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TRANSIIDI KÄSIRAAMAT - Taxation and Customs Uniontd.tisA- cp > ti!teA > ta!tea ?of an important' a~kkUrU- C/> > a~kkrU > a~kkru 'of the anchor'. elektEri- C/> > elektri > elektri ?of electricity' lii ... 4. 5. 6 Z6 Z7 Z7 - The Swiss Baysaksa keeles: «Nimi?» ' «Joachim Ribbentrop.» Ta talutatakse mööda trepi- astmeid üles võlla juurde, siis seotakse tal eririhmadega kinni jalad ja tehakse ... Isevärki inimesed - ETERA... saksa 'keelt 'You (Sg) are said to speak German'). 59. Page 59. ESTONIAN ... (-Ida-, -elda-,. -nda-, -enda-, -rda-, -erda-). The suffix -(t)ta-----da- has ... ????1,?? ?? [1]. Bye. 1,?? ?? [1]. TEAM KOMADA. B0031. ?? ?. 4,?? ??. ??JTS. Y0074. ?? ??. 1,?? ?? [1]. ??LTC. A0021. ?? ??. ????? ???????. ????. ???. ?????. ????. ?????. ????. ???. ????. 8. ????. ???. ????. 10. ????. 10. ??? ... ????? ?? ? ? ??? ?. ??. 1. ?? ?? ???. 4 NGR 12.7. ?? ?? ???. 2. DNS. ?????5?100m. ????. ?????6?100m. ????. 13.4. ?? ... The Kocaba? hominin (Denizli Basin, Turkey) at the crossroads of ...This dissertation details and contextualizes the changing nature of obsidian circulation and use in the West Mediterranean from the sixth to second millennia ... Geometric and topological recursion and invariants of the moduli ...Front cover: Obsidian artifacts from Field Museum (Feinman and Nicholas) excavations at the Mitla. Fortress and Lambityeco (Oaxaca, Mexico). Geologic map unit descriptions - USGS.govFigure 2.1 Modes of exchange from Renfrew (1975:520) showing human agents as squares, commodities as circles, exchange as an X, and boundaries as a dashed ... Obsidian Across the Americas - OAPEN LibraryThe main symbol for igneous rocks is in Italic and for metamorphic rocks it is in Quill font characters. In sedimentary rocks, in a formation ... COSMOLOGY and PARTICLES - CERN Document ServerDistribution of central Anatolian obsidian with the key sites mentioned in the text. The symbol size represents the percentage of Anatolian obsidian in the ... Specifications for the preparation of 1:10 000 scale geological mapsThe obsidian is black with fine white flow bands with a low proportion (< 1%) of plagioclase crystals. It is darker and with fewer crystals of plagioclase than ...
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