Stochastic uncertainty analysis of gravity gradient tensor components and their combinations
Pejman Shamsipour, Amin Aghaee, Tedd Kourkounakis, Shawn Hood

TL;DR
This paper introduces a stochastic inversion method using cokriging to assess the uncertainty of gravity gradient tensor components, aiding in optimal component selection for subsurface density modeling.
Contribution
It presents a quantitative geostatistical approach to evaluate the importance of gravity gradient tensor components in different scenarios.
Findings
Cokriging variances effectively distinguish tensor components.
The method is demonstrated on real-world data from the New Found dataset.
Uncertainty assessment guides optimal component selection.
Abstract
Full tensor gravity (FTG) devices provide up to five independent components of the gravity gradient tensor. However, we do not yet have a quantitative understanding of which tensor components or combinations of components are more important to recover a subsurface density model by gravity inversion. This is mainly because different components may be more appropriate in different scenarios or purposes. Knowledge of these components in different environments can aid with selection of optimal selection of component combinations. In this work, we propose to apply stochastic inversion to assess the uncertainty of gravity gradient tensor components and their combinations. The method is therefore a quantitative approach. The applied method here is based on the geostatistical inversion (Gaussian process regression) concept using cokriging. The cokriging variances (variance function of the GP)…
Peer Reviews
No public reviews on file for this paper yet. If you reviewed it on a platform where reviews are public (OpenReview, ICLR, NeurIPS, ICML), you can paste yours below so the community can read it here.
Videos
No videos yet. Explain this paper in a talk, walkthrough, or lecture? Add one.
Taxonomy
TopicsGeophysical and Geoelectrical Methods · Geophysics and Gravity Measurements · NMR spectroscopy and applications
MethodsGravity
