| | 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...the Contact Zone in the Upper Reaches of the Bogide River Our work has been carried out in accordance | | | Journal (article/letter/editorial) | this type has been studied in detail in the Bogide River basin. Anorthositization patches a r e here...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...leucocratic metasomatites (anorthosites). Kavakta River basin) against the background of weak sign-varying | | | 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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