Palaeofluid evolution in a fractured basalt hosted reservoir in the Üllés-Ruzsa-Bordány area, southern sector of the Pannonian Basin

<p>Extensive Miocene volcanic activity produced basaltic and pyroclastic successions, which were penetrated by many wells in the area of &Uuml;ll&eacute;s-Ruzsa-Bord&aacute;ny, in the western and central part of the Great Hungarian Plain. The Kecel Basalt comprises primary porosity...

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Hlavní autoři: Barbara Szabó, Félix Schubert, Tivadar M. Tóth, Gábor Steinbach
Médium: Artigo
Jazyk:Inglês
Vydáno: Croatian Geological Survey 2016-10-01
Edice:Geologia Croatica
Témata:
fractured basalt reservoir, Pannonian Basin, zeolite minerals, fluid inclusion, hydrocarbon-bearing fluid inclusions, fluorescence
On-line přístup:http://www.geologia-croatica.hr/ojs/index.php/GC/article/view/677
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