Snyder, D. В., Lucas, S. B. & McBride, J. H. Crustal and mantle reflectors from Palaeoproterozoic orogens and their relation to arc-continent collisions
Rollinson, H. R. Tonalite-trondhjemite-granodiorite magmatism and the genesis of Lewisian crust during the Archaean
Vrevsky, A., Krimsky, R. & Svetov, S. Rare earth and isotopic (Nd, O) heterogeneity of the Archaean mantle, Baltic Shield
Bibikova, E. V, Skiold, T. & Bogdanova, S. V. Age and geodynamic aspects of the oldest rocks in the Precambrian Belomorian Belt of the Baltic (Fennoscandian) Shield

NICHOLSON, K., HEIN, J. R, BCTHN, B. & DASGUPTA, S. Precambrian to Modern manganese mineralization: changes in ore type and depositional environment

Review

RoY, S. Genetic diversity of manganese deposition in the terrestrial geological record Precambrian deposits

GLASBY, G. P. Fractionation of manganese from iron in Archaean and Proterozoic sedimentary ores

KULIK, D. A. & KORZHNEV, M. N. Lithological and geochemical evidence of Fe and Mn pathways during deposition of lower Proterozoic Banded Iron Formation in the Krivoy Rog Basin (Ukraine)

BOHN, B. & STANISTREET, I. G. Insight into the enigma of Neoproterozoic manganese and iron formations from the perspective of supercontinental break-up and glaciation

EVANS, D., STOKER, M. S. & CRAMP, A. Geological processes on continental margins: sedimentation, mass-wasting and stability: an introduction mass-wasting and stability: an introduction
VAN WEERING, TJ. C. E., NIELSEN, Z., KENYON, N. H., AKENTIEVA, K. & KUIJPERS, A. H. Large submarine slides at the NE Faeroe continental margin
REEDER, M., ROTHWELL, R. G., STOW, D. A. V., KAHLER, G. & KENTON, N. H. Turbidite flux, architecture and chemostratigraphy of the Herodotus Basin, Levantine Sea, SE Mediterranean
DOBSON, M. R., O'LEARY, L. R. & VEART, M. Sediment delivery to the Gulf of Alaska: source mechanisms along a glaciated transform margin
HOLMES, R. W., LONG, D. & DODD, L. R. Large scale debrites and submarine landslides on the Barra Fan, W of Britain

TRELOAR, P. J., SEARLE, M. P., KHAN, M. A. & JAN, M. Q. Tectonics of the Nanga Parbat syntaxis and the western Himalaya: an introduction
CAPORALI, A. The gravity field of the Karakoram Mountain Range and surrounding areas

TRELOAR, P. J., GEORGE M. T. & WHITTINGTON, A. G. Mafic sheets from Indian plate gneisses in the Nanga Parbat syntaxis: their significance in dating crustal growth and metamorphic
and deformation events
BUTLER, R. W. H. Structural evolution of the western margin of the Nanga Parbat massif, Pakistan Himalaya: insights from the Raikhot-Liachar area
EDWARDS, M. A., KIDD, W. S. R, KHAN, M. A. & SCHNEIDER, D. A. Tectonics of the SW margin of the Nanga Parbat-Haramosh massif

Fifty years have now passed since Graham (1954) published his seminal paper advocating the use of anisotropy of magnetic susceptibility (AMS) as a rapid and sensitive petrofabric tool. During these five decades, Graham's 'underexploited' method has become standard, and AMS and related techniques are now routinely applied to characterizing fabrics in a wide variety of geological materials (e.g. the GEOREF database lists over 500 journal publications with 'magnetic anisotropy' as keywords).

PAYNE, S. N. J., EWEN, D. F. & BOWMAN, M. J. The role and value of 'high-impact biostratigraphy' in reservoir appraisal and development
DUXBURY, S., KADOLSKY, D. & JOHANSEN, S. Sequence stratigraphy subdivision of the Humber Group in the Outer Moray Firth area (UKCS, North Sea)
MORRIS, P. H., PAYNE, S. N. J. & RICHARDS, D. P. J. Micropalaeontological biostratigraphy of the Magnus Sandstone Member (Kimmeridgian-Early Volgian), Magnus Field, UK North Sea
Smpp, D. J. Well-site biostratigraphy of Danish horizontal wells

YIRGU, G., EBINGER, C.J. & MAGUIRE, P.K.H. The Afar volcanic province within the East African Rift System: introduction Part 1: Plate kinematic and geodynamic framework of the Afar volcanic province Introduction
CALAIS, E., EBINGER, C.J., HARTNADY, C., & NOCQUET, J.M. Kinematics of the East African Rift from GPS and earthquake slip vector data
GARFUNKEL, Z. & BEYTH, M. Constraints on the structural development of Afar imposed by the kinematics of the major surrounding plates
BUCK, W.R. The role of magma in the development of the Afro-Arabian Rift System

VAN RENSBERGEN, P., HILLIS, R.R., MALTMAN, AJ. & MORLEY, C.K. Subsurface sediment mobilization: introduction
MALTMAN, AJ. & BOLTON, A. How sediments become mobilized Shallow subsurface sediment mobilization

OWEN, G. Load structures: gravity-driven sediment mobilization in the shallow subsurface
HARRISON, P. & MALTMAN, A. J. Numerical modelling of reverse-density structures in soft non-Newtonian sediments
PARIZE, O. & FRIES, G. The Vocontian clastic dykes and skills: a geometric model
BANKWITZ, P., BANKWITZ, E., BRAUER, K., KAMPF, H. & STORR, M. Deformation structures in Plioand Pleistocene sediments (NW Bohemia, Central Europe)

ROTHWELL, R. G. & RACK, F. R. New techniques in sediment core analysis: an introduction

HASCHKE, M. The Eagle III BKA system, a novel sediment core X-ray fluorescence analyser with very high spatial resolution
RICHTER, T. O., VAN DER GAAST, S., KOSTER, R., VAARS, A., GIELES, R., DE STIGTER, H. C., DE HAAS, H. & VAN WEERING, T. C. E. The Avaatech XRF Core Scanner: technical description and applications to NE Atlantic sediments
CROUDACE, I. W., RINDBY, A. & ROTHWELL, R. G. ITRAX: description and evaluation of a new multi-function X-ray core scanner
THOMSON, J., CROUDACE, I. W. & ROTHWELL, R. G. A geochemical application of the ITRAX scanner to a sediment core containing eastern Mediterranean sapropel units

This work attempts to present the geology of Svalbard in some detail, arranged systematically as a definitive study and so reflecting the present conjuncture of research. It may thus meet the needs of specialists with information on related fields or of any geoscientist wanting an indication of what is known about this key region. Spitsbergen (peaked mountains), the name earlier referred to the whole archipelago. It is now replaced by the name Svalbard (cold coasts), within which Spitsbergen is the principal landmass. Spitsbergen alone is about the size of Switzerland and the whole archipelago a little less than the area of Scotland.