We present a new digital crustal model for Moho depth and crustal structure in Europe,
Greenland, Iceland, Svalbard, European Arctic shelf, and the North Atlantic Ocean (72W …

Eocene magmatic breakup along the mid‐Norway rifted margin was preceded by extreme
Jurassic‐Cretaceous crustal thinning in a magma‐poor environment. Along the SE borders …

Terra Nova, 23, 349–361, 2011 Abstract The long‐term evolution of kilometre (s) high,
seaward‐facing escarpments at passive margins is linked directly to the crustal thinning …

Basement fracture and fault patterns on passive continental margins control the onshore
landscape and offshore distribution of sediment packages and fluid pathways. In this study …

We present results of a multidisciplinary study of the northern segment of the Vøring volcanic
rifted margin, offshore mid‐Norway. This segment represents a transitional margin domain …

Lithospheric stretching is the key process in forming extensional sedimentary basins at
passive rifted margins. This study explores the stretching factors, resulting extension, and …

New structural data, published AFT data, and topographic data suggest that the latest
Cretaceous–Cenozoic uplift of western Norway was associated with normal reactivation of …

Well-developed detrital clay grain coats are observed in deep-marine sandstones of the
Upper Cretaceous Springar Formation of the Vøring Basin in the Norwegian Sea. The …

The mid-Norwegian passive margin is a multiphase rifted margin that developed since the
Devonian. Its geometry is affected by the long-lived activity of the Møre-Trøndelag fault …

The nature of the Lower Crustal Body (LCB) underneath the western part of the Vøring
margin (NE Atlantic) is studied with three scenarios of its extension history:(a) The LCB is …