1887

Abstract

MT data along two traverses in the Tucumán Plain<br>were analyzed and it was found that basin sediments<br>are formed mainly by two layers. Then, seismic<br>reflection data coincident to the traverses have been<br>used to constrain the geometry between the basement<br>and the sedimentary rocks. The models obtained<br>from data inversion show a sharp resistivity contrast at the interfaces.

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/content/papers/10.3997/2214-4609-pdb.217.036
2001-10-28
2022-11-28
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.217.036
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