Seismic Coupling Quantified on Inferred Décollements Beneath the Western Syntaxis of the Himalaya
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Search indexed NASA NTRS and DOE OSTI research on propulsion, heat transfer, battery materials and energy systems. Follow report and document links to the original sources.
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Examination of effects of sphere and cylinder sinking beneath surface of fluid of uniform viscosity - oceanography
Instrumentation deployment in large arrays by method applicable for use on lunar surface
Computation of impact densities and velocity distribution of debris from lunar surface explosions
Love wave amplitude data satisfying earth model with intrinsic internal friction at depths assumed due to single thermally activated relaxation
Performance tests and criteria for Mars seismometer design models
Determining sway of buildings by low frequency device using pendulum
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The analytic solution to the linear inverse problem provides estimates of the uncertainty of the solution in terms of standard deviations of corrections to a particular solution, resolution of parameter adjustments, and information distribution among the observations. It is shown that Monte Carlo inversion, when properly executed, can provide all the same kinds of information for nonlinear problems. Proper execution requires a relatively uniform sampling of all possible models. The expense of performing Monte Carlo inversion generally requires strategies to improve the probability of finding passing models. Such strategies can lead to a very strong bias in the distribution of models examined unless great care is taken in their application.
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