Orals TS2.3/ERE5.5
Thursday, 11 April 2013 Room B13 Chairperson: Peter Eichhubl, John Hooker |
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08:30–08:45 |
EGU2013-9491
Effects of faults as barriers or conduits to displaced brine flow on a putative CO2 storage site in the Southern North Sea |
08:45–09:00 |
EGU2013-10713
Regional methods for mapping major faults in areas of uniform low relief, as used in the London Basin, UK |
09:00–09:15 |
EGU2013-8464
Length-displacement scaling relations and the development of faults |
09:15–09:30 |
EGU2013-4040
Analysis of fracture networks in a reservoir dolomite by 3D micro-imaging |
09:30–09:45 |
EGU2013-4388
Initiation of Krauklis waves in fluid-filled fractures by an incident seismic body wave |
09:45–10:00 |
EGU2013-4464
Structural analysis of a fractured basement reservoir, central Yemen |
COFFEE BREAK
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10:30–10:45 |
EGU2013-1622
The Long Term Response of a Continent Adjacent to a Hyperextended Margin: A Case Study From Scandinavia (solicited) |
10:45–11:00 |
EGU2013-6152
Imaging fault zones using 3D seismic image processing techniques (solicited) |
11:00–11:15 |
EGU2013-12454
Structural interpretation of seismic data and inherent uncertainties (solicited) |
11:15–11:30 |
EGU2013-13297
Chemical-mechanical interactions during natural fracture growth in tight gas and oil reservoirs: Implications for flow during reservoir charge and production |
11:30–11:45 |
EGU2013-2986
How can K-Ar geochronology of clay-size mica/illite help constrain reactivation histories of brittle faults? An example from a Paleozoic thrust fault in Northern Norway |
11:45–12:00 |
EGU2013-9575
A natural fiber composite in a pelagic limestone-chert sequence. The importance of mechanical stratigraphy for fracture type development in carbonate anticlines. |