Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
2001
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| _version_ | 1867167711005507584 |
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| author | Udoratina, Oxana V |
| author_facet | Udoratina, Oxana V |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Rare-metal alkali (quartz-feldspathic) metasomatites are considered in terms of their geologic position, structure, and composition. Their petrochemical and geochemical characteristics are given. In the Polar Urals, the metasomatites occur as lenticular and tube-like bodies in the fault zones of the Cambrian basement within the Kharbey block. Three types of the metasomatites, dated at ~300 Ma, have been recognised: quartz-bifeldspathic (kvalmites), quarzt-albitic, and albitites. They belong to the formation of quartz-feldspathic metasomatites of the fault zones. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_107281 |
| institution | PANGAEA |
| language | en |
| publishDate | 2001 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals Udoratina, Oxana V Aluminium oxide; Antimony; Arsenic; Barium; Bromine; Caesium; Calcium oxide; Carbon dioxide; Cerium; Chromium; Cobalt; Dysprosium; Erbium; Europium; Fluorine; Gadolinium; Geological sample; GEOS; Gold; Hafnium; Holmium; Iron oxide, Fe2O3; Iron oxide, FeO; Lanthanum; Lithology/composition/facies; Loss on ignition; Lutetium; Magnesium oxide; Manganese oxide; Neodymium; Nickel; Phosphorus pentoxide; polar_ural; Potassium oxide; Praseodymium; Rubidium; Samarium; Sample code/label; Scandium; Selenium; Silicon dioxide; Silver; Sodium oxide; Strontium; Sulfur, total; Sum; Tantalum; Terbium; Thorium; Thulium; Titanium dioxide; Ural; Uranium; Ytterbium; Zinc; Zirconium Rare-metal alkali (quartz-feldspathic) metasomatites are considered in terms of their geologic position, structure, and composition. Their petrochemical and geochemical characteristics are given. In the Polar Urals, the metasomatites occur as lenticular and tube-like bodies in the fault zones of the Cambrian basement within the Kharbey block. Three types of the metasomatites, dated at ~300 Ma, have been recognised: quartz-bifeldspathic (kvalmites), quarzt-albitic, and albitites. They belong to the formation of quartz-feldspathic metasomatites of the fault zones. |
| title | Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals |
| topic | Aluminium oxide; Antimony; Arsenic; Barium; Bromine; Caesium; Calcium oxide; Carbon dioxide; Cerium; Chromium; Cobalt; Dysprosium; Erbium; Europium; Fluorine; Gadolinium; Geological sample; GEOS; Gold; Hafnium; Holmium; Iron oxide, Fe2O3; Iron oxide, FeO; Lanthanum; Lithology/composition/facies; Loss on ignition; Lutetium; Magnesium oxide; Manganese oxide; Neodymium; Nickel; Phosphorus pentoxide; polar_ural; Potassium oxide; Praseodymium; Rubidium; Samarium; Sample code/label; Scandium; Selenium; Silicon dioxide; Silver; Sodium oxide; Strontium; Sulfur, total; Sum; Tantalum; Terbium; Thorium; Thulium; Titanium dioxide; Ural; Uranium; Ytterbium; Zinc; Zirconium |
| url | https://doi.org/10.1594/PANGAEA.107281 |