FIBROUS VEINS AND THEIR STRUCTURAL INTERPRETATIONS IN THE PALEOCENE-EOCENE UNITS OF THE ÇAMARDI (NİGDE) REGION
In the Çamardı region, the Nigde Massif consist of Palaeozoic-Mesozoic marble, gneiss, quartzite and amhibolite. The high-grade metamorphic rocks of massif are cut by the Cretaceous Üçkapılı granodiorite. These basement rocks were overlain by the cover rocks of Paleocene-Eocene age that display very...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
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Pamukkale University
2008-02-01
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| Series: | Pamukkale University Journal of Engineering Sciences |
| Subjects: | |
| Online Access: | http://dergipark.ulakbim.gov.tr/pajes/article/view/5000088935 |