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BURMACHAN KAMARNING POSTKOLLIZION BOSQICHINING RIVOJLANISHI VA POSTKOLLIZION GRANITOIDLARNING SHAKLLANISHI

Fan yo'nalishi:GeologiyaMetall va qotishmalar
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MAQOLA ANNOTATSIYASI

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Mazkur maqolada burmali kamarlarning postkollizion bosqichdagi rivojlanishi hamda postkollizion granitoidlarning shakllanish mexanizmlari tahlil qilingan. Wilson sikli doirasida kontinental kolliziyadan keyingi geodinamik jarayonlar, jumladan litosfera delaminatsiyasi, gravitatsion kollaps, rifting va transkorov siljishlarning magmatizmga ta’siri ko‘rib chiqilgan. Shuningdek, postkollizion magmatizmning tarkibiy xususiyatlari, manbalari va granitoidlar hosil bo‘lishining geodinamik modellari umumlashtirilgan.

MUALLIFLAR

Science ID: FQD-0426-0008

Teglar

# magmatizm# litosfera# bosqich# granitoidlar# postkollizion# wilson# sikli# delaminatsiya# orogen# geodinamika# kolliziya# rifting

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[2] Taymaz, T., Yilmaz, Y., & Dilek, Y. (2007). The geodynamics of the Aegean and Anatolia: Introduction. Geological Society, London, Special Publications, 291(1), 1–16. https://doi.org/10.1144/SP291.1

[3] Atwater, T. (1970). Implications of plate tectonics for the Cenozoic evolution of western North America. Geological Society of America Bulletin, 81(12), 3513–3536. https://doi.org/10.1130/0016-7606(1970)81[3513:IOPTFT]2.0.CO;2

[4] Chenin, P., Manatschal, G., Lavier, L., Mohn, G., & Kusznir, N. (2017). Potential role of lithospheric mantle composition in the Wilson cycle: A North Atlantic perspective. In The Wilson Cycle Revisited. Geological Society, London, Special Publications. https://doi.org/10.1144/SP470.1

[5] Wilson, J. T. (1966). Did the Atlantic close and then reopen? Nature, 211(5050), 676–681. https://doi.org/10.1038/211676a0