Abstract
The Tauride range in southern Turkey is flanked and overlain by Neogene sedimentary basins. To the south and on top of the high range, these basins are mainly marine, whereas poorly studied intramontane basins dominated by continental deposits are exposed to the north. In this paper, we study the stratigraphy and structure of the continental Altinapa Basin, and provide
Original language | English |
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Pages (from-to) | 134-155 |
Journal | Tectonophysics |
Issue number | 532 |
DOIs | |
Publication status | Published - 2012 |