Previously published Oligocene eustatic records are compared with observed stratigraphic architecture at the New Jersey continental margin in order to evaluate the stratigraphic response to eustatic change. Lower to mid-Oligocene sequence boundaries (33.8–28.0 Ma) are associated with relatively long hiatuses (0.3–0.6 m.y.), in which sedimentation in many places terminated during eustatic falls and resumed early during eustatic rises. Upper Oligocene sequence boundaries are associated with relatively short hiatuses (less than 0.3 m.y.), and provide the best constraints on phase relations between sea-level forcing and margin response. The interval represented by each upper Oligocene sequence varies in dip profile. At updip locations, landward...
Sequence stratigraphy provides an understanding of the interplay between eustasy, sediment supply an...
2-D seismic, wireline log, and core data at ODP Leg 174A Sites 1071 and 1072 on the outer continenta...
We evaluate lithofacies, chronology, and seismic sequences from the Canterbury Basin, New Zealand pa...
"The emergence of seismic/sequence stratigraphy since the late 1970s has led to a revolution in stra...
The emergence of seismic/sequence stratigraphy since the late 1970s has led to a revolution in strat...
The Oligocene of the New Jersey continental margin is divisible into as many as eight sequences and ...
The New Jersey Sea Level Transect was designed to evaluate the relationships among global sea level ...
This study uses high resolution geochronology (from biostratigraphy and Sr-isotope age estimates), l...
Processes that build continental-margin stratigraphy on time-scales of> 20 kyr have been inves-ti...
ABSTRACT: The Oligocene of the New Jersey continental margin is divisible into as many as eight sequ...
Eustatic estimates from the backstripping of Oligocene sections are compared quantitatively with δ18...
2-D seismic, wireline log, and core data at ODP Leg 174A Sites 1071 and 1072 on the outer continenta...
International audienceIn May-July 2009, IODP Expedition 313 used an ECORD "mission-specific" jack-up...
This dissertation uses sequence stratigraphic analysis to study the early to middle Miocene growth o...
This study uses a high-resolution integrated sequence stratigraphic method to determine the paleoec...
Sequence stratigraphy provides an understanding of the interplay between eustasy, sediment supply an...
2-D seismic, wireline log, and core data at ODP Leg 174A Sites 1071 and 1072 on the outer continenta...
We evaluate lithofacies, chronology, and seismic sequences from the Canterbury Basin, New Zealand pa...
"The emergence of seismic/sequence stratigraphy since the late 1970s has led to a revolution in stra...
The emergence of seismic/sequence stratigraphy since the late 1970s has led to a revolution in strat...
The Oligocene of the New Jersey continental margin is divisible into as many as eight sequences and ...
The New Jersey Sea Level Transect was designed to evaluate the relationships among global sea level ...
This study uses high resolution geochronology (from biostratigraphy and Sr-isotope age estimates), l...
Processes that build continental-margin stratigraphy on time-scales of> 20 kyr have been inves-ti...
ABSTRACT: The Oligocene of the New Jersey continental margin is divisible into as many as eight sequ...
Eustatic estimates from the backstripping of Oligocene sections are compared quantitatively with δ18...
2-D seismic, wireline log, and core data at ODP Leg 174A Sites 1071 and 1072 on the outer continenta...
International audienceIn May-July 2009, IODP Expedition 313 used an ECORD "mission-specific" jack-up...
This dissertation uses sequence stratigraphic analysis to study the early to middle Miocene growth o...
This study uses a high-resolution integrated sequence stratigraphic method to determine the paleoec...
Sequence stratigraphy provides an understanding of the interplay between eustasy, sediment supply an...
2-D seismic, wireline log, and core data at ODP Leg 174A Sites 1071 and 1072 on the outer continenta...
We evaluate lithofacies, chronology, and seismic sequences from the Canterbury Basin, New Zealand pa...