Crustal conductivity anomalies in the Carpathian region.

A. Adam, L. Pospisil

Research output: Contribution to journalArticle

9 Citations (Scopus)


The main features of the two most characteristic crustal conductivity anomalies in the Carpathian region, ie the Carpathian and the Transdanubian anomaly are described taking into account other geophysical data. As a common feature the role of tectonics is emphasized in their development. The greatest difference appears in the depths what involves a large temperature difference, too. The Transdanubian anomaly is tentatively interpreted as a pore fluid conduction while in case of the Carpathian anomaly partial melting of sediments is considered with water release during metamorphism or partial melting of crystalline rocks.-from Authors

Original languageEnglish
Pages (from-to)19-34
Number of pages16
JournalActa Geodaetica, Geophysica et Montanistica Hungarica
Issue number1-2
Publication statusPublished - Dec 1 1984

ASJC Scopus subject areas

  • Environmental Science(all)
  • Earth and Planetary Sciences(all)

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