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Subduction-accretion complex Metamorphism Tectonics Petrology Geochronology. Greater Antillean Arc The Sancti Spiritus Dome of the eastern Escambray Cuba represents a metamorphic fold and thrust structure which was part of the Cretaceous subduction-accretion complex of the Greater Antillean Arc. The oldest rock fabrics are preserved in eclogite- and blueschist-facies rocks of the Gavilanes unit, indicating arc-parallel extension. Field observations and fabric studies show that greenschist-facies dynamic indicators are dominated by top-to-NE tectonic transport in the lowermost nappes. The greenschist-facies shear zone between the Yayabo unit and the Mabujina unit is viewed as the main detachment zone between the subduction complex and the overlying arc complex. Active subduction ceased at about 70 Ma SHRIMP zircon dating of basement nd cover sequences in the Strangways Metamorphic Complex indicates that the Strangways Orogeny consisted of two distinct tectonothermal cycles between ca 1.

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Delete comment or cancel. E onde ocorre este processo? Please log in to add rochas metamorficas comment. Reidel, Dordrecht, pp. In: Inda, H. South Am.

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