 | Dale, C.W., Gannoun, A., Burton, K.W., Argles, T.W., Parkinson, I.J. (2007) Rhenium–osmium isotope and elemental behaviour during subduction of oceanic crust and the implications for mantle recycling. Earth and Planetary Science Letters, 253 (1) 211-225 doi:10.1016/j.epsl.2006.10.029 | Journal (article/letter/editorial) | | elemental data for basalts and gabbros from the Zermatt-Saas ophiolite, metamorphosed to eclogite-facies conditions...contemporaneous basalts and gabbros from the Zermatt-Saas ophiolite, metamorphosed to eclogite-facies conditions...been collected from the Zermatt-Saas Fee ophiolite (ZSO), Switzerland (Fig. 1), which comprises structurally...Western Alps (left) and larger scale map of Zermatt-Saas ophiolite (ZSO) showing sampling areas in black... Fig. 2. N-MORB normalised spidergram for (a) Allalin gabbroic lithologies (black lines — gabbros, grey |  | | Book (edition) | | of meters, burnt rocks may crop out over a large area, especially where combusted organic-bearing strata...high-T, low-P regional metamorphism in the Qadda area, southern Arabian Shield. J Metamorph Geol 14:613–634...of coesite-bearing metasediments from the Zermatt-Saas zone, Western Alps. Eur J Miner 3:7–17 References...prehnite-pumpellyite to greenschist facies in the Danseys Pass area, Otago, New Zealand. Geo Soc Am Bull 83:3177–3198...material k. JQ is the rate of heat transfer per unit area (heat flow vector) parallel to the highest gradient |
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