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Mesoscopic and microscopic structures along the contact between Menderes massif and Lycian nappes
2021ÖZET Milas bölgesinde Menderes Masifinin güney kesimi ile Likya Naplannın batı kesimi yüzlek verir. Likya Naplan ince serpantinit dilimlerinin bulunduğu, güneye eğimli, düşük açılı tektonik bir dokanak boyunca Menderes Masifini üstlemektedir. Neojen yaşlı karasal tortullar bu iki tektonik kuşağa ait kayaları açısal uyumsuz bir dokanak boyunca örter ...
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FORMATION OF PODIFORM DUNITES IN THE LYCIAN PERIDOTITE NAPPES (AGLA - KOYCEGIZ, SW TURKEY)
2009In this study, the whole-rock major oxides, trace elements and mineral chemistry of the Agla peridotites (comprising host harzburgites and podiform dunites) are investigated to determine the formation mechanisms of the Agla podiform dunites (SW Turkey).
Gnos, Edwin +4 more
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Geology of the Menderes Massif and the Lycian Nappes South of Denizli, Western Taurides
1987Mount Honaz region in the Western Taurides is made up of superimposed several tectonic units. In the west, monotonous green metashales called the Honaz shale occur at the base of the tectonic stack. Honaz shale is tectonically overlain by weakly metamorphosed, massif white limestone, thinly bedded cherty limestone and shale which covers the Mendercs ...
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The extension of the Lycian Nappes (SW Turkey) into the Southeastern Aegean Islands
1974Bernoulli, Daniel +2 more
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FORMATION OF PODIFORM DUNITES IN THE LYCIAN PERIDOTITE NAPPES (AĞLA - KOYCEĞIZ, SW TURKEY)
, 2009Mehmet Akbulut +4 more
semanticscholar +1 more source
Environmental Monitoring & Assessment, 2019
M. Gül, K. Zorlu, Muratcan Gül
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M. Gül, K. Zorlu, Muratcan Gül
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