Landscape response to recent tectonic deformation in the SW Pannonian Basin: Evidence from DEM-based morphometric analysis of the Bilogora Mt. area, NE Croatia

Matoš, Bojan; Pérez-Peña, Jose Vicente; Tomljenović, Bruno

doi:10.1016/j.geomorph.2016.03.020

Cited by 49 publications

(19 citation statements)

References 68 publications

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“…2), ob vi ously in di cate on go ing de for ma tion in the Bilogora that may be as so ci ated to ac tive fault ing. In the work pre sented by Matoš (2014) and Matoš et al (2016), re cent tec tonic ac tiv ity in Bilogora is sup ported by DEM-based land scape anal y sis with de lin ea tion of the morphometric pa ram e ters, and struc tural anal y sis of the 2D seis mic sec tions in the wider Bilogora area (Fig. 5).…”

Section: Discussion With Conclusionmentioning

confidence: 99%

“…5 and 6B) were se lected ac cord ing to the re sults of the DEM-based land scape morphometric anal y sis per formed in ESRI ArcGIS, and struc tural anal y sis and fault mod el ling of 2D seis mic re flection pro files and ex plo ra tion wells per formed us ing Pe trel Seismic to Sim u la tion Soft ware ( TM Schlumberger) ( Fig. 6B; Matoš, 2014;Matoš et al, 2016).…”

Section: Methodology Of Ground Penetrating Radar Profilingmentioning

confidence: 99%

“…Kalnik Fault Zone (KFZ) and DDBFZ (Figs. 1 and 2) re spec tively (Herak et al, 2009;Matoš et al, 2016).…”

Section: Introductionmentioning

confidence: 91%

“…The tec tonic evo lu tion of Bilogora, rep re sent ing a NE fragment of the Cro atian part of the Pannonian Ba sin Sys tem (CPBS), is linked with the youn gest tec tonic stage in evo lu tion of the Pannonian Ba sin Sys tem (PBS) (e.g., Prelogoviae et al, 1998;Luèiae et al, 2001;Malviae et al, 2003;Saftiae et al, 2003;Malviae and Veliae, 2011;Matoš et al, 2016). The tec tonic evo lution of the PBS started with the Late Oligocene to Early Miocene col li sion be tween the Adria Microplate and the Eu ro pean Plate that yielded an E-di rected ex tru sion of the ALCAPA crustal block, and an E-W di rected ex ten sion of the PBS embayment with for ma tion of NNW-SSW strik ing rift-and wrench -re lated troughs (Royden and Horváth, 1988;Nagymarosy and Müller, 1988;Ratsch bacher, 1991;Fodor et al, 1998;Tari and Pamiae, 1998;Tari et al, 1999;Horváth and Tari, 1999;Steininger and Wessely, 1999;Lenkey et al, 2002;Csontos and Vörös, 2004;Usta szewski et al, 2008).…”

Section: Tectonic Setting Geological Setting Of the Study Areamentioning

confidence: 99%

“…Con di tioned by the sed i ment source area and dis tinc tive cli mate os cil la tions (i.e. gla cial and inter gla cial stages) in the Qua ter nary, sed i men ta tion in the Bilogora area was ge net i cally linked to the Drava River drainage sys tem and cy clic de po si tion of the weakly-to poorly-consol i dated gravel strata al ter nat ing with sands, silts, soft clays, and oc ca sion ally lig nite beds (Babiae et al, 1978;Galoviae et al, 1981;Korolija et al, 1986;Markoviae, 1986;Heaeimoviae, 1987;Šimuniae et al, 1994;Luèiae et al, 2001;Veliae et al, 2002;Saftiae et al, 2003;Matoš et al, 2016). In the Qua ter nary, aggradational de po si tion of the Drava River drain age sys tem de termined the for ma tion of four river ter races.…”

Section: Tectonic Setting Geological Setting Of the Study Areamentioning

confidence: 99%

See 4 more Smart Citations

Quaternary fault activity in the SW Pannonian Basin: GPR surveying in Bilogora (NE Croatia)

Matoš

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Section: Discussion With Conclusionmentioning

confidence: 99%

Section: Methodology Of Ground Penetrating Radar Profilingmentioning

confidence: 99%

“…Kalnik Fault Zone (KFZ) and DDBFZ (Figs. 1 and 2) re spec tively (Herak et al, 2009;Matoš et al, 2016).…”

Section: Introductionmentioning

confidence: 91%

Section: Tectonic Setting Geological Setting Of the Study Areamentioning

confidence: 99%

Section: Tectonic Setting Geological Setting Of the Study Areamentioning

confidence: 99%

See 3 more Smart Citations

Quaternary fault activity in the SW Pannonian Basin: GPR surveying in Bilogora (NE Croatia)

Matoš

Zajc

Kordić

et al. 2016

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Competition of deltaic feeder systems reflected by slope progradation: a high-resolution example from the Late Miocene-Pliocene, Drava Basin, Croatia

Špelić

Kovács

Saftić

et al. 2023

Int J Earth Sci (Geol Rundsch)

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The thick Lake Pannon sedimentary record provides insights into the downdip and lateral development of stratigraphic surfaces through the analysis of the basin-scale clinoform progradation. The clinoform architecture from the eastern part of the Drava Basin (Pannonian Basin System) was interpreted to reflect the base-level changes. A major downlap surface interpreted as a flooding event followed by rejuvenation of slope progradation was recognized on 2D seismic sections. Detailed 3D seismic interpretation combined with well data revealed that the large sigmoidal and the overlying small oblique clinoform sets that downlap the large one only apparently produce the geometry of a maximum flooding surface. Instead, the 3D mapping revealed the influence of two competing slope systems arriving from the north and northwest. Lateral switching of sediment input, similar to many recent deltaic systems. e.g., Danube and Po rivers led to the variability of stratigraphic surfaces, lithology, and thickness, which resulted in non-uniform shelf-edge migration. These observations were supported by forward stratigraphic modeling simulating different scenarios, which led to the generation of the depositional architecture with an apparent maximum flooding surface. This study also implies the potential pitfalls in basin analysis based only on scarce 2D seismic and emphasizes the role of lateral variations in sediment input controlling the depositional architecture.

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Lineament depth deduction using geomorphometry and 3D Euler solution

El Koundi,

Dhaoui,

El Ghali

2024

Acta Geophys.

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In this paper, we present a novel method for determining the depth of lineaments using satellite gravity data, which we test in the Sahel of Sfax area (eastern Tunisia). This region has a relatively flat topography with few significant discontinuities at the surface.As a first step, we used morphometric indices such as slope, aspect, and hydrographic network, calculated from SRTM-DEM, to generate separate lineament maps. We then combined these lineaments into a synthetic lineament map, which showed a high level of agreement with the Bouguer anomaly map derived from satellite gravity data and with previous studies that used geophysical data (seismic and gravity). We also validated the lineament map using field data.By fusing these lineaments with the 3D Euler solution map, we were able to deduce the depth classification of the lineaments. Our results demonstrate the effectiveness of our proposed method in estimating the depth of lineaments and its potential to provide valuable insights into the subsurface geology of an area. This method can be a useful tool for mineral exploration, hydrocarbon exploration, and geohazard assessments.

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Landscape response to recent tectonic deformation in the SW Pannonian Basin: Evidence from DEM-based morphometric analysis of the Bilogora Mt. area, NE Croatia

Cited by 49 publications

References 68 publications

Quaternary fault activity in the SW Pannonian Basin: GPR surveying in Bilogora (NE Croatia)

Quaternary fault activity in the SW Pannonian Basin: GPR surveying in Bilogora (NE Croatia)

Competition of deltaic feeder systems reflected by slope progradation: a high-resolution example from the Late Miocene-Pliocene, Drava Basin, Croatia

Lineament depth deduction using geomorphometry and 3D Euler solution

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