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Journal articles on the topic 'Relationship between tectonics and relief'

Author: Grafiati

Published: 5 June 2025

Last updated: 15 July 2025

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1

Adams, B. A., K. X. Whipple, A. M. Forte, A. M. Heimsath, and K. V. Hodges. "Climate controls on erosion in tectonically active landscapes." Science Advances 6, no. 42 (2020): eaaz3166. http://dx.doi.org/10.1126/sciadv.aaz3166.

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The ongoing debate about the nature of coupling between climate and tectonics in mountain ranges derives, in part, from an imperfect understanding of how topography, climate, erosion, and rock uplift are interrelated. Here, we demonstrate that erosion rate is nonlinearly related to fluvial relief with a proportionality set by mean annual rainfall. These relationships can be quantified for tectonically active landscapes, and calculations based on them enable estimation of erosion where observations are lacking. Tests of the predictive power of this relationship in the Himalaya, where erosion is

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Ivanik, O., L. Tustanovska, and K. Hadiatska. "MAIN CAUSES OF GRAVITATION PROCESSES WITHIN THE MIDDLE DNIEPER REGION." Visnyk of Taras Shevchenko National University of Kyiv. Geology, no. 1 (88) (2020): 6–11. http://dx.doi.org/10.17721/1728-2713.88.01.

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Integrated assessment and analyses of gravitational geological processes impact on the technogene objects is based on a systematic approach to the analysis of the geological environment; creation of geological, mathematical and spatial models of the geological environment, development of analytical tools. The complex application of geological and geomorphological methods (structural-morphometric analysis, comparative tectonics and structural analysis), remote sensing data and GIS technologies made it possible to identify the relationship between the processes of geomorphogenesis and tectogenes

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Kosmowska-Suffczyńska, Danuta. "Relationship Between Relief and Tectonics on the North-Eastern Border of the Holy Cross Mountains." Miscellanea Geographica 2, no. 1 (1986): 31–40. http://dx.doi.org/10.2478/mgrsd-1986-020106.

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4

GHERGHE, A., A. NEDELEA, A. BRICEAG, G. ION, and M. C. MELINTE-DOBRINESCU. "LINKING GEOLOGICAL AND GEOMORPHOLOGICAL FEATURES. CASE STUDY: SLĂNICUL DE BUZĂU VALLEY." Geo-Eco-Marina 26 (2020) (December 31, 2020): 135–56. https://doi.org/10.5281/zenodo.4692291.

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This paper presents the correlation between the geomorphological features of the Slănicul de Buzău Valley and the geological ones, such as the tectonic regime and the type of rocks. We are pointing out that the geomorphology of the valley and the change of the flow direction are linked to the type of rocks and tectonic elements of traversed geological structures. The change of the upper course of the river from NS to WE upstream the Lopătari locality coincides with a major tectonic element, a digitation occurring in the deposits formed by hard compact Paleogene rocks. The upper course deep val

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Ivanik, O., L. Tustanovska, D. Kravchenko, and K. Hadiatska. "ADAPTATION OF THE METHOD OF STRUCTURAL-MORPHOMETRIC ANALYSIS TO THE GIS ENVIRONMENT FOR PALEOGEOMORPHOLOGICAL STUDIES OF THE KANIV DNIEPER." Visnyk of Taras Shevchenko National University of Kyiv. Geology, no. 2 (89) (2020): 6–11. http://dx.doi.org/10.17721/1728-2713.89.01.

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Kaniv Dnieper area is a unique region that has evolved through the Neogene-Quaternary phase. The application of geological and geomorphological methods, remote sensing data and GIS made it possible to identify the genetic relationship between the processes of geomorphogenesis and tectogenesis within the Kaniv Dnieper region, to build a number of geological and geomorphological models. The methodology of structural-morphometric analysis is adapted to the GIS and the process of cartometric constructions is automated. An algorithm for creating order maps of valleys and basal surfaces has been dev

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Ivanik, O., L. Tustanovska, and К. Hadiatska. "NEOTECTONICS AND MORPHOSTRUCTURAL FEATURES OF THE RELIEF OF THE RIGHT BANK OF THE MIDDLE DNIEPER REGION." Visnyk of Taras Shevchenko National University of Kyiv. Geology, no. 4 (99) (2022): 5–11. http://dx.doi.org/10.17721/1728-2713.99.01.

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On the basis of a complex structural-morphometric analysis, methods of remote sensing of the Earth and spatial modeling, the evolution of different-scale morphostructures of the right bank of the Middle Dnieper region is analyzed. Based on the created structural-morphometric models, the features of tectogenesis and morphogenesis during the Neogene-Quaternary time were revealed. The regional and local structures are characterized and the amplitudes of the latest and modern crustal movements within them are determined. The complex relationship between endogenous and exogenous relief formation ha

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Ahmad, Sarfaraz, and Khatib Khan. "Impact of Elevation - Glaciation - Tectonics on landscape characteristics of the watersheds in Bhagirathi valley, Garhwal Himalaya." Journal of The Indian Association of Sedimentologists 37, no. 2 (2020): 141–47. http://dx.doi.org/10.51710/jias.v37i2.110.

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Terrain attributes of watersheds i.e., mean , maximum, minimum elevation, mean slope elevation, mean aspect, HI (Hypsometrical Integral), Plan and Profile curvature index were determined using ASTER DEM in Bhagirathi basin, Uttaarakhand. These attributes are used in determine the impact of elevation, glaciations and tectonic processes on terrain characteristics of the watersheds. The scatter diagrame between altitude and terrain attribute were used to analyse th impact of altitude and impact of glacition is revealed through Box Whisker diagram using moderate and fully glacier watersheds. The r

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Leonov, M. G., E. S. Przhiyalgovskii, A. K. Rybin, and G. G. Shchelochkov. "Features of the Tien Shan newest orogen morphostructure." LITHOSPHERE (Russia) 21, no. 6 (2021): 747–74. http://dx.doi.org/10.24930/1681-9004-2021-21-5-747-774.

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Research subject. The concept of morphostructure implies the presence of a relationship between the relief forms of segments of the Earth’s crust and their structural and material content. This article describes the geological ensembles of the Tien Shan orogen, the tectonic structure and modern relief of which differ in their parameters from the general morphostructural plan and which, therefore, belong to the category of morphostructural anomalies. Materials and methods. The data presented in the article were obtained in the course of field structural-geological and morphostructural study of

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Petrovic, Aleksandar, and Ratomir Veselinovic. "The genesis and evolution of uvalas in Gajina mlaka paleovalley on the Kucaj mountains." Glasnik Srpskog geografskog drustva 92, no. 1 (2012): 91–104. http://dx.doi.org/10.2298/gsgd1201091p.

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The evolution of Gajina mlaka paleovalley from pre-karstic to current phase reveals the complexity of process of transformation of valleys in karst and formation of fluviokarst uvalas. The creation of river network and formation of the valley of Gajina mlaka are related to successive withdrawal of the Pontiac Sea. Predominance of karstic process over fluvial causes the transformation of fluvial morphology into karstic. The degree of transformation depends on relationship of the intensity between these two opposed processes. Karstification covers all parts of Gajina mlaka valley which are built

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Kashyap, Abhishek, Kristen L. Cook, and Mukunda Dev Behera. "Geomorphic imprint of high-mountain floods: insights from the 2022 hydrological extreme across the upper Indus River catchment in the northwestern Himalayas." Earth Surface Dynamics 13, no. 1 (2025): 147–66. https://doi.org/10.5194/esurf-13-147-2025.

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Abstract. The interaction of tectonics, surface processes, and climate extremes impacts how the landscape responds to extreme hydrological events. In 2022, an anomalous precipitation event occurred during the monsoon season along the lower–middle reaches of the upper Indus River, resulting in short-lived high-magnitude flooding and socioeconomic disruption downstream. To understand the spatial relationship between the geomorphic response and climatic controls of this flood event, as well as their primary triggers, we performed a landscape analysis using topographic metrics and quantified the c

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Qureshi, Jahanzeb, Syed Amer Mahmood, Muhammad Khubaib Abuzar, Amer Masood, and Muhammad Shafiq. "Neotectonics of Zindapir Anticline and Sulaiman Fold and Thrust Belt: Inferences from SRTM DEM." International Journal of Economic and Environmental Geology 11, no. 1 (2020): 77–82. http://dx.doi.org/10.46660/ijeeg.vol11.iss1.2020.416.

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The current study deals with the significance of surface dynamics (SDs) and its relationship to tectonics and active erosion in Zindapir Anticline (ZPA) and neighboring Sulaiman Fold and Thrust Belt (SFTB) which is a direct result of transform plate movement between Indo-Pak continent and Eurasia. The Shuttle Radar Topographic Mission Digital Elevation Model SRTM DEM with 30 m resolution was employed to compute SDs; Isobase (IBL), drainage density (DD), relative relief (RR) and vertical dissection (VD) thematic maps for the study area. The results obtained show that the DD, RR, VD and IBL have

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Qureshi, Jahanzeb, Syed Amer Mahmood, Muhammad Khubaib Abuzar, Amer Masood, and Muhammad Shafiq. "Neotectonics of Zindapir Anticline and Sulaiman Fold and Thrust Belt: Inferences from SRTM DEM." International Journal of Economic and Environmental Geology 11, no. 1 (2020): 77–82. http://dx.doi.org/10.46660/ojs.v11i1.416.

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The current study deals with the significance of surface dynamics (SDs) and its relationship to tectonics and active erosion in Zindapir Anticline (ZPA) and neighboring Sulaiman Fold and Thrust Belt (SFTB) which is a direct result of transform plate movement between Indo-Pak continent and Eurasia. The Shuttle Radar Topographic Mission Digital Elevation Model SRTM DEM with 30 m resolution was employed to compute SDs; Isobase (IBL), drainage density (DD), relative relief (RR) and vertical dissection (VD) thematic maps for the study area. The results obtained show that the DD, RR, VD and IBL have

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Expósito, Inmaculada, Alejandro Jiménez-Bonilla, Michele Delchiaro, et al. "Geomorphic signature of segmented relief rejuvenation in the Sierra Morena, Betic forebulge, Spain." Earth Surface Dynamics 10, no. 5 (2022): 1017–39. http://dx.doi.org/10.5194/esurf-10-1017-2022.

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Abstract. The foreland relief of alpine orogenic belts is often rejuvenated due to the intraplate propagation of orogenic deformation. Thus, in these long-lived areas, the localisation of relief rejuvenation may be largely controlled by the reactivation of previous mechanical discontinuities. In this regard, we explored the relationship between the relief rejuvenation pattern and the distribution, geometry, and kinematics of faults in a wide segment of the Betic foreland (Sierra Morena, southern Spain). Specifically, we focused on the forebulge, a WSW–ENE flexural relief that formed, paired to

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Gabdykadyr, A. G., G. T. Issanova, Y. Kh Kakimzhanov, and Long Ma. "ANALYSIS OF SOIL DEGRADATION AND DESERTIFICATION IN SOUTHERN BALKASH DESERT BASED ON GIS." REPORTS 2, no. 330 (2020): 41–48. http://dx.doi.org/10.32014/10.32014/2020.2518-1483.30.

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Desertification and degradation provide a clear picture of global environmental and socio-economic issues. Most of Kazakhstan is located in a desert region, including the suburbs of South Balkhash. The reason is that desertification of the region has a strong influence on natural and anthropogenic factors. To consider the geomorphological state of the region and the problem of desertification of the territory, it is necessary to determine the importance of the process of relief of geological structure and relief of tectonics. In recent years, the environmental situation in Balkhash has deterio

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Marder, Eyal, Tara M. Smiley, Brian J. Yanites, and Katherine Kravitz. "Direct effects of mountain uplift and topography on biodiversity." Science 387, no. 6740 (2025): 1287–91. https://doi.org/10.1126/science.adp7290.

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Biodiversity hotspots in Earth’s mountain ranges suggest a strong connection between topographic development and biological processes. However, it remains unclear whether high biodiversity in mountain ranges is an evolutionary response to the rate of relief generation during mountain building. Focusing on small mammals, such as rodents, we used coupled landscape-biological simulations to show that biodiversity increases with the magnitude and rate of tectonic uplift. This relationship, visible in depositional lowlands over millions of years, underscores the considerable role of mountain buildi

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Lemenkova, Polina. "The geomorphology of the Makran Trench in the context of the geological and geophysical settings of the Arabian Sea." Geology, Geophysics and Environment 46, no. 3 (2020): 205–22. https://doi.org/10.7494/geol.2020.46.3.205.

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The study focuses on the Makran Trench in the Arabian Sea basin, in the north Indian Ocean. The area is tectonically active, with a system of ridges and fracture zones morphologically separating the Arabian Sea. The study examined the relationships between the topographic structure of the Makran Trench and the re- gional settings of the Arabian Sea: geomorphology, sediment thickness, geophysical fields, geology and tectonic lineaments. The methodology is based on the GMT scripting toolset. The spatial analysis includes high-resolu- tion datasets GEBCO, EGM2008, GlobSed and data on tectonics, g

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Anil, M. Pophare Swapnil N. Deshmukh Akshay V. Dhuldhar. "MORPHOMETRIC ANALYSES OF KOLAR RIVER BASIN, CENTRAL INDIA." International Journal of Advance and Applied Research 2, no. 17 (2022): 156–60. https://doi.org/10.5281/zenodo.7053412.

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<strong><em>Abstract</em></strong> <em>Morphometric analyses of Kolar river basin has been carried out with various aspects. The linear, areal and relief aspects of Kolar river basin suggest that river basin has elongated shape with impermeable sub-surface, low infiltration and fine drainage texture. Values of r</em><em>uggedness number fall in higher range; hence basin is more susceptible to erosion. Morphometric </em><em>values infer that the Kolar river basin has, sparse vegetation cover, high relief. Present study has confirmed the prevalence of dendritic drainage pattern, highest of 6<sup

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Rybin, I. V., I. V. Sheverdyaev, and S. A. Misirov. "Morphometric analysis as a method of searching for mineral raw materials using the example of the Dnieper-Donetsk aulakogen." Geodesy and Cartography 1018, no. 4 (2025): 48–55. https://doi.org/10.22389/0016-7126-2025-1018-4-48-55.

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The relevance of the research lies in the study of the relationship between the morphometry of the relief with ore occurrences and deposits. Its purpose is to quantify the physical (topographic) surface of the Earth in order to identify tectonic structures with subsequent rational planning of geological exploration based on determining the morphometry of the work area by comparison with identical natural structures. The object of the study is the region of the Dnieper-Donets aulacogen with the northwest-southeast direction Kharkov- the Caspian Sea and the north-south one from Millerovo to Rost

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Bouramtane, Tarik, Abdessamad Tiouiouine, Ilias Kacimi, et al. "Drainage Network Patterns Determinism: A Comparison in Arid, Semi-Arid and Semi-Humid Area of Morocco Using Multifactorial Approach." Hydrology 7, no. 4 (2020): 87. http://dx.doi.org/10.3390/hydrology7040087.

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Drainage network patterns influence the hydrological response of the watersheds and must be taken into account in the management of the water resource. In this context, it is important to identify the factors that control the configuration of drainage networks in and beyond specific climatic conditions. Here, we study 318 basins spread over three sectors (arid, semi-arid, and semi-humid) of Morocco where seven drainage network patterns have been identified. From each basin, 14 parameters were extracted, describing the relief, geology, morphometry, drainage network, land cover, precipitation, a

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Yasue, Ken-ichi, Daisuke Hirouchi, Takayuki Nakano, Hideo Sakai, Koji Okumura, and Masatomo Umitsu. "Relationship between the tectonic relief and the subsurface geological structure related to strike-slip displacement: a case of the en échelon faults." Journal of the Geological Society of Japan 111, no. 1 (2005): 29–38. http://dx.doi.org/10.5575/geosoc.111.29.

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Kroshko, Yulia, and Myron Kovalchuk. "Structural and lithological model of the Glukhivetsky deposit of eluvial kaolins." Visnyk of V.N. Karazin Kharkiv National University, series Geology. Geography. Ecology, no. 60 (June 1, 2024): 40–55. http://dx.doi.org/10.26565/2410-7360-2024-60-03.

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Introduction. The relevance of this publication is associated with the problem of foundation and developing a raw material base of kaoline raw material in accordance with the demand of the national industry. The purpose of the publication is the development of a digital structural-lithological model of the Glukhovetsky deposit, which displays the causal relationship between the geological structure of the crystalline foundation, the zoning and the material composition of the cortex of the crystalline foundation breeds, the thickness and relief of the surface and the sole of the illegal of the

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Bíl, Michal. "Using GIS to detect neotectonics in the Vsetínské vrchy Mountains and in their surroundings." Geografie 108, no. 2 (2003): 101–14. http://dx.doi.org/10.37040/geografie2003108020101.

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This paper discusses the advantages of GIS and numerical analysis in neotectonic studies. An accurate DEM is important for numerous geomorphic and hydrologic applications, particularly over large areas. The method is illustrated on the DEM of the Vsetínské vrchy Mountains, a 367 square km large area in the east of the Czech Republic. Comparing geological maps with large-scale morphometry shows a relationship between the rock resistance and topography. On average, higher mean elevations and steep slopes correlate well with regions of hard bedrock geology. The results together with new geologica

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PRATT, BRIAN R. "KINNEYIA-TYPE WRINKLE STRUCTURES ON SANDSTONE BEDS: NOT MICROBIALLY INDUCED BUT DEFORMATION FEATURES CAUSED BY SYNSEDIMENTARY EARTHQUAKES." PALAIOS 36, no. 10 (2021): 313–25. http://dx.doi.org/10.2110/palo.2021.015.

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ABSTRACT A category of wrinkle structures, often termed Kinneyia structure or Runzel marks, comprises bedding plane features consisting typically of anastomosing, low-relief, flat-topped ridges with intervening depressions. Topographic relief is usually less than a millimeter. They are locally common on the upper surfaces of fine- to medium-grained sandstone beds interbedded with mudstone deposited in offshore settings, especially in Precambrian and lower Paleozoic strata but as young as Cretaceous. For more than the last two decades these wrinkle structures have been widely regarded as due to

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Gelwick, Katrina D., Sean D. Willett, and Rong Yang. "Geomorphic indicators of continental-scale landscape transience in the Hengduan Mountains, SE Tibet, China." Earth Surface Dynamics 12, no. 3 (2024): 783–800. http://dx.doi.org/10.5194/esurf-12-783-2024.

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Abstract. Landscapes are sculpted by a complex response of surface processes to external forcings, such as climate and tectonics. Several major river captures have been documented in the Hengduan Mountains, leading to the hypothesis that the region experiences exceptionally high rates of drainage reorganization driven by horizontal shortening and propagating uplift. Here we determine the prevalence, intensity, and spatial patterns of ongoing drainage reorganization in the Hengduan Mountains and evaluate the relative timescales of this transience by comparing drainage divide asymmetry for four

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Froemchen, Malte, Ken J. W. McCaffrey, Mark B. Allen, Jeroen van Hunen, Thomas B. Phillips, and Yueren Xu. "Geomorphic expressions of active rifting reflect the role of structural inheritance: a new model for the evolution of the Shanxi Rift, northern China." Solid Earth 15, no. 10 (2024): 1203–31. http://dx.doi.org/10.5194/se-15-1203-2024.

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Abstract. Many rifts are influenced by pre-existing structures and heterogeneities during their evolution, a process known as structural inheritance. During rift evolution, these heterogeneities may aid rift nucleation, rift growth, and the segmentation of faults; encourage the linkage of various segments; or even inhibit the formation of faults. Understanding how structural inheritance influences early rift evolution could be vital for evaluating seismic risk in tectonically active areas. The Shanxi Rift in the north of China is an active rift system believed to have formed along the trend of

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Xu, Dayang, Hu Si, Qianting Hu, and Yunpei Liang. "Quantitative Study on the Stress Distribution Characteristics of Coal Rock with Faults." Geofluids 2022 (February 28, 2022): 1–11. http://dx.doi.org/10.1155/2022/8214322.

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To quantitatively describe the distribution characteristics of stress field of coal rock in fault area, a finite element model was established to study the influence mechanisms of different fault parameters on the stress distribution characteristics of coal rock and a prediction model of the tectonic stress field of a fault-containing coal rock was established based on the numerical simulations. The numerical simulation results show that the coal rock in the hanging wall of a normal fault forms an area of disturbance significantly larger than that in the footwall of the normal fault and revers

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Bartaschuk, Oleksii, Vasyl Suyarko, Oleksandr Chuienko, and Bruce J. Perry. "Tectonic Evolution of the Intra-plate Structures of Sarmatia in the Phanerozoic. 1. Geophysical analysis of structural and substance differentiation of the lithosphere and tectonic divisibility of the Earth's crust." Visnyk of V.N. Karazin Kharkiv National University, series Geology. Geography. Ecology, no. 60 (June 1, 2024): 12–27. http://dx.doi.org/10.26565/2410-7360-2024-60-01.

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Purpose. The structure of the Sarmatia`s llithospheric plate was studied based on the latest integrated geological, geophysical, tectonophysics, aerocosmo-geological, neo-tectonic data and the gravity, magnetic, dense and seismic (GSZ, seismotomography) modeling data. The aim of the study to reveal the nature of heterogeneities of the Sarmatia Lithosphere and their influence on the nature of the process of structural and material differentiation of the Earth's continental crust. Method. A comparative geotectonic analysis of the structure, composition, and relationships of individual layers of

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Fuladi, A., and M. S. Deshmukh. "Hypsometric Analysis of WRC-1 Watershed, Chargarh River Basin, Central India: A Remote Sensing and GIS Approach." Journal of Scientific Research 15, no. 3 (2023): 869–78. http://dx.doi.org/10.3329/jsr.v15i3.64183.

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Hypsometric analysis is a valuable tool for determining the tectonic evolution of a river basin and the erosion susceptibility. It is also important for integrated watershed management, which include selecting suitable locations for groundwater recharge structures and for conservation of soil and water. This type of study can analyze the relationship between horizontal cross sectional area and the altitude of the watershed. It evaluates the hypsometric curve and hypsometric integral, as generated for the WRC-1 watershed, Chargarh river basin through remote sensing and GIS technique. In the pre

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Hergert, T., O. Heidbach, K. Reiter, S. B. Giger, and P. Marschall. "Stress field sensitivity analysis in a sedimentary sequence of the Alpine foreland, Northern Switzerland." Solid Earth Discussions 7, no. 1 (2015): 711–56. http://dx.doi.org/10.5194/sed-7-711-2015.

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Abstract. The stress field at depth is a relevant parameter for the design of subsurface constructions and reservoir management. Yet the distortion of the regional stress field due to local-scale features such as sedimentary and tectonic structures or topography is often poorly constrained. We conduct a stress sensitivity analysis using 3-D numerical geomechanical modelling with an elasto-plastic material law to explore the impact of such site specific features on the stress field in a sedimentary sequence of the Swiss Alpine foreland. The model's dimensions are 14 km × 14 km × 3 km and it con

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Hergert, T., O. Heidbach, K. Reiter, S. B. Giger, and P. Marschall. "Stress field sensitivity analysis in a sedimentary sequence of the Alpine foreland, northern Switzerland." Solid Earth 6, no. 2 (2015): 533–52. http://dx.doi.org/10.5194/se-6-533-2015.

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Abstract. The stress field at depth is a relevant parameter for the design of subsurface constructions and reservoir management. Yet the distortion of the regional stress field due to local-scale features such as sedimentary and tectonic structures or topography is often poorly constrained. We conduct a stress sensitivity analysis using 3-D numerical geomechanical modelling with an elasto-plastic material law to explore the impact of such site-specific features on the stress field in a sedimentary sequence of the Swiss Alpine foreland. The model's dimensions are 14 × 14 × 3 km3 and it contains

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KOLODIYCHUK, A.V. "Processes of introduction of digital technologies and lithosphere: mutual influence and threats of interaction." Market Relations Development in Ukraine №1(212)2019 165 (March 1, 2019): 110–15. https://doi.org/10.5281/zenodo.2581209.

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The subject of the study is the processes of implementation of information and communication technologies (ICTs), the lithosphere and the nature of the interaction between them. The purpose of the study is to study the relationship and risks of the interaction of the implementation processes of digital technologies and the lithosphere – solid shell of the earth's surface. Research methods. The work uses the dialectical method of scientific knowledge, the method of analysis and synthesis, the comparative method, the method of data generalization. Results of work. The article describes

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Barannikov, Aleksandr Grigor’evich. "Spatial and genetic relationship of endogenous and exogenous gold content in the area of the Pervomaisko-Zverevsky ore cluster (Middle Urals)." NEWS of the Ural State Mining University, no. 3 (September 15, 2023): 40–54. http://dx.doi.org/10.21440/2307-2091-2023-3-40-54.

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Te relevance of the work is due to the need to improve the efciency of appraisal work on new and unconventional types of gold mineralization within the known ore-placer regions and clusters. Te purpose of the work is to show the results of the study of the spatial and genetic relationship between endogenous and exogenous gold content using the example of the Pervomaisk-Zverevsky ore-placer cluster (OPC). Research methodology. Mineralogical and geochemical sampling of ore bodies outcrops, chemical weathering crusts; schlicho-mineralogical studies; study of native gold on a digital basis, taking

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Salah, Hamad. "Morphometric Analysis of the southern Al Jabal Al Akhdar Watersheds NE Libya." International Journal of Advances in Scientific Research and Engineering (ijasre) 5, no. 7 (2019): 24–36. https://doi.org/10.31695/IJASRE.2019.33296.

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<em>The study aimed to quantify the morphometric characteristics of 11 watersheds in south Al Jabal Al Akhdar area (Green Mountain)  located on northeast Libya. Where Digital Elevation Model (DEM) data of 1 arcsec resolution for the study area downloaded from USGS Earth Explorer and processed to extract the watershed attributes using ArcGIS software. In addition, the linear, areal, and relief aspects parameters and indices were computed. The stream number for the watersheds varies from first orders to seventh orders, where a large number of streams was found in the first, second, and thir

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Puchkov, V. N. "Relationship between plume and plate tectonics." Geotectonics 50, no. 4 (2016): 425–38. http://dx.doi.org/10.1134/s0016852116040075.

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Frangen, Tihomir, Mirja Pavić, Vlatko Gulam, and Tomislav Kurečić. "Use of a LiDAR-derived landslide inventory map in assessing Influencing factors for landslide susceptibility of geological units in the Petrinja area (Croatia)." Geologia Croatica 75, no. 1 (2022): 35–49. http://dx.doi.org/10.4154/gc.2022.10.

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A landslide inventory was created for an area of 22.6 km2 near Petrinja city in northern Croatia, based on the high-resolution LiDAR data complemented by orthophoto maps. A total of 216 landslides were identified, covering 2.91 % of that area. Landslide polygons were overlain on geological units based on the Basic map of SFRY at a scale of 1:100,000 that is the largest scale geological map available for the whole of Croatia. The relationship between landslides and geological units was expressed as a landslide index. Three geological units displayed increased landslide susceptibility. A Pliocen

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Denisova, A. P., E. A. Eremenko, E. A. Moroz, et al. "Pockmarks morphology at the Barents sea shelf and its determining factors." Lomonosov Geography Journal 80, no. 2, 2025 (2025): 99–115. https://doi.org/10.55959/msu0579-9414.5.80.2.8.

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Based on the results of complex geological and geophysical works carried out during the 38th, 52nd and 56th cruises of the R/V “Akademik Nikolaj Strakhov” and the 51st cruise of the R/V “Akademik Boris Petrov”, the fluidogenic relief was studied in detail at five key polygons in the southern and northeastern parts of the Barents Sea shelf. Digital elevation models of sea bottom obtained as a result of multibeam bathymetric survey allowed identifying of 2218 pockmarks. Their diameter varies from the first dozens of meters to 250 m, and the depth from 0,2 to 7,8 m. The morphometric analysis of t

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Yang, Yi, Jie Zhang, Junjie Wu, et al. "Determination of Cenozoic Sedimentary Structures Using Integrated Geophysical Surveys: A Case Study in the Hebei Plain, China." Sensors 25, no. 2 (2025): 486. https://doi.org/10.3390/s25020486.

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The strong multi-stage tectonic movement caused the northwest of the North China Plain to rise and the southeast to fall. The covering layer in the plain area was several kilometers thick. In addition to expensive drilling, it is difficult to obtain deep geological information through traditional geological exploration. In this study, gravity, magnetotelluric (MT) sounding and shallow seismic methods are used to explore the basement relief and stratigraphic structure of the alluvial proluvial area in front of Taihang Mount in the North China Plain so as to understand the geological structure a

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AMROUNI-BOUAZIZ, Oula, Radhia SOUISSI, J.Paul BARUSSEAU, Sâadi ABDELJAOUED, Henri PAUC, and Raphaël CERTAIN. "Grain-size and morphodynamical state of the bay-of-Mahdia shoreface (Tunisia). Contribution to the assessment of coastal sensitivity." Geo-Eco-Marina No 13/2007 (December 31, 2007): 5–19. https://doi.org/10.5281/zenodo.57333.

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Abstract. Improving our knowledge about coastlines worldwide can definitely contribute to understanding how sand coastlines with offshore bar systems operate. The study undertaken on the coastal sedimentary unit on the Bay of Mahdia where moderately active tectonic activity prevails fits into that general approach. This preliminary work presents the morphology and sedimentology of a 15 km long coastline with a sandy beach and an irregular dune ridge bordering the offshore between cape Africa and cape Dimas along the Bay of Mahdia. Morphology displays a sandy sedimentary prism composed of 3 com

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Costa, Danilo Mosca da, and Edson Roberto Souza. "Conceptions of mountain formation, foulding, fault and the continental drift in geography textbooks between the decades of 1930 to 1960." Terrae Didatica 14, no. 4 (2018): 349–54. http://dx.doi.org/10.20396/td.v14i4.8654094.

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The conceptions about the origins of mountains, faults, folds or relief are very different if we compare didactic books of Geog-raphy published before and after the elaboration of Plates Tectonics theory. In this article, it was analyzed didactic books from first grade education, which is currently equivalent to the 6th grade of Elementary School 2, published between 1933 until 1961. Obviously, within this article, Plate tectonics theory had not yet been elaborated. However, the academic world was already fa-miliar with the Continental Drift theory, an innovative proposal elaborated at the beg

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Tusikova, S. A., and T. V. Merkulova. "SEISMIC LINEAMENTS OF THE PRIAMURYE REGION AND THEIR RELATIONSHIP WITH FAULT TECTONICS." Tikhookeanskaya Geologiya 44, no. 4 (2025): 40–48. https://doi.org/10.30911/0207-4028-2025-44-4-40-48.

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Based on seismic energy, earthquake density and Morishita index data, a map of Priamurye seismic lineaments that can serve as rupture indicators has been constructed. The identified seismic lineaments have been compared with the known faults identified based on geological data and indirect signs of hidden faults – linear magnetic and gravity anomalies, Vp/Vs velocity ratios and lineaments identified through relief analysis. Of the 33 constructed seismic lineaments, 23 (13 regional and 10 local ruptures) are consistent in individual segments with known geological faults and 10 do not correlate

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ΛΥΚΟΥΔΗ, Ε. "Geomorphic evolution of the upper reaches of the drainage basin of Acheloos river." Bulletin of the Geological Society of Greece 34, no. 1 (2001): 397. http://dx.doi.org/10.12681/bgsg.17333.

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The scope of this study work is to give an insight into the dynamic processes which shape the relief in the drainage basin of the upper reaches the Acheloos river, so that the geomorphological and geodynamical evolution of the region in the past can be approached, together with a possible prediction. For this reason, the relationships between the relief and the endogenic and exogenic factors are sought. The investigated area is made up of geological formations that belong to the zones: "Ionian" (inner Ionian zone), "Gavrovo", "Pindos" and "Hyperpindos". There are also younger rocks (postalpine

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Verstappen, Herman Th. "Indonesian Landforms and Plate Tectonics." Indonesian Journal on Geoscience 5, no. 3 (2010): 197–207. http://dx.doi.org/10.17014/ijog.5.3.197-207.

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DOI: 10.17014/ijog.v5i3.103The horizontal configuration and vertical dimension of the landforms occurring in the tectonically unstable parts of Indonesia were resulted in the first place from plate tectonics. Most of them date from the Quaternary and endogenous forces are ongoing. Three major plates – the northward moving Indo-Australian Plate, the south-eastward moving SE-Asian Plate and the westward moving Pacific Plate - meet at a plate triple-junction situated in the south of New Guinea’s Bird’s Head. The narrow North-Moluccan plate is interposed between the Asia and Pacific. It tapers out

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Naumko, Іhor, N. V. Batsevych, Yu I. Fedoryshyn, Myroslav Pavlyuk, Yu S. Myshchyshyn, and I. V. Repyn. "GEODYNAMICS." GEODYNAMICS 1(30)2021, no. 1(30) (2021): 36–47. http://dx.doi.org/10.23939/jgd2021.01.036.

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Purpose. The main purpose of this paper is to investigate the peculiarities of the spatial distribution of thickness and paleorelief of continental flood basalts of Luchychi stratum of Ratne suite of the Ediacaran of the Ratne–Kamin-Kashyrskyi Area in Western Volyn using maps of the thickness and relief of the paleosurface. The study also focuses on correlation between the specified parameters of the stratum and the spatial change of concentrations of native mineralization and its localization relative to the roof (sole) of the stratum. Method. The research applies a number of methods, includi

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Kozyrev, Anatoly, Andrian Batugin, Jianping Zuo, and Svetlana Zhukova. "The Impact of Surface Water Seepage on Seismicity and Rockbursting in Mines." Sustainability 14, no. 22 (2022): 15414. http://dx.doi.org/10.3390/su142215414.

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Retrospective analysis of data obtained from long-term monitoring of technogenic seismicity and rockbursts at the Apatitovy Tsirk and the Rasvumchorr Plateau deposits (Russia) showed that there is a significant (by 50% or more) increase in the number of geodynamic events during spring snowmelt periods. An upswing of seismic activity within this rock massif occurs when following conditions are true: water reserve in the snow cover on the deposit area is more than 3 × 108 m3; snowmelt period exceeds 40 days; increase in water ingress rates continues for over 5 days and total water inflow volume

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ЕСИН, Е. И., А. Н. ВАСИЛЕВСКИЙ, and Н. А. БУШЕНКОВА. "SPATIAL CORRELATIONS BETWEEN THE TERRAIN FEATURES, GRAVITATIONAL FIELD AND SEISMIC VELOCITY ANOMALIES IN THE CENTRAL KAMCHATKA REGION." Геология и геофизика 65, no. 2 (2024): 303–18. http://dx.doi.org/10.15372/gig2023165.

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Различные подходы к тектоническому районированию и разные типы (комплексы) используемых данных, на базе которых районирование производится, являют множественность прежде полученных различными авторами тектонических схем Камчатки и Камчатского региона. В данной работе для изучения пространственных связей тектонических проявлений геологических процессов использовался совместный анализ аномалий гравитационного поля, трансформант гравитационного поля и рельефа, магнитного поля и современных сейсмотомографических моделей аномалий скоростей. В результате проведенного исследования была построена тект

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Graveleau, F., J. E. Hurtrez, S. Dominguez, and J. Malavieille. "A new experimental material for modeling relief dynamics and interactions between tectonics and surface processes." Tectonophysics 513, no. 1-4 (2011): 68–87. http://dx.doi.org/10.1016/j.tecto.2011.09.029.

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Novak, Taras. "General characteristics of geomorphological structure of Mizots’ka Upland." Visnyk of the Lviv University. Series Geography, no. 42 (October 15, 2013): 265–73. http://dx.doi.org/10.30970/vgg.2013.42.1872.

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Geomorphologic structure of Mizots’ka Upland and it place in a classification of landforms were described in the article. Description of the differences in geomorphologic structure between certain parts of the upland was provided. The impact of geology and tectonics on landforms of Mizots’ka Upland was analyzed and a hypothesis about the role of neotectonic movements in the development of its relief was put forward. Keywords: Mizots’ka Upland, plateau, geologic structure, horizontal division, vertical division, neotectonic movements.

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Kusnida, Dida, Ali Albab, Tumpal B. Nainggolan, and Yulinar Firdaus. "The Occurrence of Recent-Subrecent Seabed Acoustic Anomalies and Its Relationship with Structural Uplift around the Waipoga Trough, West Papua-Indonesia." Indonesian Journal on Geoscience 10, no. 1 (2023): 109–17. http://dx.doi.org/10.17014/ijog.10.1.109-117.

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Marine Geological Institute acquired high-resolution seismic and acoustic data during a survey in the Waipoga Trough-West Papua in 2018. The profiles show acoustically blanking, turbid, and cloudy occur along the trough floor over 3,000 km2. Many accoustic chimneys are breaking through the seabed of recent and subrecent sediment layers. It is suggested due to the local expulsion of methane gas. The pockmarks occur as transparent and turbid acoustic characteristics. They locally have relief down to 2-10 m below the seafloor with horizontal dimensions up to 25 -100 m in width. Methane formation

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Radoš, Denis, Sanja Lozić, and Ante Šiljeg. "Morfometrijske značajke šireg područja Duvanjskog polja, Bosna i Hercegovina." Geoadria 2, no. 1 (1997): 177. http://dx.doi.org/10.15291/geoadria.248.

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The objects of this study are the hillslopes in the broader area of Duvanjsko polje (Bosnia and Herzegovina). Slopes can be defined as relief surfaces determined by geographical position, slope inclination (related with horizontal surface), aspect, and degree of curvature (profile and planar).Recent slope shapes can be defined as results of series of natural and anthropogenic factors during relief genesis and evolution. It is possible to correlate slope characteristics with geological structure and other natural geographic features (climate, soils, vegetation etc.) using geomorphometrical anal

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Radoš, Denis, Sanja Lozić, and Ante Šiljeg. "Morfometrijske značajke šireg područja Duvanjskog polja, Bosna i Hercegovina." Geoadria 17, no. 2 (2012): 177. http://dx.doi.org/10.15291/geoadria.352.

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The objects of this study are the hillslopes in the broader area of Duvanjsko polje (Bosnia and Herzegovina). Slopes can be defined as relief surfaces determined by geographical position, slope inclination (related with horizontal surface), aspect, and degree of curvature (profile and planar).Recent slope shapes can be defined as results of series of natural and anthropogenic factors during relief genesis and evolution. It is possible to correlate slope characteristics with geological structure and other natural geographic features (climate, soils, vegetation etc.) using geomorphometrical anal

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