By A. Solheim, P. Bryn, K. Berg, H. P. Sejrup, J. Mienert
Nice attempt has been undertaken to enquire strength geohazards on the subject of the advance of the Ormen Lange fuel box offshore Mid-Norway. the sphere is found within the scar left after the enormous, tsunami-generating Storegga Slide, which happened approximately 8200 years in the past, and the slide possibility has hence acquired specific concentration. The experiences were multi-disciplinary in personality, and feature concerned a few businesses, universities, and study associations. the result of the venture ended in an important strengthen within the realizing of the Storegga Slide particularly, and submarine slope instability quite often, and performed an enormous position within the approval of box improvement through Norwegian specialists. This publication includes 26 person contributions representing the huge span of issues addressed within the undertaking. the most scope is to supply a state of the art record on geohazard investigations in a excessive range continental margin surroundings. lots of the facts and effects released during this ebook shouldn't have reached past the exclusive record degree until the license companions of the Ormen Lange license had agreed that this knowledge merits a much broader viewers.
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Additional resources for Ormen Lange–an Integrated Study for Safe Field Development in the Storegga Submarine Area
This stratigraphy covers the strata that were affected by the Storegga Slide, and for which ground truth has been acquired during the geotechnical borings (Fig. 2). The correlation across the main Storegga Slide scar is also tied to exploration wells of the Ormen Lange field. The seismic stratigraphy coincides mostly with the lithostratigraphy, as well as with the geotechnical stratigraphy. 48 Κ. Berg et al /Marine and Petroleum Geology 22 (2005) 45-56 Fig. 3. Seismic stratigraphy of the Ormen Lange area, and a north-south running regional seismic section through the northern part of the Storegga Slide.
Hemipelagic or contouritic sediments in the northern area appear to be uncommon, but the amount of such sediments may have been underestimated due to the lack of a well-defined stratified acoustic pattern. The upper part of the combined sequences almost completely covers the Helland Hansen Arch (Figs. 2, 5 and 6) and other dome structures farther north. On the middle-lower slope west of Haltenbanken, some units of stratified sediments occur between more acoustically incoherent units, one of them being up to 70 ms twt thick.
3. , 2005). The preconditions for the third and second large slides (slides ' S ' and 'R') appear to be similar to those for the Holocene Storegga Slide, and the cartoon in Fig. , 2002). Although the large slides apparently occurred shortly after extensive shelf glaciations, it is important to note that there is no indication of major sliding in the northern part of the Storegga area after the Saalian. During this glaciation, glacigenic deposits up to 200 m thick were deposited above stratified sediments in the slope area where we, today, see the deepest incision of the Holocene Storegga Slide (Fig.