A 3D Full Stress Tensor Model for Oklahoma

The stress tensor is an important property for upper crustal studies such as those that involve pore fluids and earthquake hazards. At tectonic plate scale, plate boundary forces and mantle convection are the primary drivers of the stress field. In many local settings (10–100 s of km and

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Bibliographische Detailangaben
Veröffentlicht in:	Journal of geophysical research. Solid earth 2021-04, Vol.126 (4), p.n/a
Hauptverfasser:	Chai, Chengping, Delorey, Andrew A., Maceira, Monica, Levandowski, Will, Guyer, Robert A., Zhang, Haijiang, Coblentz, David, Johnson, Paul A.
Format:	Artikel
Sprache:	eng
Schlagworte:	Boreholes Computational fluid dynamics Convection Crystals Density Earthquakes Elasticity Finite element method Fluids Forces Geological faults Geological hazards Geophysics GEOSCIENCES Gravity Heterogeneity joint inversion Mantle convection Mathematical analysis Oklahoma Orientation Plate boundaries Plate tectonics Plates (tectonics) S waves Seismic activity Seismic hazard Stress Stress distribution stress model surface‐wave dispersion Tensors Three dimensional models Travel time travel times Velocity Wave dispersion Wave velocity
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Beschreibung
Zusammenfassung:	The stress tensor is an important property for upper crustal studies such as those that involve pore fluids and earthquake hazards. At tectonic plate scale, plate boundary forces and mantle convection are the primary drivers of the stress field. In many local settings (10–100 s of km and
ISSN:	2169-9313 2169-9356
DOI:	10.1029/2020JB021113