Results 1 to 10 of about 35 (15)

Magneto-mineralogical characteristics of mafite-ultramafites of the Middle Bug River area and Holovaniv suture zone of the Ukrainian Shield (overview)

open access: diamondГеофизический журнал, 2023
Mafites and ultramafites manifest in the magnetic field as significant magnetic anomalies due to the high content of magnetite, titanomagnetite and iron-magnesium silicates. Studying the mineralogy and magnetic properties of Archean rocks formed deep in
O. Shestopalova, V. Drukarenko
doaj   +8 more sources

Mafite-ultramafites (Peridotitovy stream, Polar Urals): mineralogy, estimation of P–T-parameters of formation

open access: bronzeVestnik of Geosciences, 2021
The petrographic features and conditions of the formation of metamorphosed mafic-ultramafic rocks of the Ampelshor complex, which are part of a small massif in the southern part of the Marunke u block of the Polar Urals (Peridotitovyi stream) and are controlled by tectonic thrust faults, have been studied. Muscovite-albite-clinozoisite-amphibole rocks (
N. S. Ulyasheva   +2 more
core   +4 more sources

PETROLOGY OF SMALL BODIES FROM NICKEL-BEARING MAFITE-ULTRAMAFITES OF THE SOUTHEASTERN ALDAN-STANOVOY SHIELD

open access: bronzeTikhookeanskaya Geologiya, 2020
V.S. Prikhod’ko   +3 more
core   +3 more sources

SYN- AND EPIGENETIC NICKEL MINERALIZATION IN THE KAMCHATKA PLUTONIC MAFITE-ULTRAMAFITE FORMATIONS [PDF]

open access: diamondBulletin of Kamchatka Regional Association «Educational-Scientific Center». Earth Sciences, 2019
The paper presents data on known objects in the sulfide copper-nickel ore formation in Kamchatka, as well as other ore occurrences and points of nickel mineralization related to certain magmatic formations. The authors have revealed the empirical regularities in the distribution of the background contents of nickel, cobalt, copper, and sulfur in ore ...
R.M. Novakov
openaire   +3 more sources

Petrogeochemical characteristics of mafite-ultramafite rocks of the southern part of the Marunkeu block (Polar Urals)

open access: diamondProceedings of the Komi Science Centre of the Ural Division of the Russian Academy of Sciences, 2021
In the Polar Urals, in the Central and Western tectonic zones, small bodies of mafic-ultramafic rocks are widespread. Their age, petrographic and geochemical features are poorly studied. The paper presents the results of petrographic and petro-geochemical study of muscovite-albite-epidote-amphibole and pyroxene-amphibole-chlorite rocks of the southern ...
N.S. Ulyasheva, O.V. Udoratina
openaire   +2 more sources

Facial accessory of high-titanium magnezium-ferruginous micas as one of evaluation criteria of metamorphic and magmatic rocks rare-metall specialization

open access: yesЛитосфера, 2015
Type-chemical features of high-titanium magnezium-ferruginous micas of granulites, mafite-ultramafites, alkaline rocks, and carbonatites are considered.
A. I. Belkovsky
doaj   +3 more sources

PETROLOGY, U-Pb ISOTOPE AGE AND METAMORPHISM OF NYASHEVO POLYGENIC MAFIT-ULTRAMAFITE MASSIVE (THE SOUTHERN URALS)

open access: yesLITOSFERA, 2017
In the article is presented data of mineralogy, petrography, geochemistry and isotope-geochronology study Nyashevo mafic-ultramafic massif in Ilmeny-Vishnevogorsk polymethamorphic shear zone. The ultramafic rocks consist of serpentine and chlorite (up to 90 %), accessory and rare minerals - talc, carbonate, tremolite, cromium-magnetite, amphibole ...
Natal’ya M. Valizer   +3 more
openaire   +4 more sources

The Early Paleoproterozoic Monchegorsk layered mafite-ultramafite massif in the Kola Peninsula: Geology, petrology, and ore potential

open access: closedPetrology, 2012
The Early Paleoproterozoic Monchegorsk Complex is exposed over an area of 550 km2 and comprises two layered mafite-ultramafite intrusions of different age: the Monchegorsk pluton of ultramafic and mafic rocks and the predominantly gabbroid Main Range Massif (also referred to as the Moncha-Chuna-Volch’i Tundras Massif), which are separated by a fault ...
E. V. Sharkov, A. V. Chistyakov
openaire   +2 more sources

Home - About - Disclaimer - Privacy