 | | 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 |  | | Report (issue) | | t a t i on: We r ne r , A. B. T. ,Si nc l a i r , W. D. ,a ndAme y ,E. B. ,2014,I nt e r na t i ona ls...(NRCan), Minerals and Metals Sector (MMS) (retired); W. David Sinclair, NRCan, Geological Survey of Canada...Olley, Australian Geological Survey Organisation; W. David Sinclair and A. Pasitschniak, NRCan/GSC; and...category ........ Estimated cumulative and annual mine production of tungsten contained in ore and concentrate—...For each country having a tungsten deposit or district listed in the ISMI tungsten inventory........ |  | | Book (volume) | | Blagodatnensk, Bodaibo Amur, Urals Primor'e River Basin, 4334/7900 5114/10931 5200/11500 5110/11640 6542/13450...Urals 5140/11400 Transbaikalia Buryat Middle Kholtoson, Bukuka, Eastern Transbaikalia Burgochan, 6743/17856...Khingan-Olonoi, Bugdainsk, Eastern Transbaikalia Dzhida, 4420/13200 Alatau, Bom-Gorkhon, Western Transbaikalia...Lovozero, Kola region Peninsula Kazakhstan Malo-Kholtoson, ASSR Obl, Northern Kuranakh, Maikain, Urals... depth 63 64 crusts deposit 64 (64) 67 basin placers Kuznetsov of and R.V. (Lena Region) |  | | 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. |
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