Diagenesis and regional metamorphism of the Mesozoic of Aggtelek- Rudabanya mountains (northeast Hungary).

Research output: Contribution to journalArticle

28 Citations (Scopus)

Abstract

A detailed study of the area shows that the grade of regional alteration of the Mesozoic sequences forming the different tectonic units ranges from diagenetic to greenschist facies (chlorite zone) . Based on the petrological data, and on plate tectonic models of the Inner W Carpathians, an attempt has been made to reconstruct the evolution of the region.-R.E.S.

Original languageEnglish
Pages (from-to)349-373
Number of pages25
JournalActa Geologica Hungarica
Volume29
Issue number3-4
Publication statusPublished - Jan 1 1986

ASJC Scopus subject areas

  • Geology

Fingerprint Dive into the research topics of 'Diagenesis and regional metamorphism of the Mesozoic of Aggtelek- Rudabanya mountains (northeast Hungary).'. Together they form a unique fingerprint.

  • Cite this