1887

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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/content/papers/10.3997/2214-4609.201407192
1998-09-14
2020-11-30
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201407192
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