Characteristic Features of the Late Precambrian Felsic Magmatism in Western Anatolia: Implications for the Pan-African Evolution in NW Perigondwana

Gondwana Research

Volumn 4, Issue 2, 2001, Pages 169-170

  Gursu S ^a   Goncuoglu M C ^b  

^a GENERAL DIRECTORATE OF MINERAL RESEARCH AND EXPLORATION   (Turkey)

^b MIDDLE EAST TECHNICAL UNIVERSITY   (Turkey)

Author keywords

[No Author keywords available]

Indexed keywords

FELSIC ROCK; GONDWANA; MAGMATISM; PRECAMBRIAN; TECTONIC EVOLUTION; TECTONIC SETTING;

ANATOLIA; TURKEY;

EID: 0010405413     PISSN: 1342937X     EISSN: None     Source Type: Journal    
DOI: 10.1016/S1342-937X(05)70680-8     Document Type: Article

References (5)

1. nd Geological Congress of Turkey, pp. 263-271.
2. Barbarin, B. (1999) A review of the relationships between granitoid types, their origins and their geodynamic environments. Lithos, v. 46, pp. 605-626.
3. Dean, W.T. and Özgül, N. (1994) Cambrian rocks and faunas, Hüdai area, Taurus Mountains, southwestern Turkey. Bull. Inst. Royal Sci. Natur. de Belgique, Sci. de la Terre, v. 64, pp. 5-20.
4. Kozlu, H. and Göncüoglu, M.C. (1996) Stratigraphy of the infraCambrian rock-units in eastern Taurides and their correlation with similar units in southern Turkey. In: Göncüoglu, M.C. and Derman, A.S. (Eds.), Early Paleozoic evolution in NW Gondwana. Turkish Assoc. Petrol. Geol. Spl. Pub., v. 3, pp. 50-60.
5. Uchmann, B., Erdogan, B. and Güngör, T. (2000) Trace fossil assemblages and age of the porphyroid-bearing metasandstones in the Sandikli region. IESCA Abstracts, p. 78.