Atıf İçin Kopyala
ROJAY F. B., Karaca A.
TURKISH JOURNAL OF EARTH SCIENCES, cilt.17, sa.4, ss.653-672, 2008 (SCI-Expanded)
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Yayın Türü:
Makale / Tam Makale
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Cilt numarası:
17
Sayı:
4
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Basım Tarihi:
2008
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Dergi Adı:
TURKISH JOURNAL OF EARTH SCIENCES
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Derginin Tarandığı İndeksler:
Science Citation Index Expanded (SCI-EXPANDED), Scopus, TR DİZİN (ULAKBİM)
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Sayfa Sayıları:
ss.653-672
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Anahtar Kelimeler:
palaeostress analysis, extensional tectonics, neotectonics, Late Miocene-Plio-Quaternary, Anatolia, TERTIARY VOLCANISM, BASIN, EVOLUTION, NEOGENE, FAULT, TECTONICS, ROTATION, AREA
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Orta Doğu Teknik Üniversitesi Adresli:
Evet
Özet
Central Anatolia, located on the immense Alpine-Himalayan orogenic belt, has a complicated neotectonic evolution, and NE-SW-trending Neogene horsts-graben systems that rejuvenate pre-existing palaeostructures are among the most important structures which help us understand the tectonic evolution of Central Anatolia.