In this section
@article{Jackson:2010:10.1144/1354-079309-011,
author = {Jackson, CA-L and Kane, KE and Larsen, E},
doi = {10.1144/1354-079309-011},
journal = {Petroleum Geoscience},
pages = {105--120},
title = {Structural evolution of minibasins on the Utsira High, northern North Sea; implications for Jurassic sediment dispersal and reservoir distribution},
url = {http://dx.doi.org/10.1144/1354-079309-011},
volume = {16},
year = {2010}
}
TY - JOUR
AB - 3D seismic and well data are integrated to determine the tectonostratigraphicevolution of the SW margin of the Utsira High, northern North Sea riftsystem. During the Triassic, a series of minibasins formed due to passive diapirismof the evaporite-bearing, Upper Permian, Zechstein Supergroup. Subsequently,during the Jurassic, a series of secondary minibasins developed as the underlying saltwalls collapsed. These minibasins were a few hundred metres deep, bound bysub-circular to elongate salt-cored structural highs and caused the development ofcomplex subaerial topography and submarine bathymetry on the SW margin of theUtsira High. Salt withdrawal may have been related to: (i) partial dissolution of salt;(ii) differential erosion of the salt walls and adjacent Triassic-filled minibasins; or (iii)salt remigration caused by sub- or supra-salt extension or sediment loading. Thisstudy provides insights into the tectono-stratigraphic evolution of the SW margin ofthe Utsira High and has implications for (i) facies distribution of the ZechsteinSupergroup within the northern North Sea rift system; and (ii) depositional systemdevelopment, and thus reservoir distribution, within the Jurassic sedimentarysuccession.
AU - Jackson,CA-L
AU - Kane,KE
AU - Larsen,E
DO - 10.1144/1354-079309-011
EP - 120
PY - 2010///
SP - 105
TI - Structural evolution of minibasins on the Utsira High, northern North Sea; implications for Jurassic sediment dispersal and reservoir distribution
T2 - Petroleum Geoscience
UR - http://dx.doi.org/10.1144/1354-079309-011
UR - http://pg.geoscienceworld.org/cgi/reprint/16/2/105
VL - 16
ER -