1887

Abstract

The Rhodopean massif during the Paleogene was an area of rich collision magmatism, mainly represented by bimodal volcanism. Its occurences could be connected to the global processes of interaction between the African Continent and the Euro-Asian Platform. An attempt has been made to outline and describe the magmatic centres using a series of regional geophysical maps, compiled by Bulgarian and Greek geophysicists .

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/content/papers/10.3997/2214-4609.201410446
1992-06-01
2020-09-27
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410446
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