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期刊论文 [6]
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2020 [1]
2017 [3]
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river terr... [3]
turkey [2]
buried riv... [1]
central an... [1]
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quaternary... [3]
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Early Pleistocene River Terraces of the Gediz River, Turkey: The role of faulting, fracturing, volcanism and travertines in their genesis
[期刊论文]
Geomorphology, 2020-01-01, 358
Maddy D.
;
Veldkamp A.
;
Demir T.
;
Aytaç A.S.
;
Schoorl J.M.
;
Scaife R.
;
Boomer I.
;
Stemerdink C.
;
van der Schriek T.
;
Aksay S.
;
Lievens C.
View/Download:29/0
Pollen, ostracod and stable isotope records of palaeoenvironment and climate: Upper Miocene and Pliocene of the Çankırı Basin (Central Anatolia, Turkey)
[期刊论文]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2017-01-01, 467
Yavuz N.
;
Culha G.
;
Demirer Ş.S.
;
Utescher T.
;
Aydın A.
View/Download:22/0
River terrace development in the NE Mediterranean region (Syria and Turkey): Patterns in relation to crustal type
[期刊论文]
Quaternary Science Reviews, 2017-01-01, 166
Bridgland D.R.
;
Demir T.
;
Seyrek A.
;
Daoud M.
;
Abou Romieh M.
;
Westaway R.
View/Download:30/0
The Gediz River fluvial archive: A benchmark for Quaternary research in Western Anatolia
[期刊论文]
Quaternary Science Reviews, 2017-01-01, 166
Maddy D.
;
Veldkamp A.
;
Demir T.
;
van Gorp W.
;
Wijbrans J.R.
;
van Hinsbergen D.J.J.
;
Dekkers M.J.
;
Schreve D.
;
Schoorl J.M.
;
Scaife R.
;
Stemerdink C.
;
van der Schriek T.
;
Bridgland D.R.
;
Aytaç A.S.
View/Download:34/0
Reconstructing Early Pleistocene (1.3Ma) terrestrial environmental change in western Anatolia: Did it drive fluvial terrace formation?
[期刊论文]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2015-01-01, 417
Veldkamp A.
;
Candy I.
;
Jongmans A.G.
;
Maddy D.
;
Demir T.
;
Schoorl J.M.
;
Schreve D.
;
Stemerdink C.
;
van der Schriek T.
View/Download:26/0
The earliest securely-dated hominin artefact in Anatolia?
[期刊论文]
Quaternary Science Reviews, 2015-01-01, 109
Maddy D.
;
Schreve D.
;
Demir T.
;
Veldkamp A.
;
Wijbrans J.R.
;
van Gorp W.
;
van Hinsbergen D.J.J.
;
Dekkers M.J.
;
Scaife R.
;
Schoorl J.M.
;
Stemerdink C.
;
van der Schriek T.
View/Download:50/0
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