1-18 OF 18 RESULTS FOR

Khudolaz Complex

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 December 2022
Russ. Geol. Geophys. (2022) 63 (12): 1388–1406.
...I.R. Rakhimov; I.A. Gottman; V.V. Kholodnov; V.S. Chervyakovskiy Abstract —We present results of mineralogical and geochemical studies (optical and electron microscopy, probe microanalysis, and LA-ICP-MS) of accessory apatite from the rocks of four ore-bearing massifs of the Khudolaz Complex...
FIGURES | View All (10)
Image
Published: 01 December 2022
Fig. 2. Photomicrographs of the Khudolaz Complex rock and ore samples in which apatite was studied: a – disseminated Cu–Ni sulfide ore (sample 3485), b – intensely metasomatized gabbro with sulfide dissemination (sample 3760, polished section), c – unaltered gabbro with poor sulfide
Image
Published: 01 December 2022
Fig. 7. REE patterns of apatite from the ultramafic–mafic rocks of sulfide-bearing massifs of the Khudolaz Complex: a – chondrite-normalized ( Lyubetskaya and Korenaga, 2007 ); b – host-rock normalized.
Image
Published: 01 December 2022
Fig. 8. Binary variation diagrams (wt.%) for apatite from the ultramafic–mafic rocks of sulfide-bearing massifs of the Khudolaz Complex. Arrows show the accumulation trends of major elements and halogens.
Image
Published: 01 December 2022
Fig. 6. F–Cl–OH (at.%), F–Cl, and Cl–SO 3 (wt.%) diagrams for apatite from the ultramafic–mafic rocks of sulfide-bearing massifs of the Khudolaz Complex. Ap-1 – magmatic unaltered apatite, Ap-2 – metasomatized apatite.
Image
Published: 01 December 2022
Fig. 9. FeO–MgO diagram for apatite from different rock associations: Ap-1 and Ap-2 – Khudolaz Complex (see the text for details), S – norites, gabbro-diorites, and quartz diorites of the Sudbury massif ( Warner et al., 1998 ), CK – granodiorites of Central Kazakhstan massifs ( Cao et al., 2012
Image
Published: 01 December 2022
Fig. 4. Postmagmatic morphologic changes of apatite grains in the ultramafic–mafic rocks of sulfide-bearing massifs of the Khudolaz Complex (plane-polarized light): a and b – cracked apatite crystals intergrown with phlogopite (partly chloritized) and amphibole, respectively, c and d
Image
Published: 01 December 2022
Fig. 5. Examples of alteration and replacement of apatite in the metasomatized ultramafic–mafic rocks of sulfide-bearing massifs of the Khudolaz Complex (plane-polarized light): a – resorbed apatite crystal in the argillized matrix, b – actinolite pseudomorphs after apatite in carbonatized
Image
Published: 01 December 2022
Fig. 3. Parageneses of apatite and silicate minerals in the unaltered ultramafic–mafic rocks of sulfide-bearing massifs of the Khudolaz Complex (transmitted light): a – apatite inclusions in amphibole, b – apatite crystal between plagioclase and clinopyroxene grains, c – skeleton apatite
Image
Published: 01 December 2022
Fig. 1. Schematic geological map of the Khudolaz trough, after Rakhimov et al. ( 2021 ): 1–8 — stratified volcanosedimentary deposits of: 1 – Irendyk Formation (D 2 ef 1 ), 2 – Karamalytash Formation (D 2 ef 2 ), 3 – Yarlykapovo Formation (D 2 ef 2 ), 4 – Ulutau Formation (D 2–3 zv–f
Image
Published: 01 December 2022
Fig. 10. Binary Y–Sr ( a ) and Mn–Sr ( b ) discrimination diagrams for apatite from layered sulfide-bearing complexes (dashed line): Khudolaz (Ap-1, Ap-2), Bushveld (B) ( Boudreau and Kruger, 1990 ), and Sudbury (S) ( Warner et al., 1998 ). The composition fields of apatite from different types
Journal Article
Journal: Economic Geology
Published: 01 March 2022
Economic Geology (2022) 117 (2): 511–512.
..., Southern Urals M.T. Krupenin, A.B. Kuznetsov, and G.V. Konstantinova 324 Multi-Stage Magmatic-Hydrothermal Sulfide-PGE Mineralization of the Khudolaz Complex (South Urals) I.R. Rakhimov, A.V. Vishnevskiy, and A.G. Vladimirov 341 Pre-Visean Bauxites and Iron-Aluminum Ores Deposit of the KMA and Prospects...
Journal Article
Published: 01 June 2021
Russ. Geol. Geophys. (2021) 62 (6): 648–665.
... O 5 (up to 0.54%) and correspond to the tholeiite series. These intrusions host the skarn–magnetite ores of the small Kanakai deposit. Rocks of the second type ( Faizullino complex ) have high MgO contents (up to 14 wt.%) and are enriched in LILE. Rocks of the third type, especially the Khudolaz...
FIGURES | View All (9)
Journal Article
Published: 16 November 2022
Mineralogical Magazine (2023) 87 (1): 118–129.
.... , Salikhov D.N. , Vishnevskiy A.V. and Vladimirov A.G. ( 2021a ) Multi-stage magmatic-hydrothermal sulfide-PGE mineralization of the Khudolaz complex...
FIGURES | View All (10)
Journal Article
Journal: Economic Geology
Published: 01 December 2021
Economic Geology (2021) 116 (8): 2011–2015.
..., V.V. Ratkin, and O.A. Eliseeva High sulfur solubility in subducted sediment melt under both reduced Genesis of sulfide and platinum-metal mineralization of the Khudolaz and oxidized conditions: With implications for S recycling in Complex (southern Urals) I.R. Rakhimov and V.N. Puchkov subduction zone...
Journal Article
Published: 08 October 2013
Geological Magazine (2014) 151 (2): 269–298.
... of the Khudolaz section (Stepanova & Kucheva, 2006 ) and the Neoarchaediscus regularis – Biseriella parva Zone of the Central Tien Shan (Orlov-Labkovsky et al . 2003 ). This zone correlates with the Eostaffellina paraprotvae Zone of the GSSR and E...
FIGURES | View All (14)
Journal Article
Published: 01 April 2020
Journal of Foraminiferal Research (2020) 50 (2): 141–173.
... & Jartzeva, 1956 , pl. 1, fig., 10), western continuation of the Donets basin (near Varvarovka), Starobeshevo sedimentary complex, presumed equivalents of Limestone D 5 and lower part of Formation C 1 4 in the Donets basin; 4, No. 121/361, sample 74/10, Muradymovo, Bashkirian, Bogdanovkian ( Kulagina et...
FIGURES | View All (5)
Series: Geological Society, London, Special Publications
Published: 13 April 2022
DOI: 10.1144/SP512-2021-134
EISBN: 9781786205827
.... The substage is represented by a complex of alluvial, mainly sandy sediments, filling several systems of shallow river valleys, alternating at the top with a cyclic succession predominantly of clays with four (in the most complete sequences) beds of shallow-water limestones with rich assemblages of brachiopods...
FIGURES | View All (4)