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Articles 1 - 7 of 7
Full-Text Articles in Physical Sciences and Mathematics
Paleocene-Eocene Sediments Interbedded With Volcanics Within The Lycian Nappes : Faralya Formation, Mustafa Şenel
Paleocene-Eocene Sediments Interbedded With Volcanics Within The Lycian Nappes : Faralya Formation, Mustafa Şenel
Bulletin of the Mineral Research and Exploration
No abstract provided.
Geology And Petrology Of The Neogene Volcanics In The Vicinity Of Hinis-Varto-Karliova Region-Turkey, Niyazi Tarhan
Geology And Petrology Of The Neogene Volcanics In The Vicinity Of Hinis-Varto-Karliova Region-Turkey, Niyazi Tarhan
Bulletin of the Mineral Research and Exploration
No abstract provided.
Geology And Mineralogy Of The Bi̇gadi̇ç Borate Deposits And Vicinity, Cahit Helvaci, Orhan Alaca
Geology And Mineralogy Of The Bi̇gadi̇ç Borate Deposits And Vicinity, Cahit Helvaci, Orhan Alaca
Bulletin of the Mineral Research and Exploration
No abstract provided.
Geology And Origin Of Clay Deposits At Orta (Çankiri) Area, Asuman G. Türkmenoğlu, Orhan Akiman, Serdar Aker, Ayla Tankut
Geology And Origin Of Clay Deposits At Orta (Çankiri) Area, Asuman G. Türkmenoğlu, Orhan Akiman, Serdar Aker, Ayla Tankut
Bulletin of the Mineral Research and Exploration
No abstract provided.
The Geology Of The Sivas-D1vri̇ği̇-Taşlitepe Iron Placer And Its Mining, Hüseyin Öztürk
The Geology Of The Sivas-D1vri̇ği̇-Taşlitepe Iron Placer And Its Mining, Hüseyin Öztürk
Bulletin of the Mineral Research and Exploration
No abstract provided.
Hydrocarbon Potential Of The Kahramanmaraş And Elbi̇stan Areas, Yüksel Önem
Hydrocarbon Potential Of The Kahramanmaraş And Elbi̇stan Areas, Yüksel Önem
Bulletin of the Mineral Research and Exploration
The Taurus mountains, which developed in the conjoining zone of the Anatolian and Arabian Plates, underwent a disruption between Bolkar mountain and Engizek mountain. This can be explained by the fact that the area was traversed and transformed by two major strike-sup faults situated at Mersin-east Bolkar mountain-Kayseri in the west and Antakya (Hatay)-Elazığ-Bingöl in the east, In fact, the east-west oriented 200 km. wide area, covering the Gulf of İskenderun and the northern pan of Adana, was compressed and deflected as far as the north of Sarız and the Arabian Plate was dislocated prior to the faulting and moved …
Facies And Depositional Environments Of The Miocene Sedimentary Sequence In North Of Torbali, Izmir, Uğur İnci̇
Facies And Depositional Environments Of The Miocene Sedimentary Sequence In North Of Torbali, Izmir, Uğur İnci̇
Bulletin of the Mineral Research and Exploration
No abstract provided.