Tectonic Structures Interpretation Using Airborne‐Based LiDAR DEM on the Examples from the Polish Outer Carpathians

Kania, Maciej; Szczęch, Mateusz

doi:10.1002/9781119813392.ch15

Cited by 4 publications

(3 citation statements)

References 14 publications

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“…The study area was cov ered by the car to graphic, lithological and strati graphic study. The car to graphic work con sisted of detailed geo log i cal map ping with the ap pli ca tion of high-res o lu tion dig i tal el e va tion model anal y ses (Szczêch and Cieszkowski, 2021;Kania and Szczêch, 2023). A de tailed study of the var iegated de pos its was con ducted on the ex po sures men tioned above and in cluded geo log i cal de scrip tions, li thol ogy iden ti fi cation, ob ser va tion of bound ary se quences, sed i men tary log ging, field doc u men ta tion, and sam pling for age pur poses.…”

Section: Methodsmentioning

confidence: 99%

The Upper Cretaceous variegated shales in the Ropianka Formation of the Magura Nappe (Outer Carpathians) – age and lithostratigraphic position

Waśkowska,

Szczęch

2023

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The lithological characteristics and age analysis of the variegated Farony Shale are presented for the first time. The Farony Shale occurs in the Lubomierz and Rabka areas in the Bystrica Subunit. It is located within medium- and thin-bedded sandy dominated turbidites of the Campanian–Paleocene Ropianka Formation. It is comprised of red shales laminated or interlayered with strongly bioturbated green shales. Exposures of the Farony Shale are observed along a distance of ~25 km, in the form of a narrow belt. The age of the variegated deposits is estimated based on agglutinated foraminifera to late Campanian–earliest Maastrichtian. Their deposition was associated with low-energy conditions and a temporary limitation of the supply of sandy material to the inner part of the Magura Basin.

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Section: Methodsmentioning

confidence: 99%

The Upper Cretaceous variegated shales in the Ropianka Formation of the Magura Nappe (Outer Carpathians) – age and lithostratigraphic position

Waśkowska,

Szczęch

2023

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“…There are no topological analyses of the lineament networks for the Outer Carpathians. Our previous article (Kania and Szczęch, 2022) was focused on one mountain massif: Gorce Mts. From the tectonic point of view, this massif is quite homogenous, being located in the one tectono-facial unit (Magura unit) with some subunits within (Bystrica and Krynica subunits).…”

Section: Topological Differentiation Of the Networkmentioning

confidence: 99%

“…Digital elevation models are especially useful in areas with lush vegetation. The application of lidar in the Carpathians' flysch-type mountains in geological interpretations was shown, for example, in Kania and Szczęch (2022).…”

Section: Introductionmentioning

confidence: 99%

Geometry and topology of a Polish Outer Carpathian digital-elevation-model-interpreted lineament network in the context of regional tectonics

Kania¹,

Szczęch²

2023

Solid Earth

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Abstract. The Polish part of the Western Outer Carpathian lineament network was analysed based on the Global Multi-resolution Terrain Elevation Data 2010 (GMTED2010) digital elevation model. Lineaments were identified in the visual screening of the hillshade model. To the best of our knowledge, no one has studied the geometrical properties of the network in relation to the topological ones. The NetworkGT QGIS toolbox was applied to identify the nodes and branches of the network as well as to calculate the topology parameters. Our aim was to find differences between the western and eastern parts of the Western Outer Carpathians; therefore, the analyses were carried out in six sectors chosen based on the geographical subdivision in the geological context: three in the north, mainly the Silesian unit, and three in the south, mainly the Magura unit. We found general agreement of the identified network with the photo-lineament map; however, some of the photo-lineaments are not confirmed by a digital elevation model (DEM). We found that the topological parameters of the networks change from west to east but not from north to south. There are areas of increased interconnectivity, especially the Nowy Sącz Basin, where the lineament network may reflect a complicated system of cross-cutting, deep-rooted fault zones in the basement.

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Introduction to “Atlas of Structural Geological and Geomorphological Interpretation of Remote Sensing Images”

Misra

Mukherjee

2022

Atlas of Structural Geological and Geomorphological Interpretation of Remote Sensing Images

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Tectonic Structures Interpretation Using Airborne‐Based LiDAR DEM on the Examples from the Polish Outer Carpathians

Cited by 4 publications

References 14 publications

The Upper Cretaceous variegated shales in the Ropianka Formation of the Magura Nappe (Outer Carpathians) – age and lithostratigraphic position

The Upper Cretaceous variegated shales in the Ropianka Formation of the Magura Nappe (Outer Carpathians) – age and lithostratigraphic position

Geometry and topology of a Polish Outer Carpathian digital-elevation-model-interpreted lineament network in the context of regional tectonics

Introduction to “Atlas of Structural Geological and Geomorphological Interpretation of Remote Sensing Images”

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