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Using a lidar-based height variability method for recognizing and analyzing fault displacement and related fossil mass movement in the Vipava Valley, SW Slovenia
ID
Popit, Tomislav
(
Avtor
),
ID
Rožič, Boštjan
(
Avtor
),
ID
Šmuc, Andrej
(
Avtor
),
ID
Novak, Andrej
(
Avtor
),
ID
Verbovšek, Timotej
(
Avtor
)
PDF - Predstavitvena datoteka,
prenos
(8,84 MB)
MD5: E58FA2BB2B7D46ABAE4828AE7743A941
URL - Izvorni URL, za dostop obiščite
https://www.mdpi.com/2072-4292/14/9/2016
Galerija slik
Izvleček
The northern slopes of the Vipava Valley are defined by a thrust front of Mesozoic carbonates over Tertiary flysch deposits. These slopes are characterized by a variety of different surface forms, among which recent and fossil polygenetic landslides are the most prominent mass movements. We used the height variability method as a morphometric indicator, which proved to be the most useful among the various methods for quantifying and visualizing fossil landslides. Height variability is based on the difference in elevations derived from a high-resolution lidar-derived DEM. Based on geologic field mapping and geomorphometric analysis, we distinguished two main types of movements: structurally induced movement along the fault zone and movements caused by complex Quaternary gravitational slope processes. The most pronounced element is the sliding of the huge rotational carbonate massif, which was displaced partly along older fault structures in the hinterland of fossil rock avalanches and carbonate blocks. In addition to the material properties of the lithology, the level of surface roughness also depends on the depositional processes of the individual sedimentary bodies. These were formed by complex sedimentary events and are intertwined in the geological past. The sedimentary bodies indicate two large fossil rock avalanches, while the smaller gravity blocks indicate translational–rotational slides of carbonate and carbonate breccia.
Jezik:
Angleški jezik
Ključne besede:
slope process
,
surface roughness
,
rock avalanche
,
geomorphometric analysis
,
geological setting
,
deep-seated rotational and translational slides
Vrsta gradiva:
Članek v reviji
Tipologija:
1.01 - Izvirni znanstveni članek
Organizacija:
NTF - Naravoslovnotehniška fakulteta
Status publikacije:
Objavljeno
Različica publikacije:
Objavljena publikacija
Leto izida:
2022
Št. strani:
16 str.
Številčenje:
Vol. 14, iss. 9, art. 2016
PID:
20.500.12556/RUL-145254
UDK:
55
ISSN pri članku:
2072-4292
DOI:
10.3390/rs14092016
COBISS.SI-ID:
105725699
Datum objave v RUL:
14.04.2023
Število ogledov:
614
Število prenosov:
80
Metapodatki:
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Objavi na:
Gradivo je del revije
Naslov:
Remote sensing
Skrajšan naslov:
Remote sens.
Založnik:
MDPI
ISSN:
2072-4292
COBISS.SI-ID:
32345133
Licence
Licenca:
CC BY 4.0, Creative Commons Priznanje avtorstva 4.0 Mednarodna
Povezava:
http://creativecommons.org/licenses/by/4.0/deed.sl
Opis:
To je standardna licenca Creative Commons, ki daje uporabnikom največ možnosti za nadaljnjo uporabo dela, pri čemer morajo navesti avtorja.
Projekti
Financer:
ARRS - Agencija za raziskovalno dejavnost Republike Slovenije
Številka projekta:
P1-0195
Naslov:
Geookolje in geomateriali
Financer:
Drugi - Drug financer ali več financerjev
Program financ.:
International Consortium on Landslides
Številka projekta:
IPL-216
Naslov:
Diversity and Hydrogeology of Mass Movements in the Vipava Valley, SW Slovenia
Financer:
Drugi - Drug financer ali več financerjev
Program financ.:
International Consortium on Landslides Adriatic–Balkan Network
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