Geoscience Reference
In-Depth Information
Fig. 2.27
Typical sub-
vertical karst precipice in
Albanian Dinarides
Fig. 2.28
Scheme of fault
ruptures in the region
investigated in 1994, sites of
structural measurements and
base karst forms orientations
in plan view 1—fault with
undetermined type of
displacements; 2—normal
fault; 3—strike-slip fault;
4—thrust; 5—sites of
structural measurements;
6—speleological camps. Fault
numbers follow these in
Fig.
2.25
: 1—Pjetroshan-
Velicikut-Kozhnjc;
2—Dobromiri;
4—Rapsh-Boçani
The youngest (Quaternary and recent) tectonic
stress field is defined by the fault-plane solution of the
only available earthquake focus near the territory
studied.
NE-SW extension) could be found in the recon-
structions for sites 13, 14, and 9. The tectonic stress
field is characterized by changed stress axes as com-
pared to those of the Neotectonic (post-Miocene)
Its
features
(NW-SE
compression
and
