Özet:

The work area is located within the Southeast Anadolu Orogenic Generation (GDAOB), approximately 50 km south of Elazığ Island. In the field of study, the old Kretase Higher Higher Complex volcanoes were possibly tectonicly overturned by the harzburgy, diny and lerzolithic manto collects of the Coal Offioliths at the end of Mesozoic. The High-Level Complex, Permo-Triyas Old Püürge Metamorphs, whereas the place is not consistently placed, the place is also tectonic touched. The volcanic rocks around Uslu (Elazığ G) are massive lavas and are basaltic compositions. Mineral and tissue-recognizable volcanic stones are rich in beach-class and impacto oxide minerals. Secondly, calcium is a mineral pressure. Amygdaloidal tissue is common. Based on the distribution of trace elements normalized according to the N-OOSB; LIL elements according to the HFS elements; and light rare soil elements (HNTEs) show a richer distribution than heavy rare soil elements (ANTEs). As a result; geochemical data indicate the opening of oceanic broadcast that when this situation is assessed along with previous data, it shows that volcanic phasees that survive around Uslu have no correlation with the Mining Complex.

Anahtar Kelimeler:

Özet:

The study area is located approximately 50 km south of Elazığ city within the Southeastern Anatolian Orogenic Belt (SEAOB). In the area, the volcanic rocks of the Upper Cretaceous Yüksekova Complex were tectonically overlain by mantle cumulates consisting of harzburgite, dunite and Iherzolites belonging to the Late Cretaceous aged Kömürhan Ophiolites. The Yüksekova Complex unconformably overlies the Permo-Triassic Pütürge Metamorphics and in places has tectonic contact. The volcanicrocks around Uslu (S Elazığ) are massive lavas and have basaltic composition. Mineralogically and texturally recognizable lavas are rich in plagioclase and opaque oxide minerals. Secondarily, calcite mineral is dominant. Amygdaloidal textures are common. According to the trace element distributions of the rock samples normalized to N-OOSB; LIL elements are enriched according to HFS elements. LREEs, on the other hand, show a richer distribution than HREEs. As a result; the geochemical data together with previous studies point to the rifting of the oceanic arc, which reveals that the volcanic facies outcropping around Uslu have no genetic relationship with the Maden Complex.