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Paleoseismological investigations on a slow-moving active fault in central Anatolia, Tecer Fault, Sivas
paleoseismology earthquake slow-moving fault central Anatolia
2015/8/26
Tecer Fault is a N60˚-70˚E-trending, left-lateral, strike-slip fault to the south of the town of Sivas, Turkey. This fault is considered as the eastward continuation of Deliler Fault, which ...
Repetitive Subtidal-to-Coastal Sabkha Cycles from a Lower-Middle Miocene Marine Sequence, Eastern Sivas Basin
Cycle Evaporite Parasequence Sabkha Subtidal Sivas Basin
2009/7/8
In the study area, southeast of Zara in the Sivas Basin, the Lower-Middle Miocene marine Karacaören Formation consists of a succession of marine sedimentary rocks deposited within two trangressi...
The Evolution of Travertine Masses in the Sivas Area (Central Turkey) and Their Relationships to Active Tectonics
active tectonics earthquake Sivas Basin Sı cak Ç ermik travertine travitonics U/Th age dating Quaternary geology
2009/7/7
Sıcak Çermik, Delikkaya and Sarıkaya are important travertine fields with active hot springs located 31 km west of Sivas. Based on their morphology, most of the travertines are classi...