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NARROW
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Khudolaz Complex
Geochemistry of Accessory Apatite from the Cu–Ni–Sulfide-Bearing Ultramafic–Mafic Rocks of the Khudolaz Complex (South Urals) as a Monitor of Magmatic and Metasomatic Processes
Photomicrographs of the Khudolaz Complex rock and ore samples in which apat...
REE patterns of apatite from the ultramafic–mafic rocks of sulfide-bearing ...
Binary variation diagrams (wt.%) for apatite from the ultramafic–mafic rock...
F–Cl–OH (at.%), F–Cl, and Cl–SO 3 (wt.%) diagrams for apatite from the ult...
FeO–MgO diagram for apatite from different rock associations: Ap-1 and Ap-2...
Postmagmatic morphologic changes of apatite grains in the ultramafic–mafic ...
Examples of alteration and replacement of apatite in the metasomatized ultr...
Parageneses of apatite and silicate minerals in the unaltered ultramafic–ma...
Schematic geological map of the Khudolaz trough, after Rakhimov et al. ( 20...
Binary Y–Sr ( a ) and Mn–Sr ( b ) discrimination diagrams for apatite from ...
Interesting Papers in Other Journals
The Akhunovo–Petropavlovsk Granitoid Area as a Continental-Margin Center of the Long-Term Mantle–Crust Interaction: The Role of Subductional and Rift–Plume Sources
Zaykovite, Rh 3 Se 4 , a new mineral from the Kazan placer, South Urals, Russia
Interesting Papers in Other Journals
Biostratigraphy and lithostratigraphy of the Mid-Carboniferous boundary beds in the Muradymovo section (South Urals, Russia)
Taxonomy and Evolution of Visean–Roadian (Late Mississippian–Guadalupian) Lasiodiscidae
Russian regional Carboniferous stratigraphy
Abstract Several existing schemes for Carboniferous stratigraphy officially adopted in regions of the Russian Federation are summarized and discussed. These regions with different geological histories and distinct depositional settings include the Moscow Basin, the Urals, North Timan, Siberia, the Kuznetsk Basin and the Mongol–Okhotsk, Verkhoyansk–Okhotsk and Kolyma–Omolon regions. Broad correlations based on macro- and microfossils are possible between the regions, while all regional schemes are correlated to the official Russian General Stratigraphic Scheme for the Carboniferous, using zonations based on orthostratigraphic fossils. The Russian General Stratigraphic Scheme is correlated to the International Stratigraphic Scale using ammonoids, conodonts, foraminifers and palynomorphs.