Abstract
P343 CARBONIFEROUS BLACK SHALE FACIES IN THE NORTH GERMANY– EVIDENCE BY MAGNETOTELLURIC DATA Introduction 1 In the past 20 years the interest in the deep subsurface of the North German basin and its oil and gas potentials has grown considerably. Geophysical studies on the geological-tectonic structure of the deep basin its genesis and development as well as the chronological and spatial distribution of hydrocarbons have primarily concentrated on reflection seismics. However at depths below the prominent Zechstein (Z) base reflector only few structural details can be distinguished. Besides other potential methods providing information at this depth range e.g. magnetics and
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