Ki­çik Qaf­qa­zın qı­zıl fi­li­zi ya­taq­la­rı me­zo­zo­yun ada qöv­sün­də­ki ar­dı­cıl di­fe­ren­si­al­laş­mış vul­kan-plu­to­nik for­ma­si­ya­sı­nın qabb­ro-dio­rit-qra­no­dio­rit-qra­nit fa­si­ya­la­rı­nın ada qöv­sü tip­li kon­ti­nen­tal kə­na­rın qa­bıq-man­ti­ya sub­duk­si­ya­üs­tü əmə­lə­gəl­mə­lə­rin­dən iba­rət­dir. On­lar  qı­zıl fi­li­zi ya­taq­la­rı­nı üç struk­tur-for­ma­si­on zonada –  me­zo­zo­yun Lök-Qa­ra­bağ və   me­zo-kay­no­zoy yaş­lı – gec tə­ba­şi­rin Göy­çə-Hə­kə­ri və qöv­sar­xa­sı spre­dinq­lə­rin ço­xakt­lı tə­za­hür et­mə­lə­ri­nə uy­ğun olan pa­leo­gen-neo­gen yaş­lı Or­du­bad zo­na­la­rın­da geo­lo­ji-ge­ne­tik tip­lər for­ma­laş­dı­rır. On­la­rın for­ma­laş­ma­sı ba­zit­lər­lə baş­la­yır və re­gi­on üçün va­hid qı­zıl fi­li­zi mi­ne­ral­laş­ma­sı­na ma­lik mis-kol­çe­dan-po­li­me­tal­ fi­liz-maq­ma­tik sis­te­mi­nin for­ma­laş­ma­sı­na sə­bəb olan, oke­an qa­bı­ğın­da si­de­ro­fil ele­ment­lə­rin şüb­hə­siz iş­ti­ra­kı ilə ada qövs­lə­ri sis­tem­lə­ri komp­leks­lə­ri­nin turş fa­si­ya­la­rı ilə so­na ça­tır. İl­kin maq­ma­tik ərin­ti­nin pa­lin­gen əri­mə­si di­fe­ren­sia­si­ya­nın ye­kun fa­za­sın­da hid­ro­ter­mal qı­zıl fi­liz­ləş­mə­si­nin bir­ba­şa əla­qə­dar ol­du­ğu flü­id­lə­rə ma­lik rio­lit-da­sit müx­tə­lif­li­yi­nin əmə­lə ­gəl­mə­si­nə sə­bəb olur. Оke­an qa­bı­ğı­nın sub­duk­si­ya olu­nan ult­raə­sa­si komp­leks sü­xur­la­rı­nın ser­pen­tin­ləş­mə­si za­ma­nı azad ol­muş qı­zıl­la onun ­qar­şı­lıq­li tə­si­ri, tək­rar əri­mə pro­se­sin­də və qı­zı­lın sü­xur­dan flüi­də keç­mə­si onun kon­sent­ra­si­ya­laş­ma­sı­nı və qı­zıl fi­li­zi yı­ğım­la­rı­nın əmə­lə gəl­mə­si­ni şərt­lən­di­rir.

Açar söz­lər: qöv­sar­xa­sı spre­dinq, geo­di­na­mi­ka, təs­ni­fat, ge­ne­tik tip­lər

 

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