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TECTONOSTRATIGRAPHY AND KINEMATICS OF THE EASTERN END OF THE SIVAS BASIN (CENTRAL EASTERN TURKEY) - IMPLICATIONS FOR THE SO-CALLED ANATOLIAN BLOCK
(JOHN WILEY & SONS LTD, 1993)
The eastern end of the Sivas Basin, just west of Erzincan, is known as the Kemah Basin. The lithostratigraphy of the Kemah Basin thus corresponds with the general characteristics described for the Sivas Basin: the upper ...