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    Estimation of petrophysical parameters by linearized inversion of angle domain pre-stack data

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    We describe a linear Bayesian inversion method to estimate the relevant petrophysical properties of the media forming a reflecting interface from the observations of amplitude variation with incidence angle. Three main steps characterize the proposed approach: – information from borehole logs are statistically analysed to estimate the empirical models that describe the functional relationship between petrophysical (e.g. porosity, saturation, pressure or depth) and seismic variable(P and S velocities and density); – the pure-mode (PP) reflection coefficient is parameterized in terms of the relevant petrophysical variables and is linearized in order to implement the linear inversion; – the sought petrophysical parameters are estimated from the seismic reflected amplitudes by applying the linearized inversion where a priori information, data and model errors and solutions are described by probability density functions. We test the method on synthetic and real data relative to reflections from a shale/gas-sand interface where the amplitude versus angle response, besides the lithological contrast, is mainly controlled by the saturation and porosity of the sand layer. The outcomes of the linearized inversion are almost identical to those obtained by a previously developed non-linear inversion method demonstrating the applicability of the linear inversion. It turns out that the gas-sand saturation in the range 0%–95% is a poorly resolved parameter while the porosity is the best resolved parameter. The issues of robustness and resolution of the inversion are discussed either through singular value decomposition analysis or the observation of the a posteriori probability density functions. The linear inversion algorithm, compared with the previously developed non-linear method, reduces significantly the computation time allowing for more extensive applications

    Integrated Geophysical Exploration Technologies for deep fractured geothermal systems (I-GET) SECOND ANNUAL REPORT: Nov. 2006 – Oct. 2007

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    The activities carried out by the University of Pisa (Unipi) in the reporting period refer to the following work-packages: WP 3 GEOPHYSICAL MEASUREMENTS & DATA PROCESSING The following activities have been carried out by Unipi : - azimuthal analysis of the seismic signal amplitudes reflected from the geothermal targets; - AVO analysis on a selected 2D profile from the 3D seismic volume. WP 5 –INTEGRATED INTERPRETATION Unipi has participated in the interpretation carried out by the ENEL colleagues of the observed seismic anomalies and in particular in the assessment of their relations with the producing geothermal targets

    Integrated Geophysical Exploration Technologies for deep fractured geothermal systems (I-GET) FIRST ANNUAL REPORT: Nov. 2005 – Oct. 2006

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    The activities carried out by the University of Pisa (Unipi) in the reporting period refer to the following work-packages: WP 2 AVAILABLE DATA FROM SELECTED EUROPEAN SITES WITH RESPECT TO EXPLORATION TECHNOLOGY Unipi has contributed to the selection of appropriate subsets of the 3D seismic data acquired in the Travale test site. The selected data are the input for the processing carried out by Unipi in the frame of WP3. WP 3 GEOPHYSICAL MEASUREMENTS & DATA PROCESSING The following activities have been carried out by Unipi from November 2005 to October 2006: - selection and reprocessing of appropriate subsets of the Travale seismic 3D dataset - simulation of several acquisition geometries for the Gross Shonebeck site, participation to the acquisition and analysis of the recorded data
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