Abstract

A probabilistic description of subsurface lithologic structures can be established by inverting multidisciplinary geophysical data constrained by geological and geostatistical priors. The methodology is based on the joint modelling of several media properties and on a statistical description of the relationships between them. The information provided by the geophysical data and the geological and geostatistical priors is represented by probability density functions (pdf) that are combined into a posterior pdf composed by: (1) a prior pdf in the space of the primary (lithologic) model parameters, (2) a pdf of the secondary (physical) model parameters conditional to the primary model parameters and (3) a joint likelihood function that is the product of the independent likelihood functions for each observed geophysical field. Applying a Markov chain sampling method enables a large sample of joint models to be generated from the posterior pdf. The true configuration of the media is then determined from the representation of models pulled from the chain and the elaboration of statistics from the large sample of posterior joint models. The method was used to invert gravity and magnetic data jointly characterising the mass density field, the magnetic susceptibility field and the lithotype field along two 2-D sections of the geological units in the Cadomian belt of northern Brittany. Besides generating 106 joint models consistent with the observations and priors, some features of the joint models and the statistical tomographic images provided additional insights to the geologic configuration of the area. For example, the Main Cadomian Thrust shows an irregular geometry that could have resulted from the belt emplacement and/or from Variscan tectonism, and the Hercynian granitic intrusion shows a deep subsurface continuation. The cosimulation of magnetic susceptibility and mass density inside each lithologic region was performed according to a multivariate Gaussian model or a mixed multivariate Gaussian functions model that was developed specially to describe multimodal distributed properties.

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call

Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.