Geophysical, petrological, and geochemical data provide important clues about the
composition of the deep continental crust. On the basis of seismic refraction data, we divide …

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 …

Accretionary orogens form at intraoceanic and continental margin convergent plate
boundaries. They include the supra-subduction zone forearc, magmatic arc and back-arc …

Recent geological studies have provided new concepts concerning the timing of the final
break-up of the Archaean craton. Age data on detrital zircons from sedimentary rocks in …

The Global Geoscience Transect SVEKA (GGT/SVEKA), a 160 km wide, 840 km long strip in
the central part of the Fennoscandian shield, covers the western part of the Archean …

A priori knowledge on large-scale sub-surface conductivity structure is required in many
applications investigating electrical properties of the lithosphere. A map on crustal …

Summary In 1989 the BABEL Working Group collected 2268 km of near-vertical reflection
data in the Baltic and Bothnian Seas. As an integrated part of the field survey, the marine …

Extensive deep seismic and electromagnetic sounding programs have resulted in tens of
deep refraction seismic profiles, normal-incidence reflection profiles, several hundred …

Two lithotectonic units (the Norrbotten and Överkalix units) occur inside the
Paleoproterozoic (2.0–1.8 Ga) Svecokarelian orogen in northernmost Sweden. Archean (2.8 …

The BABEL profiles B, C, 1–7 form a 1200km long nearly continuous cross-section through
the Svecofennides. The near-vertical marine reflection profiles display a wide range of …