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A model with a slab window vs tectonicalY and maginageneticalY depicted斤,·interpretation可the maginatisin on the caslej,mat}gin ol"the Eu二,sia continent il the Cretaceous. It has isochronouWY caused the active inagmatislus il‘,row obliquelysiretching across the margin and migrated about 7000 kil along the margin.加。,the vouthern part‘扩Guangxi in South China to the.far eastern region以、Russia. The slab window calne into being tit the subdiuvion part of' the oceanic ridge between Kula and Pacific plates and promoted the upiveling oj the hot asthenosphere to fi/ the window gal). Sonle。,/the gabbroic rocks exposed in this area inav hare 11-aImported heat.1r'om the slab windot, into the lower crust, where the granitic magma is generated bv the assimilation with the crustal niater to八)"n the greater magma chambers. The vindow width and the migration speed (ire taken on the hasis。厂the statistical anah'sis可the g二,nie age data in Southwest JUIR17, which corresponds to the refe'ren〔二field tit the Eurasia east niargin based on recommended geoscient功c data and information.

Slab window-related magmatism caused by the Kula-Pacific ridge subduction beneath the Eurasia continent in the Cretaceous