LAPIERRE, H., BOSCH, D., NARROS, A., MASCLE, G. H., TARDY, M., DEMANT, A. (2007) The Mamonia Complex (SW Cyprus) revisited: remnant of Late Triassic intra-oceanic volcanism along the Tethyan southwestern passive margin. Geological Magazine, 144 (1) 1-19 doi:10.1017/s0016756806002937
| Reference Type | Journal (article/letter/editorial) | ||
|---|---|---|---|
| Title | The Mamonia Complex (SW Cyprus) revisited: remnant of Late Triassic intra-oceanic volcanism along the Tethyan southwestern passive margin | ||
| Journal | Geological Magazine | ||
| Authors | LAPIERRE, H. | Author | |
| BOSCH, D. | Author | ||
| NARROS, A. | Author | ||
| MASCLE, G. H. | Author | ||
| TARDY, M. | Author | ||
| DEMANT, A. | Author | ||
| Year | 2007 (January) | Volume | 144 |
| Page(s) | 1-19 | Issue | 1 |
| Publisher | Cambridge University Press (CUP) | ||
| DOI | doi:10.1017/s0016756806002937Search in ResearchGate | ||
| Mindat Ref. ID | 260001 | Long-form Identifier | mindat:1:5:260001:1 |
| GUID | 059dc26b-9cee-4f36-bb0c-b5b2bdd60041 | ||
| Full Reference | LAPIERRE, H., BOSCH, D., NARROS, A., MASCLE, G. H., TARDY, M., DEMANT, A. (2007) The Mamonia Complex (SW Cyprus) revisited: remnant of Late Triassic intra-oceanic volcanism along the Tethyan southwestern passive margin. Geological Magazine, 144 (1) 1-19 doi:10.1017/s0016756806002937 | ||
| Plain Text | LAPIERRE, H., BOSCH, D., NARROS, A., MASCLE, G. H., TARDY, M., DEMANT, A. (2007) The Mamonia Complex (SW Cyprus) revisited: remnant of Late Triassic intra-oceanic volcanism along the Tethyan southwestern passive margin. Geological Magazine, 144 (1) 1-19 doi:10.1017/s0016756806002937 | ||
| In | (2007, January) Geological Magazine Vol. 144 (1) Cambridge University Press (CUP) | ||
| Abstract/Notes | Upper Triassic volcanic and sedimentary rocks of the Mamonia Complex in southwestern Cyprus are exposed in erosional windows through the post-Cretaceous cover, where the Mamonia Complex is tectonically imbricated with the Troodos and Akamas ophiolitic suites. Most of these Upper Triassic volcanic rocks have been considered to represent remnants of Triassic oceanic crust and its associated seamounts. New Nd and Pb isotopic data show that the whole Mamonia volcanic suite exhibits features of oceanic island basalts (OIB). Four rock types have been distinguished on the basis of the petrology and chemistry of the rocks. Volcanism began with the eruption of depleted olivine tholeiites (Type 1) and oceanic island tholeiites (Type 2) associated with deep basin siliceous and/or calcareous sediments. The tholeiites were followed by highly phyric alkali basalts (Type 3) interbedded with pelagic Halobia-bearing limestones or white reefal limestones. Strongly LREE-enriched trachytes (Type 4) were emplaced during the final stage of volcanic activity. Nd and Pb isotopic ratios suggest that tholeiites and mildly alkali basalts derived from partial melting of heterogeneous enriched mantle sources. Fractional crystallization alone cannot account for the derivation of trachytes from alkaline basalts. The trachytes could have been derived from the partial melting at depth of mafic material which shares with the alkali basalts similar trace element and isotopic compositions. This is corroborated by the rather similar isotopic compositions of the alkali basalts and trachytes. The correlations observed between incompatible elements (Nb, Th) and εNd and Pb isotopic initial ratios suggest that the Mamonia suite was derived from the mixing of a depleted mantle (DMM) and an enriched component of High μ (μ = 238U/204Pb, HIMU) type. Models using both Nd and Pb isotopic initial ratios suggest that the depleted tholeiites (Type 1) derived from a DMM source contaminated by an Enriched Mantle Type 2 component (EM2), and that the oceanic tholeiites (Type 2), alkali basalts (Type 3) and trachytes (Type 4) were derived from the mixing of the enriched mantle source of the depleted tholeiites with a HIMU component. None of the Mamonia volcanic rocks show evidence of crustal contamination. The Upper Triassic within-plate volcanism likely erupted in a small southerly Neotethyan basin, located north of the Eratosthenes seamount and likely floored by oceanic crust. | ||
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