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Abstract
Chapter from:
Chapter 7
The Balkan Thrust Wedge and Foreland Basin of Eastern Bulgaria:
Structural and Stratigraphic Development
H.D. SinclairThe Balkan Thrust Wedge and Foreland Basin of Eastern Bulgaria: Structural and Stratigraphic Development
The University of Birmingham
Edgbaston, Birmingham, United Kingdom S.G. Juranov G. Georgiev
Sofia University "St. Kliment Ohridski"
Sofia, Bulgaria
P. Byrne
British Gas Exploration and Production Limited
Reading, Berkshire, United Kingdom
N.P. Mountney
The University of Birmingham
Edgbaston, Birmingham, United Kingdom
ABSTRACT
cross
section
can be generated by the integration
of coastal exposures, with deeper level constraint from onshore and offshore seismic data.
In this
section
, the Balkans comprise two large synclines bounded by major faults. This
folding and thrusting detached at a horizon within the Jurassic succession at ~5 km depth.
Section
restoration across the Balkans from the remnants of the volcanic arc in the south
to the Balkan thrust front in the north gives a minimum of 18 km of shortening.
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