| Инд. авторы: | Smelov A.P., Shatsky V.S., Ragozin A.L., Reutskii V.N., Molotkov A.E. |
| Заглавие: | Diamondiferous Archean rocks of the Olondo greenstone belt (western Aldan-Stanovoy shield) |
| Библ. ссылка: | Smelov A.P., Shatsky V.S., Ragozin A.L., Reutskii V.N., Molotkov A.E. Diamondiferous Archean rocks of the Olondo greenstone belt (western Aldan-Stanovoy shield) // Russian Geology and Geophysics. - 2012. - Vol.53. - Iss. 10. - P.1012-1022. - ISSN 1068-7971. - EISSN 1878-030X. |
| Внешние системы: | DOI: 10.1016/j.rgg.2012.08.005; SCOPUS: 2-s2.0-84866746234; |
| Реферат: | eng: Diamond from metaultramafic rocks of the Mesoarchean (2.96-3.0 Ga) Olondo greenstone belt, located in the western Aldan-Stanovoy shield, has been studied. Diamonds occur in lenses of olivine-serpentine-talc rocks within metaultramafic rocks of intrusive habit, whose composition corresponds to peridotite komatiites. All diamonds from the metaultramafic rocks are crystal fragments 0.3 to 0.5 mm in size. Morphological examination has revealed laminar octahedra, their transitional forms to dodecahedroids, crystals with polycentric faces, and spinel twins. The crystals vary in photoluminescence color: dark blue, green, yellow, red, or albescent. Characteristic absorption bands in crystals point to nitrogen impurities in the form of A and B1 defects and tabular B2 defects. The crystals studied belong to the IaA/B type, common among natural diamonds. The overall nitrogen content varies from <100 to 3800 ppm. The relative content of nitrogen in B1 centers varies from 0 to 94%, pointing to long stay in the mantle. The carbon isotope ratio in the diamonds, 13C = -26‰, is indicative of involvement of subducted crust matter in diamond formation in the Archean. © 2012.
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| Ключевые слова: | Komatiites; Archean; carbon isotope ratio; crystal structure; diamond; greenstone belt; komatiite; olivine; serpentine; talc; Aldan Shield; Russian Federation; Sakha; Stanovoy Range; Siberian Platform; Diamond; Archean; Greenstone belt; Aldan-Stanovoy shield; |
| Издано: | 2012 |
| Физ. характеристика: | с.1012-1022 |