Depositional evolution of the Soma coalfield, Western Turkey: A preliminary and probably in allochthonous peat mires of a braided river system that
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Braided river deposits related to progressive Miocene surface uplift in Kahraman Mara? area, SE Turkeydoi:10.1002/(sici)1099-1034(199901/06)34:1/2159
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Sedimentological architecture of the Ballik continental carbonates, SW Turkey, The conglomerates correspond to braided river deposits. This siliciclastic
an Active Strike-Slip Basin, Southeastern TurkeyFluvial deposits consist of braided channel and single faults and are long, gently-sloping,
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Multiaxis three dimensional (3D) woven and braided preform unit cells and (BAP), Kayseri /TURKEY Position : Principal Investigator Project No : FBY-
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braid delta or braidplain with local ponds (4) high sediment accumu- lation rates implying Turkey (Yosh- ioka, 1996) and in restricted
Southern Turkey: implications for the inception braided rivers depositing coarse conglomerates in (40.4 Ma) and before the Aquitanian (23.03
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studied in an area north of Ankara, Turkey. flows, with subordinate braided-stream distributgrouped in four lithofacies associations are
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(Late Miocene-Early Pliocene), Eastern Elazığ, Eastern TurkeyThe braided river deposits is characterized by parallel bedded conglomerate,
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The Manisa basin is one of the areas studied braided river, meandering river, flood plain, Önder KayadibiGeological Congress of Turkey
A different approach to age range of Neogene sediments in SW TurkeyBesides, meander and braided river conglomerates and sandstones, and also
Multiaxial and multilayered 8-step circular braided preform for composite (BAP), Kayseri /TURKEY Position : Principal Investigator Project No : FBY-
in contact is obtained using semi-empirical single braid optimization formulasAkdeniz University, Antalya, TurkeyInternational Kharkiv Symposium on Physics
and Gelibolu (Gallipoli) Peninsula paleoenviroments , (North Aegean, Turkey)Gelibolu, such as turbidities, deltas, lacustrine, braided rivers, reefs,
Braided river deposits related to progressive Miocene surface uplift in Kahraman Mara area, SE Turkey (p 159-174)doi:10.1002/(SICI)1099-1034(199901/
River response to Quaternary tectonics with examples from northwestern Anatolia, Turkey on ResearchGate, the professional network for scientists. to Quate
SEDIMENT IN ŞELMO FORMATION OUTCROPPING AT SOUTH OF ADIYAMAN (TURKEY)The Tırpal Member is represented by conglomeratic facies of braided
Turkey, provides a record of environmental change braided rivers depositing coarse conglomerates in (40.4 Ma) and before the Aquitanian (23
