Kür çö­kək­liyi sa­hə­si­nin pa­leo­me­zo­zoy geo­lo­ji ta­ri­xi­nə aid mə­lu­mat­la­rın az ol­ma­sı, pa­leo­zo­ya aid fakt­la­rın mü­qa­yi­sə­li ana­liz ba­xı­mın­dan araş­dı­rıl­ma­ma­sı və ən əsa­sı isə, geo­fi­zi­ki mə­lu­mat­la­rın bə­zi sa­hə­lər­də düz­gün təh­lil olun­ma­ma­sı sə­bə­bin­dən Kür çö­kək­li­yi haq­qın­da və, ümu­mi­yət­lə, Qaf­qazın geo­lo­gi­ya­sın­da bir-bi­ri ilə uz­laş­ma­yan səhv fi­kir­lər de-fak­to sə­viy­yə­sin­də təq­dim olun­muş­dur. Müa­sir dövr­də geo­di­na­mik təd­qi­qat­lar Yer elm­lə­ri­nin ən prio­ri­tet is­ti­qa­mət­lə­rin­dən ol­ma­sı­na bax­ma­ya­raq, tə­əs­süf ki, son vaxt­la­ra qə­dər Kür  çö­kək­liyi sa­hə­si­nin mo­bi­lizm ba­xı­mın­dan fa­ne­ro­zoy geo­tek­to­nik və geo­di­na­mik tə­ka­mül ta­ri­xi və çö­kək­li­yin ay­rı-ay­rı blok­la­rı­nın subst­ra­tın­da iş­ti­rak edən Pa­leo-və Me­zo­te­ti­sin struk­tur-geo­mor­fo­lo­ji pleyt­tek­to­ni­ka­sı aş­kar olun­ma­mış­dır. Hə­min mə­sə­lə­lə­rin araş­dı­rıl­ma­sı Qaf­qazın geo­lo­gi­ya­sın­da prob­lem mə­sə­lə­lə­ri əha­tə et­mək­lə bə­ra­bər, Kür çö­kək­li­yi­nin neft-qaz po­ten­sia­lı­nın qiy­mət­lən­di­ril­mə­si üçün çox mü­hüm əhə­miy­yət kəsb edir. Ilk də­fə ola­raq Me­zo­te­ti­sin Qaf­qaz seq­men­ti tim­sa­lın­da Kür çö­kək­liyi sa­hə­si­nin geo­di­na­mik tə­ka­mü­lün­də pleyt­tek­to­nik möv­qe­yi, ay­rı-ay­rı blok­la­rın struk­tur-geo­mor­fo­lo­ji tip­lə­ri, kon­so­li­da­si­ya də­rə­cə­si­nə və ya­şı­na gö­rə subst­ra­tın me­zok­rat-ba­zit və ley­kok­rat yet­kin kon­ti­nen­tal­yön­lü ol­ma­sı aş­kar edil­miş­dir. Li­tos­fer pli­tələri tek­to­ni­ka­sı­nın ən sə­ciy­yə­vi xü­su­siy­yət­lə­ri­nə ye­ni re­gi­on qütb­ləş­mə qa­nu­na­uy­ğun­lu­ğu əla­və olun­muş­dur. On­la­rın təs­vi­ri Te­ti­sin ke­çid mər­hə­lə­lə­ri üz­rə tər­tib olun­muş xə­ri­tə və mo­del­lər­də öz təs­di­qi­ni tap­mış­dır.

Açar sözlər: geodinamika, paleotektonika, Mezotetis, pleyttektonik strukturlar, maqmatizm, spredinq, dərinsulu hövzə, plitə

 

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