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Fine-Scale Three-Dimensional Characterization of a Reservoir Comprising Braided River Sand Bodies with a Complex Stacking Pattern in a Cratonic Basin
A Method to Generate Initial Fault Stresses for Physics‐Based Ground‐Motion Prediction Consistent with Regional Seismicity
Relative Seismic Source Scaling Based on Pn Observations from the North Korean Underground Nuclear Explosions
NGA-subduction global ground motion models with regional adjustment factors
Ground-motion models for Vrancea intermediate-depth earthquakes
Meso-Cenozoic negative inversion model for the Linhe Depression of Hetao Basin, China
Experimental Research on the Thresholds of Scale-Dependent Dispersivity of Solute Transport
Emergent simplicity despite local complexity in eroding fluvial landscapes
Simplified methods to estimate mean hazard due to updated ground motion model: Application to nuclear power plants in CEUS
Upscaling of outcrop information for improved reservoir modelling – exemplified by a case study on chalk
Nonlinear fault damage zone scaling revealed through analog modeling
The influence of inter- and intra-channel architecture on deep-water turbidite reservoir performance
A test of the efficacy of sand saltation for silt production: Implications for the interpretation of loess
Dune-scale cross-strata across the fluvial-deltaic backwater regime: Preservation potential of an autogenic stratigraphic signature
Fault zone architecture and its scaling laws: where does the damage zone start and stop?
Abstract Damage zones of different fault types are investigated in siliciclastics (Utah, USA), carbonates (Majella Mountain, Italy) and metamorphic rocks (western Norway). The study was conducted taking measurements of deformation features such as fractures and deformation bands on multiple 1D scanlines along fault walls. The resulting datasets are used to plot the frequency distribution of deformation features and to constrain the geometrical width of the damage zone for the studied faults. The damage-zone width of a single fault is constrained by identifying the changes in the slope of cumulative plots made on the frequency data. The cumulative plot further shows high deformation frequency by a steep slope (inner damage zone) and less deformation as a gentle slope (outer damage zone). Statistical distributions of displacement and damage-zone width and their relationship are improved, and show two-slope power-law distributions with a break point at c. 100 m displacement. Bleached sandstones in the studied siliciclastic rocks of Utah are associated with a higher frequency of deformation bands and a wider damage zone compared to the unbleached zone of similar lithology. Fault damage zones in the carbonate rocks of Majella are often host to open fractures (karst), demonstrating that they can also be conductive to fluid flow.
Subduction of trench-fill sediments beneath an accretionary wedge: Insights from sandbox analogue experiments
Fracture attribute and topology characteristics of a geothermal reservoir: Southern Negros, Philippines
Experimental evidence for crustal control over seismic fault segmentation
Multiscale fracture length analysis in carbonate reservoir units, Kurdistan, NE Iraq
A consistent global approach for the morphometric characterization of subaqueous landslides
Abstract Landslides are common in aquatic settings worldwide, from lakes and coastal environments to the deep sea. Fast-moving, large-volume landslides can potentially trigger destructive tsunamis. Landslides damage and disrupt global communication links and other critical marine infrastructure. Landslide deposits act as foci for localized, but important, deep-seafloor biological communities. Under burial, landslide deposits play an important role in a successful petroleum system. While the broad importance of understanding subaqueous landslide processes is evident, a number of important scientific questions have yet to receive the needed attention. Collecting quantitative data is a critical step to addressing questions surrounding subaqueous landslides. Quantitative metrics of subaqueous landslides are routinely recorded, but which ones, and how they are defined, depends on the end-user focus. Differences in focus can inhibit communication of knowledge between communities, and complicate comparative analysis. This study outlines an approach specifically for consistent measurement of subaqueous landslide morphometrics to be used in the design of a broader, global open-source, peer-curated database. Examples from different settings illustrate how the approach can be applied, as well as the difficulties encountered when analysing different landslides and data types. Standardizing data collection for subaqueous landslides should result in more accurate geohazard predictions and resource estimation.