(The general geomorphological features and evolution of the western part of the Elazig district, Turkey).
| dc.contributor.author | Tonbul, S. | |
| dc.date.accessioned | 2026-08-12T16:10:31Z | |
| dc.date.issued | 1987 | |
| dc.department | Fırat Üniversitesi | |
| dc.description.abstract | The district has been formed as a swell between Malatya depression on the west and Elazig-Uluova depression on the east and in general, it shows a plateau character which has the average elevation of 1300-1400 m. The high parts of both Hasandagi and Bulutlu and Piran mountain chains are seen as two separate erosional surfaces (Pre-Miocene and Lower Miocene surfaces) which have formed from which different levels from one another. -from English summary | |
| dc.identifier.endpage | 52 | |
| dc.identifier.issn | 0250-2844 | |
| dc.identifier.scopus | 2-s2.0-0023469489 | |
| dc.identifier.scopusquality | N/A | |
| dc.identifier.startpage | 37 | |
| dc.identifier.uri | https://hdl.handle.net/11508/41981 | |
| dc.identifier.volume | 15 | |
| dc.indekslendigikaynak | Scopus | |
| dc.language.iso | tr | |
| dc.relation.ispartof | Jeomorfoloji Dergisi | |
| dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | |
| dc.rights | info:eu-repo/semantics/closedAccess | |
| dc.snmz | KA_Scopus_20260511 | |
| dc.title | (The general geomorphological features and evolution of the western part of the Elazig district, Turkey). | |
| dc.title.alternative | Elazig batisinin genel jeomorfolojik ozellikleri ve gelisimi. | |
| dc.type | Article |
