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Artykuły w czasopismach na temat „Morphotectonics”

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Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 30 lipca 2024

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1

Novak, Taras, i Andriy Bermes. "Morphotectonics of Myzotska Upland". Visnyk of the Lviv University. Series Geography, nr 47 (27.11.2014): 194–201. http://dx.doi.org/10.30970/vgg.2014.47.955.

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The aim of this work is the interpretation results of morphotectonic analysis of Myzotska Upland for investigation its neotectonic history and identifying regional morphotectonic differences. We used planed surface reconstruction method and stream gradient index (SL index). We recognized that Myzotska Upland consist of several blocks with differentiated neotectonic movements. Northwest and western ledges of upland have tectonic origin but northeast, northern and southern ledges have erosional origin. Northern and eastern parts have tectonic structure that more similar to Rivnenska Upland than to other territories of Myzotska Upland. Parts of Myzotska Upland have similar geomorphological structure but different tectonic history. Key words: morphotectonics, neotectonic movements, stream gradient index (SL index), faults, planed surfaces, Volynska Upland, Myzotska Upland.

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2

Jayko, Angela S. "Morphotectonics". Eos, Transactions American Geophysical Union 85, nr 44 (2004): 456. http://dx.doi.org/10.1029/2004eo440007.

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3

Bermes, Andrii. "Morphotectonics of Kremenets Mountains". Visnyk of the Lviv University. Series Geography, nr 50 (28.12.2016): 34–44. http://dx.doi.org/10.30970/vgg.2016.50.8675.

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The aim of this work is the analysis and interpretation of the results of morphotectonic analysis of the territory of the Kremenets Mountains in order to study its neotectonic history and to identify the regional morphotectonic differences. The methods of the reconstruction of the post-Sarmatic planation surface and lineament analysis were used for this analysis as well as the data received in the process of field studies on the territory where the exploration took place, in particular the study of rocks fracturing. A number of previous studies of the upland area was analysed, in particular, its tectonics and relief. It is discovered that the Kremenets Mountains are the mountains of the monolithic structure, which are under the influence of the differentiated neotectonic movements; a number of faults, that affect the relief situation in the natural area, is also discovered. The theory of the coincidence of the directions of drains valleys with the rocks fracturing is confirmed. The theories of the formation of the North-Podillia ledge, of its confirmation and denial are considered. The origin of the north-west ledge of the escarpment is tectonic and the origin of the south and east ledges is erosive. The relief-forming role of tectonic structure of the region and its expression in the modern morphodynamic processes is evaluated. Key words: the Kremenets Mountains, the Podillia Upland, morphotectonics, neotectonic movements, faults, North-Podillia ledge, planation surfaces, lineament analysis.

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4

Gavrilov, A. A. "GEOLOGICAL AND GEOMORPHOLOGICAL RESEARCH METHODOLOGY FOR METALLOGENIC PURPOSES". Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences, nr 3(51) (2021): 84–95. http://dx.doi.org/10.31431/1816-5524-2022-3-51-84-95.

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The basic questions of the methodology of geological and geomorphological study (ore geomorphology, morphostructural analysis, morphotectonics, neotectonics) of ore-bearing territories are considered. The concepts of "geomorphologic systems organization element" as the smallest particle of matter preserving the structure and properties of a mineral, as well as "objectives", "objects" and "subjects" of morphostructural and morphotectonic studies for solving problems of metallogeny have been formulated. In areas with complex geological structure, it is recommended to carry out complex of morphostructural and morphotectonic works with repeated solution of direct and inverse problems: relief and geological environment, geological environment relief. This will make it possible to establish the totality of available deterministic and chronological relations between landforms and structural elements of the lithosphere. Along with the solution of traditional problems of ore geomorphology, it is proposed to use the developed original complex of morphostructural and morphotectonic studies.

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5

Gavrilov, A. A. "GEOLOGICAL AND GEOMORPHOLOGICAL RESEARCH METHODOLOGY FOR METALLOGENIC PURPOSES". Bulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences, nr 3(51) (2021): 84–95. http://dx.doi.org/10.31431/1816-5524-2022-3-51-84-95.

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The basic questions of the methodology of geological and geomorphological study (ore geomorphology, morphostructural analysis, morphotectonics, neotectonics) of ore-bearing territories are considered. The concepts of "geomorphologic systems organization element" as the smallest particle of matter preserving the structure and properties of a mineral, as well as "objectives", "objects" and "subjects" of morphostructural and morphotectonic studies for solving problems of metallogeny have been formulated. In areas with complex geological structure, it is recommended to carry out complex of morphostructural and morphotectonic works with repeated solution of direct and inverse problems: relief and geological environment, geological environment relief. This will make it possible to establish the totality of available deterministic and chronological relations between landforms and structural elements of the lithosphere. Along with the solution of traditional problems of ore geomorphology, it is proposed to use the developed original complex of morphostructural and morphotectonic studies.

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6

Singh, Archana, Bijoylakshmi Gogoi, Devojit Bezbaruah i Neelratan Singh. "Assessment of active tectonics in the Siwalik basin around the Subansiri river, NE India". IOP Conference Series: Earth and Environmental Science 1032, nr 1 (1.06.2022): 012043. http://dx.doi.org/10.1088/1755-1315/1032/1/012043.

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Abstract In this paper we evaluate the morphotectonics of the area around the Subansiri river in north-eastern India. Research focuses on understanding the impacts on areas experiencing active tectonic deformation. It also explains the variety of kinematics observed in the area from the Miocene to the present. The tectonics can explain some structures related to the extensional tectonics predominant in the region and the development of the minor and major morph structures driven by faults with different kinematics. We developed a morphotectonic evolutionary model for the area based on the morphotectonic analysis and geological mapping. Morphotectonic indices used to evaluate the tectonic activeness in this study are Mountain Front sinuosity Index, Valley Floor Width to Valley Height Ratio, Asymmetry Factor, Transverse Topographic Symmetry Factor, Mountain Front Steepness Index, Basin Shape Index and Stream Length Gradient Index. There are numerous lineaments present in the study area which are trending in NW-SE and NE-SW direction.

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7

Novikov, I. S. "MORPHOTECTONICS OF ALTAI". Geomorphology RAS, nr 3 (13.08.2015): 10. http://dx.doi.org/10.15356/0435-4281-2003-3-10-25.

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8

Migon, Piotr. "Book Review: Morphotectonics". Progress in Physical Geography: Earth and Environment 30, nr 1 (styczeń 2006): 138–40. http://dx.doi.org/10.1177/030913330603000113.

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9

Lopatin, D. V. "MORPHOTECTONICS OF NORTHEAST EURASIA". Geomorphology RAS, nr 2 (10.08.2015): 3. http://dx.doi.org/10.15356/0435-4281-2003-2-3-9.

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10

Nikonov, A. A. "MONOGRAPH ON MORPHOTECTONICS OF ALTAI". Geomorphology RAS, nr 1 (2.07.2015): 103. http://dx.doi.org/10.15356/0435-4281-2006-1-103-104.

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11

Cotilla Rodr�guez, M. O., i D. C�rdoba Barba. "Morphotectonics of the Iberian Peninsula". Pure and Applied Geophysics 161, nr 4 (1.03.2004): 755–815. http://dx.doi.org/10.1007/s00024-003-2473-2.

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12

Ufimtsev, G. F., S. N. Alekseenko i F. S. Onukhov. "Morphotectonics of the Lower Amur region". Russian Journal of Pacific Geology 3, nr 6 (grudzień 2009): 585–95. http://dx.doi.org/10.1134/s1819714009060062.

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13

Mukherjee, Sucheta, i V. C. Jha. "Morphotectonics and resultant features in Kaliani River Basin (Assam)". Sociedade & Natureza 23, nr 2 (sierpień 2011): 285–94. http://dx.doi.org/10.1590/s1982-45132011000200011.

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The surficial structure and impressions upon the crust due to endogenetic and exogenetic mechanisms are witnessed all around us. These landforms have evolved as a result of plate movements, subsidence, upliftment and various erosional processes. This concept can be collectively referred to as morphotectonics of any region and can be used as a key to understand its genesis as well as present physical state. Morphotectonics refers to forms and shapes that have evolved in the past or in recent times as a result of past or recent tectonic activity. The most vivid evidences of past tectonic activity can be assessed through drainage lines, in any area which are guided and controlled by physical structures over which they flow.

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14

Twidale, C. R. "Edwin Hills: morphotectonics and other geomorphological contributions". Proceedings of the Geologists' Association 111, nr 1 (styczeń 2000): 71–82. http://dx.doi.org/10.1016/s0016-7878(00)80037-1.

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15

Ufimtsev, G. F. "Morphotectonics of the Mongolia-Siberian mountain belt". Journal of Geodynamics 11, nr 4 (marzec 1990): 309–25. http://dx.doi.org/10.1016/0264-3707(90)90014-l.

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16

Ufimtsev, G. F. "Great Scarps Above Sea Coasts in Global Morphotectonics". Earth Science Frontiers 16, nr 1 (styczeń 2009): 226–33. http://dx.doi.org/10.1016/s1872-5791(08)60072-x.

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17

Urbano, Tullio, Tommaso Piacentini i Marcello Buccolini. "Morphotectonics of the Pescara River basin (Central Italy)". Journal of Maps 13, nr 2 (12.06.2017): 511–20. http://dx.doi.org/10.1080/17445647.2017.1338204.

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18

Suo, Y. H., S. Z. Li, S. Yu, Z. Zhang, X. Y. Li i L. L. Guo. "Morphotectonics and ridge jumpings in the Indian Ocean". Geological Journal 51 (27.11.2015): 624–33. http://dx.doi.org/10.1002/gj.2746.

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19

Shvarev, S. V. "Morphotectonics, Seismicity, and Exogenous Processes of the Kola Peninsula". Russian Geology and Geophysics 63, nr 8 (1.08.2022): 940–54. http://dx.doi.org/10.2113/rgg20204310.

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Abstract —The purpose of this study is to determine a morphologically pronounced fault–block structure identified with the neotectonic stage and compare it with sites with manifested exogenous processes, as well as modern and historical paleoseismicity in order to establish faults activated in the postglacial time. Based on the analysis of space images (Landsat-ETM+) and a digital elevation model (GTOPO-30), the territory of the Kola Peninsula and the adjacent part of North Karelia is subjected to morphostructural interpretation with identifying morpholineaments and an elementary block structure. It is shown by the analyzing the directions and extent of elementary, single (simple), and complex (echeloned, parallel conjugated, and imbricated) linear structures and their zones that both linear (fault) and areal (block) structures are characterized by a predominance of a single system of northwestern and northeastern differences with a clear dominance of the former and unimodal distribution of the extent of faults and the area of blocks, depending on their number. This indicates a single (recent) stage in the formation of the morphotectonic appearance of the territory and no discrete hierarchy of the morphostructures. The degree of fragmentation of the territory at different depths is calculated depending on the number and extent of morpholineaments. It is determined that morpholineaments have a high degree of inheritance from Archean–Proterozoic structures (≈50%). Elementary morphotectonic blocks are grouped into composite blocks bounded by linear zones of great extent (100–600 km) having individual physiognomic features determined by fault patterns, which indicates the nature of the neotectonic dynamics and the degree of inheritance or reformation of the structural plan. The localization of manifestations of exogenous processes, epicenters of paleo-, historical, and modern earthquakes is determined on the basis of the analysis of topographic maps scaled at 1:100,000, catalogs of historical and paleoearthquakes, and the consolidated literature (including the data obtained by the authors of this study) on paleoseismic deformations. A geoinformation base is compiled, which is used to simulate the spatial distribution of endo- and exogenous signs of tectonic activity and compare it with the neotectonic fault–block structure. The spatial similarity of endogenous and exogenous activation zones and their confinement to faults, defined as activated in the postglacial time, are revealed. It is revealed that the following elements are most active in the postglacial–Holocene. First, flank elements on the Kola Peninsula along the Barents Sea coast, the Kandalaksha Bay shores, and the Gorlo Strait of the White Sea. Second, the central (nodal) part with the Khibiny and Lovozero massifs. Third, submeridional (transverse) secant structures separating the eastern part of the peninsula from the western part (Khibiny–Kola and Khibiny–Niva). The spatial parameters of the activated zones indicate a range of earthquake magnitudes M ≈ 6.5–7.5 generated by these structures both in the postglacial period and in the Neopleistocene as a whole.

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20

Tzankov, Tzanko, i Svetla Stankova. "New ideas about the Balkan peninsula East Part morphotectonics". Acta Scientifica Naturalis 7, nr 2 (1.07.2020): 133–44. http://dx.doi.org/10.2478/asn-2020-0025.

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AbstractThe article introduces the results of the author’s new investigations about the origin, Quaternary morphotectonic evolution and the modern morphostructure of the Bulgarian Continental Microplate in the eastern part of Balkan Peninsula. The research was realized on a base of the contemporary Plate tectonic study principia by means of the morphostructural analysis apply. It was provided the principal relief building role of the regional mosaic pattern and the listric faulting in the Balkan Peninsula East Part.

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21

Květ, Radan. "Valleys and river benches from the viewpoint of morphotectonics". GeoJournal 30, nr 4 (sierpień 1993): 403–8. http://dx.doi.org/10.1007/bf00807221.

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22

Foster, David A., i Andrew J. W. Gleadow. "Fission-track morphotectonics of crustal extension in Central Kenya". Nuclear Tracks and Radiation Measurements 21, nr 4 (październik 1993): 620. http://dx.doi.org/10.1016/1359-0189(93)90273-c.

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23

Tsimi, Ch, A. Ganas, N. Soulakellis, O. Kairis i S. Valmis. "MORPHOTECTONICS OF THE PSATHOPYRGOS ACTIVE FAULT, WESTERN CORINTH RIFT, CENTRAL GREECE". Bulletin of the Geological Society of Greece 40, nr 1 (8.06.2018): 500. http://dx.doi.org/10.12681/bgsg.16657.

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The study area is located on the western part of the Gulf of Corinth which is considered as a paradigm of an active rift system in Greece. This rift was formed by normal slip on big faults which extend the crust of the Earth in the N-S direction. The morphotectonic indices (hypsometric curve, hypsometric integral, drainage basin asymmetry, ratio of valley floor width to valley height) have been estimated using the 20-m digital elevation model of this area and the ARC software. The normal faults of the study area have been extracted by use of a DEM mosaic of 20-m pixel size, satellite images from Landsat 7 ETM+ and SRTM 90m. Our results highlight the recent activity of the Psathopyrgos normal fault on the basis of a series of morphotectonic evidence and suggest the existence of a single fault segment for a distance of 16 km.

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24

Shchetnikov, Alexander. "MORPHOTECTONICS OF THE SOUTH-WESTERN CIS-BAIKAL AND CIS-HOVSGOL". Proceedings of the Siberian Department of the Section of Earth Sciences, Russian Academy of Natural Sciences. Geology, Prospecting and Exploration of Ore Deposits, nr 3 (wrzesień 2016): 134–43. http://dx.doi.org/10.21285/0130-108x-2016-56-3-134-143.

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25

Erol, Oğuz, i A. Ünal Akman. "Morphotectonics and seismicity in the east of Marmara region, Turkey". Zeitschrift für Geomorphologie 52, nr 1 (1.03.2008): 65–83. http://dx.doi.org/10.1127/0372-8854/2008/0052-0065.

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26

Reicherter, Klaus, Nadine Hoffmann, Katja Lindhorst, Sebastian Krastel, Tomás Fernández-Steeger, Christoph Grützner i Thomas Wiatr. "Active basins and neotectonics: morphotectonics of the Lake Ohrid Basin (FYROM and Albania)". Zeitschrift der Deutschen Gesellschaft für Geowissenschaften 162, nr 2 (1.06.2011): 217–34. http://dx.doi.org/10.1127/1860-1804/2011/0162-0217.

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27

Chandrakant, Gurav, Md Babar i Anilraj Jagdale. "Morphotectonics Study of Dhamani River Basin in Kolhapur District, Maharashtra, India". Bulletin of Pure & Applied Sciences- Geology 39f, nr 2 (2020): 131–49. http://dx.doi.org/10.5958/2320-3234.2020.00013.x.

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28

Taesiri, V., M. Pourkermani, A. Sorbi, M. Almasian i M. Arian. "Morphotectonics of Alborz Province (Iran): A Case Study Using GIS Method". Geotectonics 54, nr 5 (wrzesień 2020): 691–704. http://dx.doi.org/10.1134/s001685212005009x.

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29

Shchetnikov, A. A. "Morphotectonics of lacustrine basins: The Baikal rift zone as an example". Russian Journal of Pacific Geology 1, nr 2 (kwiecień 2007): 120–29. http://dx.doi.org/10.1134/s1819714007020029.

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30

Kukowski, Nina, Thies Schillhorn, Katrin Huhn, Ulrich von Rad, Stephan Husen i Ernst R. Flueh. "Morphotectonics and mechanics of the central Makran accretionary wedge off Pakistan". Marine Geology 173, nr 1-4 (marzec 2001): 1–19. http://dx.doi.org/10.1016/s0025-3227(00)00167-5.

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31

Hsiung, Kan-Hsi, Ho-Shing Yu i Cheng-Shing Chiang. "The modern Kaoping transient fan offshore SW Taiwan: Morphotectonics and development". Geomorphology 300 (styczeń 2018): 151–63. http://dx.doi.org/10.1016/j.geomorph.2017.10.013.

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32

Gasperini, Luca, Alfredo Marzocchi, Stefano Mazza, Roberto Miele, Matteo Meli, Hassan Najjar, Alessandro M. Michetti i Alina Polonia. "Morphotectonics and late Quaternary seismic stratigraphy of Lake Garda (Northern Italy)". Geomorphology 371 (grudzień 2020): 107427. http://dx.doi.org/10.1016/j.geomorph.2020.107427.

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33

Gioia, Dario, Marcello Schiattarella, Massimo Mattei i Giovanni Nico. "Quantitative morphotectonics of the Pliocene to Quaternary Auletta basin, southern Italy". Geomorphology 134, nr 3-4 (listopad 2011): 326–43. http://dx.doi.org/10.1016/j.geomorph.2011.07.009.

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34

Miccadei, E., C. Berti, M. Calista, G. Esposito, V. Mancinelli i T. Piacentini. "Morphotectonics of the Tasso Stream - Sagittario River valley (Central Apennines, Italy)". Journal of Maps 15, nr 2 (19.03.2019): 257–68. http://dx.doi.org/10.1080/17445647.2019.1589588.

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35

Thannoun, Rayan Gh, Salim A. Fanoosh i Hadeer Gh M. Adeeb. "Integration of satellite data processing with seismic sections for tectonic interpretation and modeling for the breaks and omissions of continuous stratigraphic units". International Review of Applied Sciences and Engineering 12, nr 1 (20.03.2021): 34–43. http://dx.doi.org/10.1556/1848.2020.00123.

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AbstractSatellite thematic maps in geological field studies are an important tool for the delineation, interpretation, representation, and visualization of geological processes, while the development of seismic sections offers an increasingly detailed analysis of subsurface geology and inferring and understanding the subsurface structure of the earth. This combination promoted a fast-growing research in the fields of morphotectonics and neotectonics. The area under investigation is one of the most significant Iraqi places which includes several oil fields. The study area is located in northern Iraq and administratively follows Kirkuk governorate. Landscapes in this area are characterized by asymmetrical, cylindrical and extended folds. Kirkuk, Bai-Hasan and Qarachuq Anticlines reflect these structural elements and their fold axis trends towards northwest-southeast within the Zagros folded zone. The main objective of this study is to use the visual and digital interpretation of Landsat image to discriminate the sudden breaks and omissions of rock beds in the study area. Therefore, a morphotectonic map was created, the accurate location of the sudden breaks was provided and the zones affected by tectonic deformation, which left its imprint on the successive lithological units were detected. Seismic data were used to assess the tectonic impact on subsurface formations and their reflections on exposure rocks. The seismic lines were selected based on the locations of the identified sudden breaks as interpreted from satellite images. The hypothesis derived from this study is that the sudden breaks in the study area were triggered by a series of faults. In addition, the region was affected by the vertical stresses resulting from these faults and morphological aspects of the region were determined by the temporal variations of the above stresses.

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36

Kimura, Kazuo. "Comparative morphotectonics in the Himalayan foreland and the forearc of Southwest Japan". Himalayan Journal of Sciences 2, nr 4 (11.02.2008): 182. http://dx.doi.org/10.3126/hjs.v2i4.865.

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37

Grando, Gianluca, i Ken McClay. "Morphotectonics domains and structural styles in the Makran accretionary prism, offshore Iran". Sedimentary Geology 196, nr 1-4 (marzec 2007): 157–79. http://dx.doi.org/10.1016/j.sedgeo.2006.05.030.

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38

Granja Bruña, J. L., U. S. ten Brink, A. Carbó-Gorosabel, A. Muñoz-Martín i M. Gómez Ballesteros. "Morphotectonics of the central Muertos thrust belt and Muertos Trough (northeastern Caribbean)". Marine Geology 263, nr 1-4 (lipiec 2009): 7–33. http://dx.doi.org/10.1016/j.margeo.2009.03.010.

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39

Arzhannikova, A. V., R. Vassallo, S. G. Arzhannikov i M. Jolivet. "Morphotectonics and paleoseismology of the eastern end of the Bolnay fault (Mongolia)". Russian Geology and Geophysics 56, nr 10 (październik 2015): 1484–90. http://dx.doi.org/10.1016/j.rgg.2015.09.010.

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40

Longkumer, Limasanen, Khayingshing Luirei, J. N. Moiya i Glenn T. Thong. "Morphotectonics and neotectonic activity of the Schuppen Belt of Mokokchung, Nagaland, India". Journal of Asian Earth Sciences 170 (luty 2019): 138–54. http://dx.doi.org/10.1016/j.jseaes.2018.11.010.

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41

Wopfner, H., i C. Z. Kaaya. "Stratigraphy and morphotectonics of Karoo deposits of the northern Selous Basin, Tanzania". Geological Magazine 128, nr 4 (lipiec 1991): 319–34. http://dx.doi.org/10.1017/s0016756800017593.

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AbstractLate Permian Karoo deposits of the northern Selous Basin in south-central Tanzania comprise conglomerates and diamictitic boulder beds of alluvial and scarp-foot fan origin. These merge with grey to greenish sandstones, siltstones and black shales of deltaic and lacustrine environments. Microflora assemblages indicate a late Permian age. Lateral changes and interfingering of various lithofacies units are common. Depositional development was controlled by syndepositional faulting and variations of gradients resulting from fault movements. The position of the fault scarp separating the basin area from the elevated basement horst to the west roughly corresponded with the present boundary between the Selous Basin and the Precambrian metamorphics of the Uluguru Mountains.The late Permian Karoo succession of this part of the Selous Basin apparently overlaps older Karoo deposits contained in the north-northeast trending narrow graben structures. It is therefore regarded as a new depositional event which was initiated by renewed tensional tectonism in late Permian time. During this tectonic episode the narrow early Karoo graben structures were expanded into much broader rift basins. Material eroded from the rift shoulders and associated highlands was literally dumped across the fault scarps, forming debris aprons and scarp-foot fans. Rivers emanating from the highlands formed large alluvial fans and, further afield, deltas issued into freshwater lakes.Some of these late Permian faults were rejuvenated by late Cretaceous to early Tertiary tectonism. Thermal waters circulating along fractures converted feldspars, biotites and hornblendes to prehnite. Further tectonic adjustments in mid Tertiary time led to the present-day morphology.

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Chiang, Cheng-Shing, i Ho-Shing Yu. "Morphotectonics and incision of the Kaoping submarine canyon, SW Taiwan orogenic wedge". Geomorphology 80, nr 3-4 (październik 2006): 199–213. http://dx.doi.org/10.1016/j.geomorph.2006.02.008.

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Pavlides, Spyros B., Nikos C. Zouros, Fang Zhongjing, Cheng Shaoping, Markos D. Tranos i Alexandros A. Chatzipetros. "Geometry, kinematics and morphotectonics of the Yanqing–Huailai active faults (northern China)". Tectonophysics 308, nr 1-2 (lipiec 1999): 99–118. http://dx.doi.org/10.1016/s0040-1951(99)00074-8.

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Arzhannikova, A. V., S. G. Arzhannikov, A. A. Chebotarev i E. Nomin-Erdene. "Morphotectonics and paleoseismology of the North Darhad fault (SW Baikal Rift, Mongolia)". Journal of Asian Earth Sciences 259 (styczeń 2024): 105882. http://dx.doi.org/10.1016/j.jseaes.2023.105882.

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Mirlin, E. G., i E. I. Сhesalova. "SOURCES OF ENDOGENOUS AND ORE MATERIAL IN WORLD OCEAN: MORPHOTECTONICS, GEODYNAMICS, SCALE". РУДЫ ОКЕАНА: ОТ ИЗУЧЕНИЯ К ОСВОЕНИЮ 51, nr 4 (29.12.2023): 13–34. http://dx.doi.org/10.29006/1564-2291.jor-2023.51(4).2.

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The basis of the work is the postulate of V. I. Smirnov that the metallogeny of the ocean is determined by basaltoid magmatism. The morphotectonics and geodynamic position of the structures of the World Ocean, the evolution of which was accompanied by the outpouring of basalt lavas to the bottom and their interaction with ocean water and ocean biota, were characterized by the analysis of multi-scale geological and geophysical date. Two categories of global morphostructures are identified as potential sources of endogenic and ore matter: the first are genetically related to the accretion of the lithosphere at the boundaries of plate separation, the second – with intraplate volcanic-tectonic processes. Comparative estimates of the scale of the substance intake for the two categories have been carried out and it is shown that they may differ slightly or be close.

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Arzhannikova, A. V., S. G. Arzhannikov, R. M. Semenov i A. V. Chipizubov. "Morphotectonics and Late Pleistocene-Holocene deformations in the Tunka system of basins (Baikal rift, Siberia)". Zeitschrift für Geomorphologie 49, nr 4 (29.12.2005): 485–94. http://dx.doi.org/10.1127/zfg/49/2005/485.

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Bashir, Bashar, i Abdullah Alsalman. "Geospatial Analysis for Tectonic Assessment and Soil Erosion Prioritization: A Case Study of Wadi Al-Lith, Red Sea Coast, Saudi Arabia". Applied Sciences 13, nr 22 (20.11.2023): 12523. http://dx.doi.org/10.3390/app132212523.

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An investigation into tectonics and erosion reveals that they play an important role in causing uplifting, valley incision, and soil erosion. The analysis of drainage basins at different scales is irreplaceable in the development of sustainable plans, particularly in arid regions. Morphotectonics and morphometric characterization analyses are very effective methods for defining the evolution of different landforms, current-day tectonic activity, and hydrological and morphological signatures of basins under investigation. The reorganization of critical drainage basins and sub-basin risk priority ranking are essential for effective and accurate sustainable plans for drainage basin management and water resources. In this study, the coupling of geospatial techniques and statistical strategies was used to examine the tectonic activity and priorities in terms of soil erosion for 15 sub-basins of Wadi Al-Lith along the Red Sea coast of Saudi Arabia. Two effective models, namely, the relative tectonic activity model and the weighted sum analysis model, were applied for examining each geomorphological and hydrological characteristic based on an analysis of the morphotectonics and morphometric parameters. Regarding the relative tectonic activity model, the 15 sub-basins were classified into three classes of tectonic activity: low, moderate, and high. Sub-basins 5, 6, 13, and 15 were considered to be in class 1 (high relative tectonic activity). On the other hand, the weighted sum analysis model assigned the sub-basins into three different ranks: low-, moderate-, and high-soil-erosion priorities. The current study’s results suggest that sub-basins 5, 6, 10, 13, and 15 were recorded within the high-soil-erosion zone and highly relative tectonic activity, covering approximately 53.52% of the total sub-basin areas. The relative tectonic activity and weighted sum analysis models proved their validity in the risk studies, which will be very useful for decision makers in various fields, including natural resources and agriculture.

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Mood, Shahram Habibi, Mohsen Jami, Javad Shahraki i Nazanin Sarhaddi. "Study on Saravan Fault Activities on the Basis of Earthquake and Morphotectonics Evidences". Open Journal of Geology 06, nr 02 (2016): 79–86. http://dx.doi.org/10.4236/ojg.2016.62008.

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Lai, Kuang-Yin, Yue-Gau Chen i Doãn Đình Lâm. "Pliocene-to-present morphotectonics of the Dien Bien Phu fault in northwest Vietnam". Geomorphology 173-174 (listopad 2012): 52–68. http://dx.doi.org/10.1016/j.geomorph.2012.05.026.

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Kempf, Jürgen. "Morphotectonics and denudation in the landform history of the Namibian Great Escarpment landscapes". Zeitschrift für Geomorphologie 54, nr 3 (1.09.2010): 347–75. http://dx.doi.org/10.1127/0372-8854/2010/0054-0035.

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