Kontaktne i strukturne odlike karsta Dževrinske grede:
Gespeichert in:
| 1. Verfasser: | |
|---|---|
| Format: | Buch |
| Veröffentlicht: |
Beograd
Geografski Inst. Jovan Cvijić
2008
|
| Schriftenreihe: | Posebna izdanja / Geografski Institut Jovan Cvijić
72 |
| Schlagworte: | |
| Online-Zugang: | Inhaltsverzeichnis Abstract |
| Beschreibung: | PST: Karst of the ridge Dževrinska Greda - contact features and structural characteristics. - In kyrill. Schr., serb. - Zsfassung in engl. Sprache |
| Beschreibung: | 163 S. Ill., graph. Darst., Kt. 24 cm |
| ISBN: | 9788680029412 |
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Datensatz im Suchindex
| _version_ | 1804149545505914880 |
|---|---|
| adam_text | САДРЖАЈ
Увод
7
Појам контактног
карета
9
Џевринска
греда:
опште геолошке, геоморфолошке
и карстолошке
одлике
21
Регионални
прикази са геоморфолошким
карактеристикама
36
Џеврински камен
36
Предео Кашајне
39
Средњи део греде,
са неточним
кречњачким изданцима
53
Предео Дрењара
68
Јужни
део греде, у сливу Реке
101
Кинематика
Џевринског раседа
и
њен утицај
на
еволуцију
карста
105
Хидролошке карактеристике
131
Закључци, дискусија
и
нерешена
питања
149
Литература
156
Summary
162
SUMMARY
Thanks to its extremely elongated shape (length
18
km, average width
250
m),
karst
of the ridge
Dževrinska
Greda
has all the conditions for the development
of contact
karst
and fiuviokarst. Its dimensions make it a perfect case study for
scientific interpretation of stripe
karst
(as described by
Lauritzen, 2001).
Over¬
lapping allogenic influences from both sides of the ridge (concentrated allogenic
water input, huge input of mechanical sediments) have caused modifications in
karst
development.
Following the general inclination of the area, most surface streams flow
from the west to the east, rushing into the limestone ridge on their way. The main
surface streams, that are of permanent character, and rich in water, carry out with
their surface flow, forming the through gorges. On the other hand, weaker surface
streams, of seasonal character, mostly sink into limestone, continuing with their
flow through the
karst
conduits, until their reappearance on the surface. Consid¬
ering a great number of concentrated allogenic input points
(22
stream-sinks, or
ponors) on a relatively small limestone surface (only
4,4
km2, without eastern
limestone outcrops), we can say that the
karst
of the ridge
Dževrinska
Greda
is
very well developed. This has been confirmed by exploration of considerable
lengths of cave passages per unit of the karstic surface. Up to now,
34
caves have
been explored on
Dževrinska
Greda,
with the total length of surveyed cave pas¬
sages exceeding
6
km. The morphology of the cave passages is also under a strong
allogenic influence, which is mostly related to great quantities of clastic sediment
infill. These infills have caused formation of numerous paragenetic flat ceilings,
paragenetic pendants, chokes in narrow passages resulting in upstream flooding,
etc. Very similar morphological characteristics of caves are present in the caves
of
Mehedinţi
plateau in Romania, in the continuation of
Dževrinska
Greda,
espe¬
cially in the longest cave in that area,
Topolniţa-Epuran
system
(20,5
km long).
Another factor that had a crucial influence on direction and dynamics of
karst
development is definitely the activity of the
Dževrin
fault, along which the
limestones of
Dževrinska
Greda
have been uplifted to the surface. The first move¬
ments along this fault were of vertical normal character (uplifting of the eastern
block), while the present movements are dextral transcurrent. Considering the
small width of the limestone ridge, the whole ridge is situated in the zone of the di¬
rect influence of the fault. Fractures of the same orientation as the main fault plane
are present also at the eastern contact. Using the structural-geological field map¬
ping and analysis, the patter of most prominent and most numerous fractures has
KARST
OF THE RIDGE
DŽEVRINSKA
GREDA
-
SUMMARY
163
been obtained. Orientation of these fractures can be explained in accordance with
the former and present tectonic movements in this area. Structural analysis in the
caves has shown that the main directions match those from the surface mapping,
but their importance is varying (fractures that have lead the development of cave
passages can be observed at the surface, but they are not the dominant ones).
Main directions of karstification and, simultaneously, development of
cave passages, have been guided by shear fractures parallel to the
Dževrin
fault.
They are
subvertical,
dipping towards the west. Therefore, the main direction of
groundwater flow on the ridge
Dževrinska
greda
is from the south to the north.
Beside the mentioned shear fractures, it is important to stress the role of ten¬
sion joints formed within dextral transcurrent movement along the
Dževrin
fault.
These joints are striking generally 45°-225° and are present in the zones of most
conspicuous consequences of tectonic activity, like huge collapses, abrupt chang¬
es in cave passages directions, etc.
Location along the huge regional dislocation
-
the
Dževrin
fault
-
has
enabled deep siphonal circulation of part of the
karst groundwaters.
It is one of
the factors that influences the warming of groundwaters (e.g. subthermal springs
Dževrinska Banja
and Banjica). Both subthermal and cold springs are character¬
ised by permanent discharges, and relatively small discharge fluctuations (com¬
pared to typical
karst
springs). Even in periods of extreme drought, the springs are
active, which points to great retention capabilities of
karst
aquifer, either because
of deep groundwater circulation, or thanks to huge quantities of mechanical sedi¬
ments in
karst
conduits, which contributes to longer retention of water. Further¬
more, there is a possibility that
karst
is occasionally fed by groundwaters from the
surrounding fissured aquifers.
In this moment, it is difficult to give a precise chronology of karstification
in this area. Instrumental dating methods, which are the only appropriate indicator
of absolute chronology, were not available at this point of research. In the upcom¬
ing studies, it will be necessary also to pay attention to possible indications of
paleokarst, as well as to
hydrothermal
karstification, considering the presence of
several subthermal
karst
springs. As in many other
karst
areas, multidisciplinary
studies are the best way to find answers to the remaining questions related to the
karst
of
Dževrinska
Greda.
|
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| author | Ćalić, Jelena 1974- |
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| indexdate | 2024-07-10T00:24:44Z |
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| spelling | Ćalić, Jelena 1974- Verfasser (DE-588)102687579X aut Kontaktne i strukturne odlike karsta Dževrinske grede Jelena Ćalić Beograd Geografski Inst. Jovan Cvijić 2008 163 S. Ill., graph. Darst., Kt. 24 cm txt rdacontent n rdamedia nc rdacarrier Posebna izdanja / Geografski Institut Jovan Cvijić 72 PST: Karst of the ridge Dževrinska Greda - contact features and structural characteristics. - In kyrill. Schr., serb. - Zsfassung in engl. Sprache Geografie (DE-588)4020216-1 gnd rswk-swf Grat (DE-588)4423714-5 gnd rswk-swf Karst (DE-588)4129942-5 gnd rswk-swf Serbien Ost (DE-588)4322580-9 gnd rswk-swf Serbien Ost (DE-588)4322580-9 g Grat (DE-588)4423714-5 s Karst (DE-588)4129942-5 s Geografie (DE-588)4020216-1 s DE-604 Geografski Institut Jovan Cvijić Posebna izdanja 72 (DE-604)BV008905274 72 Digitalisierung BSB Muenchen 2 application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=025331677&sequence=000003&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA Inhaltsverzeichnis Digitalisierung BSB Muenchen 2 application/pdf http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=025331677&sequence=000004&line_number=0002&func_code=DB_RECORDS&service_type=MEDIA Abstract |
| spellingShingle | Ćalić, Jelena 1974- Kontaktne i strukturne odlike karsta Dževrinske grede Geografie (DE-588)4020216-1 gnd Grat (DE-588)4423714-5 gnd Karst (DE-588)4129942-5 gnd |
| subject_GND | (DE-588)4020216-1 (DE-588)4423714-5 (DE-588)4129942-5 (DE-588)4322580-9 |
| title | Kontaktne i strukturne odlike karsta Dževrinske grede |
| title_auth | Kontaktne i strukturne odlike karsta Dževrinske grede |
| title_exact_search | Kontaktne i strukturne odlike karsta Dževrinske grede |
| title_full | Kontaktne i strukturne odlike karsta Dževrinske grede Jelena Ćalić |
| title_fullStr | Kontaktne i strukturne odlike karsta Dževrinske grede Jelena Ćalić |
| title_full_unstemmed | Kontaktne i strukturne odlike karsta Dževrinske grede Jelena Ćalić |
| title_short | Kontaktne i strukturne odlike karsta Dževrinske grede |
| title_sort | kontaktne i strukturne odlike karsta dzevrinske grede |
| topic | Geografie (DE-588)4020216-1 gnd Grat (DE-588)4423714-5 gnd Karst (DE-588)4129942-5 gnd |
| topic_facet | Geografie Grat Karst Serbien Ost |
| url | http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=025331677&sequence=000003&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=025331677&sequence=000004&line_number=0002&func_code=DB_RECORDS&service_type=MEDIA |
| volume_link | (DE-604)BV008905274 |
| work_keys_str_mv | AT calicjelena kontaktneistrukturneodlikekarstadzevrinskegrede |