High-Density OBC-A Step Change in Reservoir Imaging-A BP North Sea View

Author(s):  
Daniel Milo David Davies ◽  
Herlinde Charlotte Mannaerts ◽  
John McGarrity ◽  
Mark Ibram ◽  
Colin McKenzie ◽  
...  
Keyword(s):  
2018 ◽  
Author(s):  
Hany Ahmed Beeh ◽  
Haitham Khalil ◽  
Steven Leonardus Paulus ◽  
Arun Tiku ◽  
Bjarte Andre Karlsen

2014 ◽  
Vol 93 (1-2) ◽  
pp. 31-42 ◽  
Author(s):  
S. van Heteren ◽  
J.A.C. Meekes ◽  
M.A.J. Bakker ◽  
V. Gaffney ◽  
S. Fitch ◽  
...  

AbstractThe North Sea subsurface shows the marks of long-term tectonic subsidence. Much of it contains a thick record of glacial and interglacial deposits and landscapes, formed during multiple glacial cycles and the associated regressions and transgressions during the past two million years. At times of lower sea level than today, areas that are presently submerged were fertile lowlands more favourable for hunting and gathering than the surrounding upland. These drowned lowlands are not captured by traditional 1:250,000 geological maps of the North Sea subsurface because the underlying seismic and core data are commonly too widely spaced to achieve this. Palaeolandscape mapping requires identification of building blocks with spatial scales in the order of 1 km or less. As high-density 2D and high-quality 3D seismics are becoming available for an increasing part of the North Sea, glacial and interglacial palaeolandscapes can be reconstructed for more and more areas. An overview of published palaeolandscape reconstructions shows that shallow time slices through 3D data provide map views that are very suitable for the identification of landscape elements. For optimal results, each time slice needs to be validated and ground-truthed with 2D seismics and with descriptions and analyses of cores and borehole samples. Interpretations should be made by teams of geoscientists with a sufficiently broad range of expertise to recognise and classify even subtle or unfamiliar patterns and features. The resulting reconstructions will provide a context and an environmental setting for Palaeolithic, Mesolithic, and Neolithic societies and finds.


1999 ◽  
Author(s):  
T.M. Gaynor ◽  
G.T. Irvine ◽  
R. Boulton ◽  
D.A. Gilchrist ◽  
Ian Lane

2002 ◽  
Author(s):  
A.G. Norrie ◽  
S. Akram ◽  
M.R. Niznik
Keyword(s):  

Author(s):  
Y. Li ◽  
L. Zhu ◽  
K. Tachibana ◽  
H. Shimamura

This paper presents a method of reshaping and extraction of markers and masks of the dense houses from the DSM based on mathematical morphology (MM). Houses in a digital surface model (DSM) are almost joined together in high-density housing areas, and most segmentation methods cannot completely separate them. We propose to label the markers of the buildings firstly and segment them into masks by watershed then. To avoid detecting more than one marker for a house or no marker at all due to its higher neighbour, the DSM is morphologically reshaped. It is carried out by a MM operation using the certain disk shape SE of the similar size to the houses. The sizes of the houses need to be estimated before reshaping. A granulometry generated by <i>opening-by-reconstruction</i> to the NDSM is proposed to detect the scales of the off-terrain objects. It is a histogram of the global volume of the top hats of the convex objects in the continuous scales. The obvious step change in the profile means that there are many objects of similar sizes occur at this scale. In reshaping procedure, the slices of the object are derived by morphological filtering at the detected continuous scales and reconstructed in pile as the dome. The markers are detected on the basis of the domes.


2014 ◽  
Vol 93 (4) ◽  
pp. 197-197 ◽  
Author(s):  
S. van Heteren ◽  
J.A.C. Meekes ◽  
M.A.J. Bakker ◽  
V. Gaffney ◽  
S. Fitch ◽  
...  
Keyword(s):  

2003 ◽  
Author(s):  
Morten Stenhaug ◽  
Leif Erichsen ◽  
Fokko H.C. Doornbosch ◽  
Robert A. Parrott

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