2012
DOI: 10.1016/j.quaint.2012.06.033
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Geomorphology and Late Holocene morphogenesis of Tchinguiz Tepe hill (Old Termez, Uzbekistan, Central Asia)

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Cited by 9 publications
(10 citation statements)
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“…Although a deeper geological study is needed to identify the source(s) of the raw materials procured by ancient potters, the petrographic data is in agreement with the geological environment (Sánchez del Corral and Thum ). Kampyr Tepe is located on the south‐western limit of the Surkhan Darya valley.…”
Section: Pottery Analysismentioning
confidence: 84%
“…Although a deeper geological study is needed to identify the source(s) of the raw materials procured by ancient potters, the petrographic data is in agreement with the geological environment (Sánchez del Corral and Thum ). Kampyr Tepe is located on the south‐western limit of the Surkhan Darya valley.…”
Section: Pottery Analysismentioning
confidence: 84%
“…The floodplain on which ancient Termez was located has an almost flat topography (mean altitude 300 m), although its physiography includes some hills that provide evidence of the area's geology (Figure ). The geomorphological units identified are organized as follows (Sánchez Del Corral & Thum, ): The recent fluvial domain of Amu Darya‐Surkhan Darya, which divides into two surfaces: S1 (altitude ~307 m) and S2 (between 300 and 292 m). S1 comprises the remains of the northern sector together with Kara Tepe, Tchingiz Tepe, and part of Rabat.…”
Section: Natural Landscape and Geological Backgroundmentioning
confidence: 99%
“…The depression comprises a Hercynian basement, with Precambrian‐Paleozoic high‐grade metamorphic rocks cropping out mostly along the orogenic margins, and Permian‐Triassic sedimentary and volcanic rocks to the north, east and south (e.g., Bourgeois, Cobbold, Rouby, & Thomas, ; Leith & Alvarez, ; Nikolaev, ; Yachminnikov & Nikolaev, ). The filling of the Afghan‐Tajik Depression includes mainly Mesozoic and Cenozoic sediments that have undergone several deformation episodes as a consequence of the indentation of the Pamir into the Asian continent when India and Asia collided (see Figure in Sánchez Del Corral & Thum, ). The Mesozoic‐Cenozoic sedimentary cover comprises a lower (Pre‐Molasse) assemblage deposited between the Jurassic and Eocene‐Oligocene, and an upper (Molasse) assemblage belonging to the Miocene and Pliocene (Nikolaev, ; Sánchez Del Corral & Thum, ; Yachminnikov & Nikolaev, ).…”
Section: Natural Landscape and Geological Backgroundmentioning
confidence: 99%
“…These sediments, together with the successions of clayey, silty and sandy layers, constitute the stratigraphic sequence of this mound. Along with the northern and southern hills, they correspond to the southernmost Cenozoic outcrops of the Surkhan Darya depression where Termez is located (Sánchez del Corral and Thum , 90–1, fig. ).…”
Section: Geological Background and Raw Claysmentioning
confidence: 99%
“…The Cretaceous and Palaeocene outcrops are composed of clays, gypsum, sandstones, anhydrite, dolomite and marls (suprasalt sediments), while the Eocene and Oligocene sediments are formed by clays, sandstone, limestone and marls. The Miocene deposits from the Molasse correspond to clays, gypsum, sandstones, siltstones and conglomerates, while conglomerates, sandstones, siltstones and clays from the Pliocene lie discordantly over these materials (Sánchez del Corral and Thum , 91).…”
Section: Geological Background and Raw Claysmentioning
confidence: 99%