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3. Geophysical Data (Gravity and Magnetic) from the Area Between Adana, Kahramanmaras and Hatay in the Eastern Mediterranean Region: Tectonic Implications

Author

Rahime Sen, Uğur Akin, Semir Over, Mühendislik ve Doğa Bilimleri Fakültesi -- İnşaat Mühendisliği Bölümü, and Över, Semir

Subjects
Geochemistry & Geophysics, Anatolian fault, Derivative ratios, Turkey, 010504 meteorology & atmospheric sciences, Eurasian plate, Fault (geology), 010502 geochemistry & geophysics, Magnetic storage, 01 natural sciences, Kahramanmaras, Quaternary deposits, Bromelia plumieri, Active tectonics, Sea, geography.geographical_feature_category, North Anatolian Fault | Marmarum Sea | Fault Zone, Mediterranean Region, Eurasian Plate, Anomalies, Subduction, Geophysics, Magnetic methods, Southern neotethys, Geology, Evolution, Eastern Mediterranean, Gravity and magnetic methods, Ophiolites, Structural basin, Ophiolite, Magnetic method, Western Turkey, Tectonic framework, Adana [Turkey], Paleontology, Geochemistry and Petrology, Tectonic implications, Plate boundary, Hatay, Anatolia, Arabian plate, 0105 earth and related environmental sciences, East Mediterranean, Metadata, geography, Alpine-himalayan belt, Faulting, Tectonics, Geomagnetism, Block (meteorology), Plates (structural components), Fault, Plate tectonics, SE Anatolia, Gravity survey, Quaternary
Abstract

WOS: 000435590500018, The gravity and magnetic maps of the area between Adana-Kahramanmaras-Hatay provinces were produced from a compilation of data gathered during the period between 1973 and 1989. Reduced to the pole (RTP) and pseudo-gravity transformation (PGT) methods were applied to the magnetic data, while derivative ratio (DR) processing was applied to both gravity and magnetic data, respectively. Bouguer, RTP and PGT maps show the image of a buried structure corresponding to ophiolites under undifferentiated Quaternary deposits in the Adana depression and Iskenderun Gulf. DR maps show two important faults which reflect the tectonic framework in the study area: (1) the Karatas-Osmaniye Fault extending from Osmaniye to Karatas in the south between Adana and Iskenderun depressions and (2) Amanos Fault (southern part of East Anatolian Fault) in the Hatay region running southward from Turkoglu to Amik Basin along Amanos Mountain forming the actual plate boundary between the Anatolian block (part of Eurasian plate) and Arabian plate.

Published
2018
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