Yayınlanmış 1 Ocak 2019
| Sürüm v1
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Açık
Geochemical Evidences of Paleoenvironmental Changes in Late Quaternary Lacustrine Sediments of the Konya Closed Basin (Konya, Turkey)
Oluşturanlar
- 1. Selcuk Univ, Dept Geol Engn, Konya, Turkey
- 2. Canakkale 18 Mart Univ, Dept Geol Engn, Canakkale, Turkey
- 3. DSI 4 Reg Directory, Konya, Turkey
- 4. Selcuk Univ, Dept Phys, Konya, Turkey
- 5. Dokuz Eylul Univ, Dept Phys, Izmir, Turkey
- 6. Cukurova Univ, Dept Geol Engn, Adana, Turkey
Açıklama
Important geochemical evidence reflecting Quaternary climatic changes was obtained by evaluating geochemical data from 51 samples and datings from 3 samples by ESR method from sediments of a 7-m-deep trench in Great Konya lake area at the southwest of Adakale village (Konya, Turkey). The geochemical data indicate that the study area was influenced, four times, by a climate having strong precipitation, which caused strong erosion and high detrital input between 25,276 +/- 1732-year BP and approximately 50,000-year BP. These periods correspond to climatic changes during the last glacial periods, the warm climate of D-O-2, D-O-5, D-O-6 and D-O-14 events and the cold climate of H2, H3, H4 or H5 and H6 events.
Dosyalar
bib-8fa3d366-20a8-4c2d-b958-f6e99271993e.txt
Dosyalar
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