Özet:

In the area of Turoniyen-Koniyasiyen yafll› basalt and pyroclastites, Koniyasiyen-Santoniyen yafll› dasit/riyodasit and pyroclastites with Kampaniyen-Maestrihtiyen (?) Yafll’s biotithic and pyroclastites are surface. The Cretase-Paleosen It is the one that gives righteousness to the wicked, and the one that gives righteousness to the wicked, and the one that gives righteousness to the wicked. Granitoyidi, which is usually non-sphlected, thin-sphleated porphyric, ground-site summer and micropegmatic tissue, contains quvars, ortoclas, plajiyoclas, hornblend, biotite, accessory apatite and sphen, secondary chloride, epidot and calcite. Mineral thermometer and barometer calculations indicate ~650-700oC and ~0.9-1.5 (χ -) kbar’l›k crystallization coffles›n. Granitoyidi is geochemically characterized by I-type, calcalin, peralumin of metal (A/CNK=0.9-1.2) character, fractionalflm›fl and aluminium-cachemic (ALCAF). The main and trace element also reveals that the rock’n’roll’s “mlaflman” was important. The eye element is also similar to one another, and the basic examples K, Rb, Ba and Th show more wealth than see m. The rare soil element is also a medium-sized richleflmifl (LaN/LuN=1-2) and a head-k flekiled, with a possible hornblend and beach-clastic distinction of mlaflmas’n’ yans’tmaktad’. Granitoyidi is a hybrid main magma, and this main magma is likely covered by the foam and manto sources›n›r. Granite magman’s crystallization, in the relatively profound parts of the foam cage (~6 km) by bafllam’fl and magma elevation with s’¤ in the depths (~3 km) completion by flt’r.

Anahtar Kelimeler: