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Tertiary structural evolution of the southern Rhodope metamorphic province: a fundamental revision

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Abstract

The Rhodope province is conventionally interpreted as a continental fragment that was caught between Apulia and Europe and deformed and metamorphosed in the hinterland of the Hellenic collisional orogen. Geologic mapping in the Strymon Valley region of northeastern Greece augmented by new U-Pb and 40Ar/ 39Ar geochronologic data support an alternative view that the southwestern Rhodope province represents the core of an Alpine collisional orogen that was extended and tectonically unroofed by a succession of three late Cenozoic low-angle normal fault systems that alternated in polarity.

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Additional publication details

Publication type:
Conference Paper
Publication Subtype:
Conference Paper
Title:
Tertiary structural evolution of the southern Rhodope metamorphic province: a fundamental revision
Volume:
30
Issue:
1
Year Published:
1994
Language:
English
Publisher:
Ellenike Geologike Etaireia
Publisher location:
Athens, Greece
Description:
11 p.
Larger Work Title:
Proceedings of the 7th congress of the Geological Society of Greece with emphasis on the geology of Macedonia and Thrace
First page:
79
Last page:
89
Conference Title:
7th Congress of the Geological Society of Greece, with Emphasis on the Geology of Macedonia and Thrace
Conference Location:
Thessaloniki, Greece
Conference Date:
May 25-27, 1994
Country:
Greece
Other Geospatial:
Strymon Valley