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Los Angeles Basin
Imaging Complex Structures of the Los Angeles Basin via Adjoint‐State Travel‐Time Tomography
Fault Damage Zone Effects on Ground Motions during the 2019 M w 7.1 Ridgecrest, California, Earthquake
A Partially Nonergodic Ground‐Motion Model for Cascadia Interface Earthquakes
Origin of the Palos Verdes Restraining Bend and Its Implications for the 3D Geometry of the Fault and Earthquake Hazards in Los Angeles, California
Ground motions in urban Los Angeles from the 2019 Ridgecrest earthquake sequence
The 2018 update of the US National Seismic Hazard Model: Ground motion models in the western US
The 2018 update of the US National Seismic Hazard Model: Overview of model and implications
Quantification of the Influence of Deep Basin Effects on Structural Collapse Using SCEC CyberShake Earthquake Ground Motion Simulations
Evaluation of Building Collapse Risk and Drift Demands by Nonlinear Structural Analyses Using Conventional Hazard Analysis versus Direct Simulation with CyberShake Seismograms
Martian gullies: a comprehensive review of observations, mechanisms and insights from Earth analogues
Abstract Upon their discovery in 2000, Martian gullies were hailed as the first proof of recent (i.e. less than a few million years) flowing liquid water on the surface of a dry desert planet. Many processes have been proposed to have formed Martian gullies, ranging from liquid-water seepage from aquifers, melting of snow, ice and frost, to dry granular flows, potentially lubricated by CO 2 . Terrestrial analogues have played a pivotal role in the conception and validation of gully-formation mechanisms. Comparison with the terrestrial landscape argues for gully formation by liquid-water debris flows originating from surface melting. However, limited knowledge of sediment transport by sublimation is a critical factor in impeding progress on the CO 2 -sublimation hypothesis. We propose avenues towards resolving the debate: (a) laboratory simulations targeting variables that can be measured from orbit; (b) applications of landscape-evolution models; (c) incorporation of the concept of sediment connectivity; (d) using 3D fluid-dynamic models to link deposit morphology and flow rheology; and (e) a more intense exchange of techniques between terrestrial and planetary geomorphology, including quantitative and temporal approaches. Finally, we emphasize that the present may not accurately represent the past and that Martian gullies likely formed by a combination of processes.
Structure of the Northern Los Angeles Basins Revealed in Teleseismic Receiver Functions from Short‐Term Nodal Seismic Arrays
Poroelastic stress changes associated with primary oil production in the Los Angeles Basin, California
A versatile solution for the gravity anomaly of 3D prism-meshed bodies with depth-dependent density contrast
Potentially Induced Earthquakes during the Early Twentieth Century in the Los Angeles Basin
Comparison of Equivalent Linear and Nonlinear Site Response Analysis Results and Model to Estimate Maximum Shear Strain
Chemometric recognition of genetically distinct oil families in the Los Angeles basin, California
2014 Update to the National Seismic Hazard Model in California
Los Angeles Basin: A Tectonically Complex Rift with Exceptionally Rich Petroleum Concentrations
Abstract The Los Angeles basin is a Neogene rift containing a nearly ideal petroleum system. Highly organicrich strata accumulated slowly during tectonic rotation, followed by rapid subsidence and burial beneath thick successions of submarine fan deposits and nonmarine sediments. Late Miocene and Pliocene slope-channel and basin-floor fan sandstones are the main reservoirs. Most petroleum accumulations have been found in faulted anticlines that are associated with the principal structures of the basin and that have been greatly enhanced and modified by transpressional tectonics during the past 6 million years. The basin’s 68 named oil fields probably originally contained more than 40 billion barrels of oil in place. In spite of many years of production, large volumes of technically recoverable petroleum remain in undiscovered accumulations, as additional recoverable oil in existing fields, and possibly in source-rock system reservoirs. Additional large-scale development is problematic, however, owing to the complexities of oil production within a modern megacity.