"PETROGEOCHEMICAL FEATURES OF KSENOLITHS IN THE KOYTASH FIELD"

Ksenolits they are pieces of strauger genus whitch are met in structure of magmatic appearance are principal thing because They
show dup parts and hingh structure of mantiya of the Earth’s bark. Entering new supplements to the Earth’s bark and learning
structure of ksenolits in daykas, all of them culmination matters. At the result of researches, spreading almost equal of the
elements in structure of examples and intrusive of granodiorits and petrographic recommendation of supplement in Koytash
testify to be theic relative genus and the supplements are colled avtolits. The same conclusion belongs to gabbro suplemets of
cersutit in daykas. Because They are correspond a avtolit al nature at all of indicatours. In order to the result of researches the
conclusion, avtolits in structure of granodiorits indicate primary phases product which appeared before the only fire of magma.
Depth ksenolits in daykas are structure of Earth’s bark.