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  • 1
    Online Resource
    Online Resource
    Cham : Springer International Publishing
    Keywords: Geology ; Geology ; Archaeology ; Archaeology ; Geomorphology ; Historical geology. ; Hydrology. ; Physical geography. ; Türkei ; Geomorphologie ; Landschaftsentwicklung
    Description / Table of Contents: This book on Turkish geomorphology offers location descriptions, based on their dynamics and evolution processes, including hydrology, tectonics, volcanism, slopes, coasts, ice/snow, and wind. It presents landforms as a result of evolution (Quaternary, Holocene, historic) and in relation to the elements determining and/or impacting this evolution (vegetation, soil, hydrology, geology, climate, sea level and human action) as well as the resulting landscapes. Richly illustrated with pictures from each site, including geomorphological maps and sections, it explains the risks associated with the geomorphological dynamics (on local and global scales), natural and/or cultural heritage (archaeology, prehistory, history, architectural specifications adapted to the landscape), as well as challenges for human society (endangered landscape, protection/conservation rules/statutes, posters/paintings.)
    Type of Medium: Online Resource
    Pages: Online-Ressource (XXXI, 632 p. 489 illus., 473 illus. in color, online resource)
    Edition: Springer eBook Collection. Earth and Environmental Science
    ISBN: 9783030035150
    Series Statement: World Geomorphological Landscapes
    Language: English
    Location Call Number Limitation Availability
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  • 2
    Keywords: Earth sciences. ; Sedimentology. ; Physical geography. ; Geology. ; Geochemistry. ; Engineering geology.
    Description / Table of Contents: Cosmogenic surface exposure dating applications from Turkey: moraines, alluvial fans, fluvial terraces, lava flows and incision rates -- Tectonic Geomorphology and Paleoseismology of the Muğla-Yatağan Fault (Southwest Turkey) -- Slip rate estimation of the North Anatolian Fault using geomorphology and paleoclimate chronology: The Ganos Fault, Turkey -- Energy relief analysis of the northern Marche-Romagna region, northern Apennine, central Italy -- Evaluation of Electromagnetic Induction method to map soil salinity in semi-arid Tunisia -- Comparison of organic carbon stock of Regosols under two different climates in Tunisia -- Evolution of organic carbon stocks in a Vertisol after three years of no-tillage practice in northern Tunisia -- Spectral characteristics of soil types in northwestern Jordan: consideration of iron oxides effects and colors -- Wind-eroded sediment in southern Hungary, with special reference to the content of toxic elements -- Time-Scale Variations of organic carbon in Paddy Soils: Sanjiang Plain, China.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource(XXIX, 395 p. 259 illus., 226 illus. in color.)
    Edition: 1st ed. 2022.
    ISBN: 9783030725471
    Series Statement: Advances in Science, Technology & Innovation, IEREK Interdisciplinary Series for Sustainable Development
    Language: English
    Location Call Number Limitation Availability
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Geologische Rundschau 85 (1996), S. 669-682 
    ISSN: 0016-7835
    Keywords: Key words Turbidites ; Submarine fan ; Sequence ; stratigraphy ; Fore-arc basin ; Eocene ; Turkey
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  The Haymana basin in central Anatolia (Turkey) formed on a Late Cretaceous to Middle Eocene fore-arc accretionary wedge. A sequential model is proposed for the 1-km-thick Lutetian Yamak turbidite complex (YTC) which is the youngest paleotectonic unit of the basin. The YTC represents a prograding submarine fan subdivided into three depositional sequences (DS), each several hundred meters thick. Each depositional sequence consists of a turbidite system (TS), with sandstone and conglomeratic sandstone beds alternating with mudstones, overlain by basin plain mudstones. In each turbidite system, the sandstone and mudstone sequential organization allows the distinction of smaller subdivisions, namely, basic sequences (BS) and basic units (BU), with each basic sequence being composed of several basic units. This subdivision, associated with a two-dimensional geometric reconstruction of the YTC, leads to a better understanding of the evolution in time and space of the submarine fan system. Lower to middle fan depositional lobes, and upper fan and slope channels, are represented. As a whole, the YTC progressed from a sand-poor to a sand-rich system. Depositional sequences (DS) of the YTC may correspond to third-order sea-level cycles of tectonic origin. Accordingly, fourth- and fifth-order cycles might be proposed for the BS and BU, respectively. However, partly because of the limited extent of exposures, the allocyclic origin of these finer subdivisions remains problematic.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 85 (1996), S. 669-682 
    ISSN: 1437-3262
    Keywords: Turbidites ; Submarine fan ; Sequence stratigraphy ; Fore-arc basin ; Eocene ; Turkey
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The Haymana basin in central Anatolia (Turkey) formed on a Late Cretaceous to Middle Eocene fore-arc accretionary wedge. A sequential model is proposed for the 1-km-thick Lutetian Yamak turbidite complex (YTC) which is the youngest paleotectonic unit of the basin. The YTC represents a prograding submarine fan subdivided into three depositional sequences (DS), each several hundred meters thick. Each depositional sequence consists of a turbidite system (TS), with sandstone and conglomeratic sandstone beds alternating with mudstones, overlain by basin plain mudstones. In each turbidite system, the sandstone and mudstone sequential organization allows the distinction of smaller subdivisions, namely, basic sequences (BS) and basic units (BU), with each basic sequence being composed of several basic units. This subdivision, associated with a two-dimensional geometric reconstruction of the YTC, leads to a better understanding of the evolution in time and space of the submarine fan system. Lower to middle fan depositional lobes, and upper fan and slope channels, are represented. As a whole, the YTC progressed from a sand-poor to a sand-rich system. Depositional sequences (DS) of the YTC may correspond to third-order sea-level cycles of tectonic origin. Accordingly, fourth- and fifth-order cycles might be proposed for the BS and BU, respectively. However, partly because of the limited extent of exposures, the allocyclic origin of these finer subdivisions remains problematic.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
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