Faruk Ocakoğlu
Eskisehir Osmangazi University, Eskisehir
Activity
2023
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DRIP TECTONICS AND THE DRIVERS OF PROTO-PLATEAU DEVELOPMENT IN COLLISIONAL OROGENS – INSIGHTS FROM CENTRAL ANATOLIA
T226 Geological and Geophysical Constraints on Orogenic Architecture as Windows to Tectonic Style Through TimeWednesday, 18 October 20238:00 AM - 12:00 PM326
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UNCOVERING HIDDEN PROVENANCE SIGNALS USING DETRITAL RUTILE: NEW PERSPECTIVES ON DATA WORKFLOWS
T245 Advances in Detrital Heavy Minerals: Applications and Methods (Posters)Wednesday, 18 October 20238:00 AM - 5:30 PMHall B
2022
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THE UTILITY OF DETRITAL RUTILE U-PB AND TRACE ELEMENTS IN ACCRETIONARY OROGENIC SETTINGS
T108 Advances and Applications of Thermochronology in Tectonic, Magmatic, Basin, and Geomorphic Studies IIMonday, 10 October 20221:30 PM - 5:30 PM601
2021
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FOREARC AND FORELAND BASIN EVIDENCE FOR PROTRACTED LATE CRETACEOUS-EOCENE COLLISION IN WESTERN ANATOLIA
T168 Initiation and Evolution of Arc-Forearc Systems in Cascadia and BeyondTuesday, 12 October 20211:30 PM - 5:30 PMPortland Ballroom 257 (Hybrid Room)
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THE PHYSIOGRAPHIC RESPONSE TO CENOZOIC DRIP TECTONICS IN CENTRAL ANATOLIA
T7 Tectonometamorphic Evolution of the Mediterranean from the End of the Variscan Orogeny to PresentSunday, 10 October 20218:00 AM - 12:00 PMA106
2020
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SUBDUCTING GONDWANAN-AFFINITY PASSIVE MARGIN TRIGGERED LATE CRETACEOUS BACK-ARC EXTENSION OF THE BLACK SEA
157 D26. Structural Geology & Tectonics IIWednesday, 28 October 20205:30 PM - 8:00 PMMeeting Rooms
2019
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DID THE CENTRAL ANATOLIAN CANKIRI BASIN FORM AS A RESULT OF AN OLIGO-MIOCENE RAYLEIGH-TAYLOR INSTABILITY? IMPLICATIONS FOR EARLY MIOCENE PLATEAU DEVELOPMENT IN CENTRAL ANATOLIA
T292 From Oceanic Subduction to Inter-Continental Collision: Examples of Convergent Margin Processes in Non-Collisional and Collisional SettingsWednesday, 25 September 20191:30 PM - 5:30 PMRoom 231ABC, North Building