Alluvial terrace geometry in French Jura estimated from DC electric and TDEM measurements

J. C. Gourryl; R. Guérin; Y. Albouy; T. Winter

doi:10.3997/2214-4609.201407192

Alluvial terrace geometry in French Jura estimated from DC electric and TDEM measurements
By J. C. Gourryl, R. Guérin, Y. Albouy and T. Winter
Publisher: European Association of Geoscientists & Engineers
Source: Conference Proceedings, 4th EEGS Meeting, Sep 1998, cp-43-00167
ISBN: 978-94-6282-127-9
DOI: https://doi.org/10.3997/2214-4609.201407192

Abstract

The aim of this work is the determination of the neotectonic activity of the Jura mountains. Alluvial terraces are a good index of mountain uplift. Our hypothesis is to use the terrace base as a reference. With the age and altitude variations, we could also calculate the uplift velocity variations during the last hundred thousand years. Then a test of DC electric and TDEM measurements was carried out in the Seille valley (french Jura) for mapping alluvial terraces.

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1998-09-14

2024-04-26

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Alluvial terrace geometry in French Jura estimated from DC electric and TDEM measurements

Abstract

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Characterizing the effect of elastic interactions on the effective elastic properties of porous, cracked rocks

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Laboratory measurements of guided‐wave propagation within a fluid‐saturated fracture