To determine the geophysical structure of a region, we measure seismic travel times and reconstruct velocities at different depths from this data. There are several algorithms for solving this inverse problem, but these algorithms do not tell us how accurate these reconstructions are. Traditional approach to accuracy estimation assumes that the measurement errors are independently normally distributed. Problem: the resulting accuracies are not in line with geophysical intuition. Reason: a typical error is when we miss the first arrival of the seismic wave; it is not normal (bounded by the wave period T) and not independent. Typically, all we know is the upper bound D on the measurement error, so when the measured value is X, we conclude tha...
International audienceEarthquake hypocentre locations are crucial in many domains of application (ac...
In many practical application, we process measurement results and expert estimates. Measur...
Measured scientific data make possible a quantitative analysis of observations (e.g., a seismometer ...
In many real-life situations, we have several types of uncertainty: measurement uncertainty can lead...
Combining uncertainty models within cyberinfrastructure is a challenging problem. The main objective...
This paper examines downhole measurement inaccuracy with respect to the sampling interval by utilizi...
In many engineering applications, we have to combine probabilistic and interval uncertainty. For exa...
Seismic tomography is now a common approach to estimating velocity structure of the Earth, regardles...
Seismic tomography is a powerful tool for illuminating Earth structure across a range of scales, but...
Quantifying uncertainty in models derived from observed seismic data is an important issue in explor...
In many practical application, we process measurement results and expert estimates. Measurements and...
Moveout velocities sampled frequently along seismic horizons on a selection of seismic lines are use...
We attempt to address two issues in seismic data processing: 1) quantifying the various forms of err...
In many engineering applications, we have to combine probabilistic, interval, and fuzzy uncertainty....
Seismic tomography is a powerful tool for illuminating Earth structure across a range of scales, but...
International audienceEarthquake hypocentre locations are crucial in many domains of application (ac...
In many practical application, we process measurement results and expert estimates. Measur...
Measured scientific data make possible a quantitative analysis of observations (e.g., a seismometer ...
In many real-life situations, we have several types of uncertainty: measurement uncertainty can lead...
Combining uncertainty models within cyberinfrastructure is a challenging problem. The main objective...
This paper examines downhole measurement inaccuracy with respect to the sampling interval by utilizi...
In many engineering applications, we have to combine probabilistic and interval uncertainty. For exa...
Seismic tomography is now a common approach to estimating velocity structure of the Earth, regardles...
Seismic tomography is a powerful tool for illuminating Earth structure across a range of scales, but...
Quantifying uncertainty in models derived from observed seismic data is an important issue in explor...
In many practical application, we process measurement results and expert estimates. Measurements and...
Moveout velocities sampled frequently along seismic horizons on a selection of seismic lines are use...
We attempt to address two issues in seismic data processing: 1) quantifying the various forms of err...
In many engineering applications, we have to combine probabilistic, interval, and fuzzy uncertainty....
Seismic tomography is a powerful tool for illuminating Earth structure across a range of scales, but...
International audienceEarthquake hypocentre locations are crucial in many domains of application (ac...
In many practical application, we process measurement results and expert estimates. Measur...
Measured scientific data make possible a quantitative analysis of observations (e.g., a seismometer ...