Добрый день, Коллеги. Важное сообщение, просьба принять участие. Музей Ферсмана ищет помощь для реставрационных работ в помещении. Подробности по ссылке
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.
WILSON, M., NEUMANN, E.-R., DAVIES, G. R., TIMMERMAN, M. J., HEEREMANS, M. & LARSEN, B. T. Permo-Carboniferous magmatism and rifting in Europe: introduction
NEUMANN, E.-R., WILSON, M., HEEREMANS, M., SPENCER, E. A., OBST, K., TIMMERMAN, M. J. & KIRSTEIN, L. Carboniferous-Permian rifting and magmatism in southern Scandinavia, the North Sea and northern Germany: a review TIMMERMAN, M. J. Timing, geodynamic setting and character of Permo-Carboniferous magmatism in the foreland of the Variscan Orogen, NW Europe HEEREMANS, M., FALEIDE, J. I. & LARSEN, B. T. Late Carboniferous-Permian of NW Europe: an introduction to a new regional map PRAEG, D. Diachronous Variscan late-orogenic collapse in response to multiple detachments: a view from the internides in France to the foreland in the Irish Sea
Берлинские трактаты по наукам о Земле. Серия E. Том 11. Пересмотр, документация и стратиграфия остракод Верхней Юры и нижней Беррии на северо-западе Германии
Die Ostracodenfaunen des Unter-Oxfordium (höchste Omaten-Tone) bis Unter-Berriasium (Serpulit) im Niedersächsischen Becken werden, da die Forschungen hier seit den intensiven Bearbeitungen der 40er, 50er und beginnenden 60er Jahre stagnierten, auf der Grundlage eines modernen taxonomischen Konzeptes neu untersucht und zum Teil rekombiniert. Es werden 98 Arten und 6 Unterarten aus 36 Gattungen und 10 Untergattungen, davon eine neue Art
The purpose of this course is to introduce you to Petrel Geophysics functionality and the workflows. You will go thorough different functionalities in Petrel and learn how to efficiently use these for interpreting 2D/3D seismic data. The powerful tools and algorithms can be used to calculate size/area of your leads and prospects which, in turn, can be used for reserves estimation. You will be provided with a ready-to-use Petrel 2013 project containing 2D/3D seismic and well data. The exercises provide hands on training that enables you to explore the functionalities through dedicated exercises. <...>