐D magnetotelluric (MT) inversion scheme, in which the local weights
of the regularizing smoothness constraints are based on the envelope attribute of a …

During continental collision, large tracts of crust are mobilized along major shear zones. The
metamorphic conditions at which these zones operate, the duration of thrusting, and the …