 | | Journal (article/letter/editorial) | | Tungsten Ores of the Dzhida W-Mo Ore Field (Southwestern Transbaikalia, Russia): Mineral Composition...the Russian Academy of Sciences, 670047 Ulan-Ude, Russia; damdinov@mail.ru * Correspondence: ludamdinova@mail...Tungsten Ores of the Dzhida W-Mo Ore Field (Southwestern Transbaikalia, Russia): Mineral Composition...text) study of the Kholtoson W and Inkur W deposits located within the Dzhida W-Mo ore field (Southwestern...(Southwestern Transbaikalia, Russia). The Mo mineralization spatially coincides with the apical part of the Pervomaisky |  | | Journal (article/letter/editorial) | | is a stock, exposed in numerous drill holes and mine workings. On the eastern flank of the ore field...by [New York University] at 01:00 28 April 2015 *w Sit N s • a2 v rt CD * ^ u-i i o o 2 -aS 11..."3 h V c 1 o B _o co to a> o o o g a] fc a Q w « O 858 G.F. IVANOVA. Z.M. MOTORl.YA. AiND V.ll...contain abundant limonite, psilomelane, powellite, cerussite, anglesite, mala chite, azurite, and bismuth...from the Kholtoson huebnerite deposit formation in the Yugodzyr' deposit took place (the Dzhida ore region |  | | Book | | the Institute of Solid Fuels Preparation, Moscow, Russia Lev A. Barsky, Canadian Institute of Mining, Metallurgy...of 4.4 Physical properties of Minerals, Primary Russia Concentration 2.3 Mineral Resources of Ukraine...framework of the newly formed republics and regions of Russia. Furthermore we have found it possible and convenient... VII VIII Ni,Co As,Sb,Bi Al Nb,Ta,V Ag, Au Mo,W Pt,Os,Ir, Ru,Rh,Pd TR,Sc,Y Ga,In,Tl Rb, Cs Ra...deposits. There are ores of Fe, Cu, Co, Pb, Zn, W, Mo, Sn, Be, U, Au, Bi, rock crystal, graphite and other |  | | Book (volume) | | stratigraphy and structure of the rocks of the district, sedimentary, igneous, and metamorphic; (3) the...explain the ideas of those who have worked on it (and mine, where they differ from those readily available...a stratigraphie et la structure des roches du district (roches sédimentaires, ignées et métamorphiques);...o r a M Β Η 3 Υ ^ Θ Η Η Η pyjiHbix M e c T o p o w e H H i i . H nonbiTaJicn o x B a T H T b Β 3TOH p...B p o n e f t C K H x H3bIKaX . 06 3 Ο Ρ n o K a w o M y H a M e c T o p o ^ m e H K H B K J n c m a |  | | Book | | CX 3 C_ > > * S as X Γ CO 3 O •-I C X y-, w CU O H ...x: .—ι en CO · en en O Û X C U CO v _. o HJ M < W ^ > 1-4 < ,-J CQ <£ ci MASSES andésite, e t... ISUBIVOLCANIC >-« e 3i < ■ Λ 0 en eu •H w 1 3 _o u o a, cu J cX aJ 16 km % > DIKES ...1 / >v ^* w ^ \< K-> 0 Z —- 1Λ1 c/D 10km o ÖJO CU Τ3 4-> u cC 35 H PH w Q W M-i O a cu...pipes Chile Fig. 27-4. + + + Porphyry Cu and Mo deposits, interpreted depths of origin. Fig. 27-5 |  | | Book | | mechanical, photocopying, recording or otherwise, w i t h o u t the prior written permission of the publisher...in the USA — This publication has been registered w i t h the Copyright Clearance Center Inc. (CCC), Salem...c0 1. 1 1 c° 1 1 CL °a 1 8 km 3 U 16 km 1o W VJ 3 O en 1 3 O -H DC < ■ 1 £ cto en CU ...en "07 c (-1 QJ CO CD en CO Cß U en J < M W y ■ MEDIUM LEVEL cfl J0 C U M =C o CQ ...foliated, gneissic, migmatitic granite Pi Q < >"W PH Fig. 27-1. Depths of associated intrusives. |
|
