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- W4248664314 abstract "Layers of trondhjemite occur in eclogites and high pressure amphibolites belonging to the leptyno-amphibolitic complex of Rouergue (Southern Massif Central). These trondhjemites are low in Al and depleted in K, Rb, Cs, but they have high content of other lithophile elements compared to oceanic plagiogranites and granites. Trace element data imply at least two stages in the genesis of these rocks. The textures and initial mineral assemblage (quartz, plagioclase, kyanite, zoisite, garnet) suggest that these rocks crystallized from a melt under high pressure granulite facies conditions (P ≈ 12.5 - 20 kb; T ≈ 750-840°). Solid-solid reactions, such as zoisite-Al-epidote, indicate a subsequent retrogression under conditions of the amphibolite facies.(Abbreviations for phases in text and figures: qz = quartz, pl = plagioclase, Ab = albite, ol = oligoclase, an = anorthite, ky = kyanite, sill = sillimanite, ga = garnet, stl = staurolite, zo = zoisite, al ep = Al epidote, cpx = clinopyroxene, amph = amphibole, hb = green hornblende, mus = muscovite, bi = biotite, co = corundum, sp = green spinel, rt = prismatic rutile, il = ilmenite, sph = sphene, V = H2O vapor, L = liquid.)" @default.
- W4248664314 created "2022-05-12" @default.
- W4248664314 date "1988-01-01" @default.
- W4248664314 modified "2023-10-18" @default.
- W4248664314 title "Papers published in Nuclear tracks and radiation measurements volume 14, nos. 1/2" @default.
- W4248664314 doi "https://doi.org/10.1016/0277-3791(88)90009-1" @default.
- W4248664314 hasPublicationYear "1988" @default.
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