Crustal disequilibrium of the central Pontides (northern Turkey) due to oroclinal bending revealed by gravity modelling
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DOI: 10.1016/j.jseaes.2019.104058
Abstract: Abstract The Turkish Pontide orogenic belt belongs to the former Eurasian margin, which is the result of two major successive processes of the closure of the Tethyan oceans: subduction followed by collision. This almost E-W… read more here.
Keywords: crustal thickness; northern turkey; gravity; gravity modelling ... See more keywords