Results 31 to 40 of about 305,558 (359)
Seismic characteristics of polygonal fault systems in the Great South Basin, New Zealand
Open Geosciences, 2020 A well-developed multi-tier polygonal fault system is located in the Great South Basin offshore New Zealand’s South Island. The system has been characterised using a high-quality three-dimensional seismic survey tied to available exploration boreholes ...
Jitmahantakul Sukonmeth +3 more
doaj +1 more source
Application of Change-Point Detection to a Structural Component of Water Quality Variables [PDF]
, 2011 In this study, methodologies were developed in statistical time series models, such as multivariate state-space models, to be applied to water quality variables in a river basin.
Costa, Marco, Gonçalves, A. Manuela
core +2 more sources
The Laga basin: Stratigraphic and Structural Setting
Geological Field Trips, 2008 Most of the ancient turbidite systems are known being deposited in foredeep basins at the front of active thrust belt. Differently from fluvio-deltaic systems generally lacated in the more internal portion of these basins, the turbidite systems occur at different depth in the more deeper portions of these basins (foredeep turbidite systems) or in the ...
Salvatore Milli +3 more
openaire +3 more sources
Rates of erosion and landscape change along the Blue Ridge escarpment, southern Appalachian Mountains, estimated from in situ cosmogenic 10Be [PDF]
, 2016 The Blue Ridge escarpment, located within the southern Appalachian Mountains of Virginia and North Carolina, forms a distinct, steep boundary between the lower-elevation Piedmont and higher-elevation Blue Ridge physiographic provinces.
Bierman, Paul R. +5 more
core +2 more sources
Structural analysis of the Malay Basin [PDF]
Bulletin of the Geological Society of Malaysia, 1997 The structural patterns within the Malay Basin are divided into fold and fault systems. Three main fold domains are demarcated based on fold geometry and characteristics of associated faults: Basin Hinge; Basin Axis; and Basin Ramp. As for fault systems, high density and low density fault domains are identified.
Jalan Bukit Bintang +3 more
openaire +1 more source
Faulting patterns in the Lower Yarmouk Gorge potentially influence groundwater flow paths [PDF]
, 2019 Recent studies investigating groundwater parameters, e.g., heads, chemical composition, and heat transfer, argued that groundwater flow paths in the Lower Yarmouk Gorge (LYG) area are controlled by geological features such as faults or dikes.
Alraggad, Marwan +7 more
core +1 more source
Energy Exploration & Exploitation, 2020 The analysis and interpretation of the Dachaidan area, Qaidam Basin, is difficult, owing to the co-location of two groups of thrust faults (N–E faults and N–W faults) there and the area’s complicated structural deformation history.
Li Zongxing +4 more
doaj +1 more source
Structure of the western Somali Basin [PDF]
Journal of Geophysical Research, 1967 The western Somali Basin in the northwestern Indian Ocean is covered by thick deposits of terrigenous sediments. Seismic reflection profiles show, however, the northern and southern parts to be very different. The northern sections is a deep basin filled with thick uniformly stratified sediments. It is enclosed by the continental margin to the west and
Elizabeth T. Bunce +3 more
openaire +2 more sources
Analogue experiments on releasing and restraining bends and their application to the study of the Barents Shear Margin [PDF]
Solid Earth, 2023 The Barents Shear Margin separates the Svalbard and Barents Sea from the North Atlantic. During the break-up of the North Atlantic the plate tectonic configuration was characterized by sequential dextral shear, extension, and eventually contraction and ...
R. H. Gabrielsen +7 more
doaj +1 more source
The Stratigraphic Record of Pre-breakup Geodynamics: Evidence from the Barrow Delta, offshore Northwest Australia [PDF]
, 2016 The structural and stratigraphic evolution of rift basins and passive margins has been widely studied, with many analyses demonstrating that delta systems can provide important records of post-rift geodynamic processes.
Bastow, ID +4 more
core +2 more sources