Paleomagnetic Reconstruction for the Origin of the Supra- Subduction Zone Ophiolites during the Progressive Closure of the Neotethys Ocean in Eastern Mediterranean

The paleomagnetic data comprise stereonets from tilt corrected each site used for mean direction. The results contain rocks from the Hatay, Koçali, Göksun, İspendere, Kömürhan and Guleman ophiolites as well as from the overlying sedimentary units emplaced in  SE Anatolian region. Specimens of each site were described with its declination/inclination and MAD angles.