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Including massive to foliated rocks (Seck et al. 1996). Based on textural criteria and the resemblance of their REE patterns to those of the Tsaki metabasalts, the Syros glaucophanites may have been derived from similar, moderately enriched basaltic protoliths. The textural variability of Syros eclogites and garnet glaucophanites is also reflected in their REE patterns. The coarser-grained, massive members have low to moderate total abundances of REE and positive Eu anomalies that suggest cumulate gabbro precursors.

8; Stolz et al. 1997). However, this cannot account for a major penetrative regional metamorphism observed in all rock types and exposures of the Tinos Upper Unit. Given the field evidence for early oceanic thrusting, Katzir et al. (1996) suggested that metamorphism was induced by continued thrusting and piling of nappes that have created the necessary overburden to cause greenschist-facies conditions. Based on K –Ar ages on amphiboles extracted from an amphibolite-facies slice that constitutes the topmost part of the Upper Unit on Tinos (Patzak et al.

Given the field evidence for early oceanic thrusting, Katzir et al. (1996) suggested that metamorphism was induced by continued thrusting and piling of nappes that have created the necessary overburden to cause greenschist-facies conditions. Based on K –Ar ages on amphiboles extracted from an amphibolite-facies slice that constitutes the topmost part of the Upper Unit on Tinos (Patzak et al. 1994), a Late Cretaceous age was assigned to the metamorphic event that affected the entire sequence of the Upper Unit (Katzir et al.

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