 | | Journal (article/letter/editorial) | | THE CONTACT ZONE OF THE GERAN MASSIF, STANOVOY RANGE (and the problem of the origin of massif-type anorthosites)...THE CONTACT ZONE OF THE GERAN MASSIF, STANOVOY RANGE (and the problem of the origin of massif-type anorthosites)...THE CONTACT ZONE OF THE GERAN MASSIF, STANOVOY RANGE (and the problem of the origin of massif-type anorthosites)...rivers in the Dzhugdzhur portion of the Stanovoy range. Here, it is possible to observe undisturbed relationships...anorthosite complexes. Nevertheless, a U-Pb date on a hypersthene from the granulites of the Chogar complex (3050 |  | | Journal (article/letter/editorial) | | this type has been studied in detail in the Bogide River basin. Anorthositization patches a r e here...the comparatively homogeneous two-pyroxene and hypersthene-plagioclase schists acquire a highly inhomogeneous...massif, in the Lavla massif, in the Taas-Yurekh River basins in the eastern part of the Imangakit massif...points (middle reaches of the Dzhana River, the Dyalinka River, the Bol'shoy Chaydakh, the Yukta, the...as local elevated anomalies AT a that sometimes range up to +2500 gamma (in the 282 I.N. DAGELAYSKAYA |  | | Journal (article/letter/editorial) | | apatite-ilmenite-titanomagnetite ore shows of the Dzhugdzhur Range A. N. Solyanik To cite this article: A. N. Solyanik...apatite-ilmenite-titanomagnetite ore shows of the Dzhugdzhur Range, International Geology Review, 25:6, 681-689, DOI:...apatite-ilmenite-titanomagnetite ore shows of the Dzhugdzhur Range Downloaded by [University of Florida] at 11:11...r i n g gabbrosyenite complex of the Dzhugdzhur Range, and a l s o the study of the s t r u c t u r a...a p a t i t e , not only within the Dzhugdzhur Range, but a l s o throughout the Stanovoy zone, e s p |
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