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Facies analysis, depositional activity, and internal structure of sieve deposits on an active alluvial fan
ID
Novak, Andrej
(
Avtor
),
ID
Vrabec, Marko
(
Avtor
),
ID
Popit, Tomislav
(
Avtor
),
ID
Vižintin, Goran
(
Avtor
),
ID
Šmuc, Andrej
(
Avtor
)
PDF - Predstavitvena datoteka,
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(20,79 MB)
MD5: A81C1CEC2E60E3ADF590B3498EC21FC4
URL - Izvorni URL, za dostop obiščite
https://onlinelibrary.wiley.com/doi/10.1002/esp.5508
Galerija slik
Izvleček
Sieve lobes typically appear in gravel-rich and matrix-poor alluvial fans. Despite being extensively studied, the sieve-lobe facies has been defined largely based on qualitative field observations without quantitative sedimentological analyses. Additionally, depositional activity of sieve lobes has not been monitored over extended periods (monthly to annually) and not directly associated with specific precipitation triggers. Furthermore, the internal geometry of sieve-lobe built alluvial fans has not yet been imaged by subsurface methods. We performed a multi-method analysis of sieve lobes in the Julian Alps (NW Slovenia) on an alpine alluvial fan composed of carbonate gravels. We performed a detailed textural and structural sedimentological analysis of 11 recent sieve lobes differing in size and age. A three-year aerial survey of the alluvial fan surface with a small unmanned aircraft and photogrammetric modelling was used to detect active sieve-lobe evolution. Detected sieve-lobe formation events and volumetric surface changes were paired with triggering precipitation events. Ground-penetrating radar (GPR) profiling depicted the geometry of the sieve-lobe built alluvial fan. The sieve-lobe facies consists of over 80% poorly sorted, open-framework gravels and less than 2% mud. Lobes exhibit downward coarsening and increase in clast mean size. These textural and structural characteristics are present in all sieve lobes regardless of their age and size. Sieve lobes form with a subannual frequency, usually following 24 h rainfall events exceeding 50 mm. Over 1000 m$^3$ of sediment was deposited during these events. The GPR profiles confirm that the studied alluvial fan is formed predominantly by stacked sieve lobes. Quantitative sedimentary analysis of sieve lobes, monitoring of their recent evolution, and depiction of their subsurface geometry—demonstrated in this study—reinforce the challenged concept that sieve lobes are one of the main building blocks of alluvial fans. This work also demonstrates that, under specific conditions, sieving may become the dominant alluvial fan-forming process.
Jezik:
Angleški jezik
Ključne besede:
sieve deposits
,
alluvial fans
,
gravel
,
surface changes
,
rainfall events
Vrsta gradiva:
Članek v reviji
Tipologija:
1.01 - Izvirni znanstveni članek
Organizacija:
NTF - Naravoslovnotehniška fakulteta
Status publikacije:
Objavljeno
Različica publikacije:
Objavljena publikacija
Leto izida:
2023
Št. strani:
Str. 647-664
Številčenje:
Vol. 48, iss. 3
PID:
20.500.12556/RUL-144981
UDK:
55
ISSN pri članku:
0197-9337
DOI:
10.1002/esp.5508
COBISS.SI-ID:
129349123
Datum objave v RUL:
28.03.2023
Število ogledov:
443
Število prenosov:
96
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Objavi na:
Gradivo je del revije
Naslov:
Earth surface processes and landforms
Skrajšan naslov:
Earth surf. processes landf.
Založnik:
Wiley
ISSN:
0197-9337
COBISS.SI-ID:
25358336
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
Program financ.:
Young researchers
Financer:
ARRS - Agencija za raziskovalno dejavnost Republike Slovenije
Številka projekta:
P1-0195
Naslov:
Geookolje in geomateriali
Financer:
ARRS - Agencija za raziskovalno dejavnost Republike Slovenije
Številka projekta:
P2-0268
Naslov:
Geotehnologija
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