 | | 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...siderable areal extent, consisting mainly of plagioclase-rich rocks, the massif-type anortho sites [2 |  | | Journal (article/letter/editorial) | | most abundant in the Stanovoy area are pyroxene-plagioclase schists of the Kuril'ta and Dzhana series and...production of larger grains of basic and intermediate plagioclase, which form irregular patches in the rock. The...gabbro-anorthosite, or anorthosite. Fine-grained pyroxene-plagioclase schists constitute only isolated relict areas...which vein-type and banded patches of basic plagioclase are formed in a comparatively homogeneous massive... 6) Arbagas, 7) Galam, 8) Shevla. pyroxene-plagioclase schist. Anorthositization of this type has been |  | | 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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