Hyperfine Interactions

, Volume 192, Issue 1–3, pp 101–107 | Cite as

Rhyolite–dacite–trachyandesite association: a Mössbauer spectroscopy study

  • K. M. HassanEmail author


Three volcanic dykes, rhyolite, dacite and trachyandesite cutting a radioactive granite, located between Latitudes 22° 47′ 396″–22° 47′ 884″ N and Longitudes 31° 54′ 883″–31° 54′ 894″ E in the south Western Desert of Egypt were sampled and analyzed by X-ray diffraction, 57Fe Mössbauer spectroscopy and chemical method. They are consisted of feldspar and quartz together with some paramagnetic minerals including aegirine plus minor riebeckite in the rhyolite; aegirine plus some riebeckite in the dacite; and riebeckite plus trace aegirine in the trachyandesite, respectively. The bulk content of iron in each dyke has characteristic ferric-quadrupole splitting and oxidation values: 0.29 millimeters per second (mm/s) and 100% for rhyolite; 0.31 mm/s and 82% for dacite; and 0.35 mm/s and 0.69% for trachyandesite. Variations in the quadrupole splitting have been attributed to changes from the local crystal chemistry, while the oxidation variations are source-related.


Volcanic dykes Aegirine Riebeckite Mössbauer Egypt 


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© Springer Science+Business Media B.V. 2009

Authors and Affiliations

  1. 1.Department of Radioactive Sedimentary DepositsNuclear Materials AuthorityCairoEgypt

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