Results 171 to 180 of about 254,715 (432)
Geostatistical analysis of an experimental stratigraphy [PDF]
[1] A high-resolution stratigraphic image of a flume-generated deposit was scaled up to sedimentary basin dimensions where a natural log hydraulic conductivity (ln( K)) was assigned to each pixel on the basis of gray scale and conductivity end-members ...
Davis, J M+5 more
core +1 more source
Early-Middle Pleistocene benthic turnover and oxygen isotope stratigraphy from the Central Mediterranean (Valle di Manche, Crotone Basin, Italy): data and trends [PDF]
Ostracod faunal turnover and oxygen isotope data (foraminifera) along the Valle di Manche (VdM) section are herein compiled. Specifically, the material reported in this work includes quantitative palaeoecological data and patterns of ostracod fauna ...
Azzarone, Michele+7 more
core +2 more sources
The Post-Cretaceous Stratigraphy of Southern Nigeria [PDF]
John Parkinson
openalex +1 more source
The Upper Permian Castile Formation of the Delaware Basin, a 515.3 m (1690.6 ft) thick deep‐water evaporitic sequence dominated by anhydrite and halite, is the focus of this study. This study's sedimentological and geochemical analysis of cores from the basin's centre and margin reveals that dynamic reflux of deep hypersaline brines significantly ...
Ander Martinez‐Doñate+6 more
wiley +1 more source
On the Stratigraphy and Structure of the Tarnthal Mass (Tyeol). [PDF]
Alfred P. Young
openalex +1 more source
A classical peripheral foreland basin is bounded longitudinally by a pair of marginal ocean basins (DeCelles & Giles, 1996). The WTFB sediments transfer to adjacent marginal ocean basins. The western Taiwan foreland basin (WTFB) is regarded as a classical peripheral foreland basin, longitudinally bounded by the southern Okinawa Trough (SOT) to the ...
Cheng‐Shing Chiang+2 more
wiley +1 more source
X. The Stratigraphy of the Arden Basin [PDF]
R. G. Carruthers, E. M. Anderson
openalex +1 more source
Lacustrine and fan‐delta sediments in syn‐rift lake basins
A consistent model for the sequence framework and depositional pattern of asymmetric half‐grabens in syn‐rift lake basins bounded by active faults has been established, complementing existing models for marine rift successions. Syn‐rift lake basins are characterised by relatively small dimensions, steep slopes, poorly developed shoreline strata ...
Qianyou Wang+6 more
wiley +1 more source
Timing of initiation of reverse displacement on the Taranaki Fault, northern Taranaki Basin: Constraints from the on land record (Oligocene Te Kuiti Group) [PDF]
Structures associated with the wedge of basement overthrust into Taranaki Basin along the Taranaki Fault, are regarded as hydrocarbon plays and have been tested by drilling through the tip of the overthrust.
Kamp, Peter J.J.+1 more
core
New radiocarbon dates and late-Pleistocene stratigraphy [PDF]
Richard Foster Flint
openalex +1 more source