EASTERN- AND WESTERN-TYPE ULTRAMAFIC MASSIFS OF THE MIRDITA OPHIOLITE, ALBANIA: INTRAOCEANIC DETACHMENT FAULT SYSTEM OR COMPRESSIONAL OROGENIC SUTURE?
The Western-type mantle-crust transition is exposed in the Puka and Krabbi ultramafic massifs. Here, the mantle displays zones of lithospheric ductile flow 10s of m wide. The crust/mantle transition is also marked by amphibolitized layers of crustal and mantle rocks affected by intense ductile shearing. These ductile shear zones trend parallel to the mantle-crust transition, and are locally associated with cataclastic breccias of peridotite, gabbro and basalt. The amphibolite-breccia complexes are interpreted as slivers of crust and mantle entrained into syn-oceanic extensional detachments. The overall lithologic pattern also implies fault-related excision of the ophiolite pseudostratigraphy, indicating these are not compressional orogenic structures, and suggesting instead that Western-type ultramafic massifs were exhumed prior to obduction as oceanic core complexes. The lack of time gaps for the formation of Eastern- and Western-type massifs, the presence of extension-related structures in the Western-type mantle-crustal rocks, and the similar 40Ar/39Ar ages of metamorphic sole rocks are more consistent with formation during intermittent magmatic/amagmatic episodes of extensional tectonism, crustal excision, lower crust-mantle exhumation and formation of a lower plate-upper plate boundary between the Eastern- and Western-type massifs as implied by Model #1.