Aeg relics pdf download
Discussion other minerals of the rock matrix, the thermal history of M outlined in the next section indicates that the P-T 9. Late albite could also belong to this retro- bration as a driving force for recrystallization, defining grade growth stage. The Al-rich amphiboles taramite and possible equilibrium assemblages and reaction relation- ferropargasite and associated chlorite replacing augite ships between them is difficult and in part speculative.
At relics probably represent recrystallization at the highest best, a sequence of phase growth can be outlined for each temperatures reached, suggestive of the epidote-amphibo- sample. In M the augite relics appear to represent lite facies.
No formation of any amphibole until this very domains where local equilibrium predominated. Jadeite is late stage in metamorphic development is observed in a dominant phase that replaces both augite and especially metabasite M Omphacite may in part be coeval with but definitely replaces jadeite.
Recrystallization is much more pervasive than in sample M, and TEM observations indicate that early sodic pyroxene and augite were later extensively altered to glaucophane. Minor albite, actinolite and a second generation of chlorite are clearly younger, replacing glaucophane and sodic pyroxene. Such assemblages were not encountered in this study.
Metamorphic evolution of the jadeite-bearing Schneider et al. Pyroxene reaction curves from Waterwiese metabasites et al.
These data are summarized in Fig. Maximum reported pressures for for metabasite compositions the stability field of pumpel- the various rocks vary between 15 and 25 kbar.
Maximum lyite is even more restricted. Considering of them. These lie in the stability field of jadeite in the that Al-rich amphiboles grew in M, such conditions presence of quartz Fig. Thus exhumation show that the P-T trajectories of Fig. Al-rich amphiboles conclusions to be reached for the P-T development of M found in both samples suggest that conditions of the epi- and M Jadeite-omphacite equilibration Fig.
Depending on bulk vides information on minimum temperatures reached. The trend of the P-T trajec- during the prograde or the retrograde path of the rock.
For tories in Fig. Figure 14 indicates although this conclusion cannot be unequivocally corrobo- that the intergrown pumpellyite in the matrix of sample rated from petrographic observation. Sample M equilibrated rocks were filled by jadeite-rich assemblages.
These display to a large extent in the epidote-blueschist facies before the typical features of open-system precipitation from an passing through the epidote-amphibolite and then the aqueous fluid known from well-studied jadeite jade occur- greenschist facies. Sample M shows no evidence of rences e. Cathodoluminescence until epidote-amphibolite conditions are reached.
These jadeite jade veinlets suggest calls for conditions close to the blueschist facies. Given appropriate bulk material and the enclosing rock. There are no obvious com- compositions, lawsonite-bearing assemblages are possible. Without additional information from REE spectra and trace element distributions it is not possible to decide whether the fluids were derived from a completely external source, were expelled from the rock itself at near-peak conditions, or Augite relics to jadeite jade reflects domain equilibration and enhanced of 1.
Even if the enrichment in Na2O could lead to Ophitic texture is common. Domain equilibra- tion appears to have dominated, and ophitic textures were preserved. Jadeite and minor omphacite crystallized in for- Acknowledgements: We thank H. Bernhardt and mer plagioclase laths enclosed in augite in epitactic relation- R.
Neuser, Bochum, for invaluable help with the electron ship to the host augite. Jadeite and more abundant omphacite microprobe and with hot-cathode cathodoluminescence growing from plagioclase in the rock matrix encroached microscopy, respectively.
Arne Willner gave decisive input upon augite grains from the outside. All their thoughtful reviews that helped us clarify some impor- three pyroxenes are generally in crystallographical optical tant points and improve the presentation as a whole. References 3 At increasing temperatures, more omphacite replaced earlier jadeite along grain boundaries.
Where sufficient Armbruster, T. Baese, R. Scottish Highlands. Interaction between jadeitite-forming fluids and meta- Grant, J. Green, E. Pergamon Press Inc. Baziotis, I. Earth Planet. Grevel, C. Black, P. Sociedad Geol. Carpenter, M. Carswell, ed. Harlow, G. Seitz, R. Ofioliti, 28, — Sorensen, S.
Geology, 32, 17— Evans, B. Lithos, Harlow, G. Groat, ed. Society of Canada Short Course Series, 37, — Acta, 9, — Acta, 4, 63— Hatert, F. Cretaceous collision?
Carrasquilla, S. Carpenter E. Schertl, H. Jadeitite as a monitor of subduction-zone fluids: the Rio San 1 atm. Juan Serpentinite Complex Dominican Republic. Maresch, W. Coexisting jadeite and omphacite in metabasites from the Schiffman, P. Editorial academia, Lardeaux, J. To date, the well-known and popular AEG brand stands for timeless, functional and convenient design, which continues to receive awards and prizes for example, the F-Design-Award.
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