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Abstract

A detailed structural analysis has been carried out in the area named "Tiszaföldvár-Kiskunfélegyháza" (south-western part of the Great Hungarian Plain, between Tisza and Danube rivers) based on the integrated interpretation of 1000 km 2D migrated seismic time sections, lithological data from boreholes and some well-logs.

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/content/papers/10.3997/2214-4609.201409725
1995-05-29
2024-04-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409725
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