2012
DOI: 10.1016/j.gloplacha.2011.05.005
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Interaction of mantle dynamics, crustal tectonics, and surface processes in the topography of the Romanian Carpathians: A geomorphological approach

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Cited by 46 publications
(31 citation statements)
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References 81 publications
(176 reference statements)
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“…The imprints of these processes are reflected in the form of changes of local relief, drainage pattern, hypsometry, steepness, and channel slope relationship [2][3][4][5][6][7][8]. These parameters can be used to quantitatively characterize the relationship between shallow and deeper crustal structure, and geomorphic processes [1,9]. The dry land fluvial systems of intraplate Kachchh rift basin, allow us to study the effects and linkage between brittle -ductile dynamics and surface processes on landscape evolution.…”
Section: Introductionmentioning
confidence: 99%
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“…The imprints of these processes are reflected in the form of changes of local relief, drainage pattern, hypsometry, steepness, and channel slope relationship [2][3][4][5][6][7][8]. These parameters can be used to quantitatively characterize the relationship between shallow and deeper crustal structure, and geomorphic processes [1,9]. The dry land fluvial systems of intraplate Kachchh rift basin, allow us to study the effects and linkage between brittle -ductile dynamics and surface processes on landscape evolution.…”
Section: Introductionmentioning
confidence: 99%
“…[11]; shows location of earthquake epicenters. Focal mechanisms (1)(2)(3)(4)(5)(6)(7)(8)(9)(10)(11)(12)(13)(14)(15)(16) plotted in the figure are after [12][13][14][15]. (C) CARTOSAT-DEM driven local relief map of Wagad Highland.…”
Section: Introductionmentioning
confidence: 99%
“…The DEM was prepared using the Hydrological tool in the ESRI TM ArcGIS software; the same tool, in association with the free package ET Geowizard, was also used for deriving drainage network, streams and relief parameters. The geo-morphometric analyses include the computation and discussion of stream length-gradient (SL) index (Hack 1973;Troiani and Della Seta 2008), filtered topography (Molin et al 2012), local relief (Scotti et al 2013 and reference therein), and regional swath profiles (Burbank 1992;Molin et al 2012 and reference therein). Geo-morphometry aimed at locating the anomalies on longitudinal stream-profiles related to active tectonics and at better understanding of the regional Quaternary morphoevolution of drainage network and relief.…”
Section: Methodsmentioning
confidence: 99%
“…60 km in length, strikes roughly NW-SE, along the general direction of the principal structures of the central Apennines. To compute the swath profiles, we sampled the ASTER GDEM elevation dataset every 28 m inside three 5-km-wide straps, in agreement with the method reported by Molin et al (2012); this procedure allows to process topography within the three swaths and obtain the maximum, minimum and mean topography profiles (Fig. 4a).…”
Section: Geostatistical Analyses Of Topographymentioning
confidence: 99%
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