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Introduction
Mustafa Cihan has been pursuing his MBA degree at İstanbul Bilgi Üniversitesi. He works in the mining industry as Exploration Manager. He continues his research on Structural Geology, Ore Geology, and Mineral Exploration. Their most recent publication is 'Inter-relationships between deformation partitioning, metamorphism and tectonism'.
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Publications
Publications (13)
Öksüt is a breccia-hosted high-sulfidation epithermal gold-copper deposit, situated within the Develidag Volcanic Complex in south-central Anatolia. The volcanic complex, exposed on the northern edge of the Tauride range, is largely made up of late Miocene andesitic to dacitic porphyries, covered by a succession of Pliocene basalts and basaltic and...
The Öksüt high sulfidation (HS) epithermal Au (-Cu) deposit (35.32 million tonnes of ore at 1.22 g/t Au) is located in the Central Anatolian Volcanic Province (CAVP) at the south-eastern segment of the Central Anatolian Crystalline Complex (CACC). The deposit is hosted by large hydrothermal breccia bodies and hornblende-rich basaltic andesite porph...
Öksüt (Kayseri) high sulfidation epithermal gold mineralization is located in Central Anatolian Volcanic Province (CAVP a part of the Central Anatolian Crystalline Complex (CACC) and Tethyan Metallogenic Belt (TMB). According to petrographic and geochemical studies, the host rock of the mineralization is hornblende-rich basaltic andesite and covere...
Kayseri'nin 45 km uzağındaki Öksüt köyü yakınlarında bulunan Öksüt yüksek sülfidasyon epitermal altın cevherleşmesi, Orta Anadolu Volkanik Provensi'nde (OAVP) yer almaktadır. Öksüt epitermal cevherleşmesi Keltepe, Keltepe KB, Boztepe, Boztepe B, Büyüktepe, Güneytepe ve Yelibelentepe olmak üzere 7 potansiyel cevher zonlarından oluşmaktadır. Keltepe...
Thrusting from the east loaded the thick Pomfret dome stratigraphic sequence in Vermont to such an extent that by the time the first schistosity had formed it was 20 km deep. This occurred without garnet growth even though rock compositions were ideal for this phase to grow before they reached this depth. The rocks remained at this depth until garn...
Breccias are commonly regarded as having random fabrics, but clast alignment can cause significant fabric anisotropy. Orientation and shape are two complementary aspects of clast anisotropy. Standard circular statistics can be used to characterize orientation anisotropy, such as the direction and length of the mean resultant vector (with standard e...
EPMA dating of monazite confirms the relative timing of a succession of Foliation Intersection Axis trends in porphyroblasts (FIAs) and two periods of progressive metamorphism intervened by retrogression in the Robertson River Metamorphics (NE Australia). A complete pressure-temperature-deformation-time (P-T-D-t) path has been deciphered involving...
The successions of inclusion trail asymmetries defining foliation intersection/inflection axes (FIAs) preserved in porphyroblasts document the geometry of deformation associated with folding and fabric development during discrete episodes of bulk shortening and suggest that deformation histories are commonly more complex than previously considered....
Understanding the relationships of inclusion trail geometries in porphyroblasts relative to matrix foliations is vital for unravelling complex deformation and metamorphic histories in highly tectonized terranes and the approach used to thin sectioning rocks is critically important for this. Two approaches have been used by structural and metamorphi...
West Anatolia, together with the Aegean Sea and the easternmost part of Europe, is one of the best examples of continental extensional tectonics. It is a complex area bounded by the Aegean–Cyprus Arc to the south and the North Anatolian Fault Zone (NAFZ) to the north. Within this complex and enigmatic framework, the Sandıklı Graben (10 km wide, 30 ...
