Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals

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...

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Bibliographic Details
Main Author: Udoratina, Oxana V
Format: Dataset
Language:English
Published: PANGAEA 2001
Subjects:
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
FeO
Lanthanum
Lithology/composition/facies
Loss on ignition
Lutetium
Magnesium oxide
Manganese oxide
Neodymium
Nickel
Phosphorus oxide
polar_ural
Potassium oxide
Praseodymium
Rubidium
Samarium
Sample code/label
Scandium
Selenium
Silicon dioxide
Silver
Sodium oxide
Strontium
Sulfur
total
Sum
Tantalum
Kharbey
Polarforschung
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.107281
https://doi.org/10.1594/PANGAEA.107281
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.107281
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.107281 2023-05-15T18:02:51+02:00 Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals Udoratina, Oxana V LATITUDE: 67.300000 * LONGITUDE: 65.900000 * MINIMUM ELEVATION: 0.0 m * MAXIMUM ELEVATION: 0.0 m 2001-10-13 text/tab-separated-values, 997 data points https://doi.pangaea.de/10.1594/PANGAEA.107281 https://doi.org/10.1594/PANGAEA.107281 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.107281 https://doi.org/10.1594/PANGAEA.107281 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Udoratina, Oxana V (2001): Alkali-Metasomatites from the Polar Urals. Polarforschung, 69, 143-148, hdl:10013/epic.29837.d001 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 FeO Lanthanum Lithology/composition/facies Loss on ignition Lutetium Magnesium oxide Manganese oxide Neodymium Nickel Phosphorus oxide polar_ural Potassium oxide Praseodymium Rubidium Samarium Sample code/label Scandium Selenium Silicon dioxide Silver Sodium oxide Strontium Sulfur total Sum Tantalum Dataset 2001 ftpangaea https://doi.org/10.1594/PANGAEA.107281 2023-01-20T07:39:37Z 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. Dataset Polarforschung PANGAEA - Data Publisher for Earth & Environmental Science Kharbey ENVELOPE(67.500,67.500,66.700,66.700) ENVELOPE(65.900000,65.900000,67.300000,67.300000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
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
FeO
Lanthanum
Lithology/composition/facies
Loss on ignition
Lutetium
Magnesium oxide
Manganese oxide
Neodymium
Nickel
Phosphorus oxide
polar_ural
Potassium oxide
Praseodymium
Rubidium
Samarium
Sample code/label
Scandium
Selenium
Silicon dioxide
Silver
Sodium oxide
Strontium
Sulfur
total
Sum
Tantalum
spellingShingle 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
FeO
Lanthanum
Lithology/composition/facies
Loss on ignition
Lutetium
Magnesium oxide
Manganese oxide
Neodymium
Nickel
Phosphorus oxide
polar_ural
Potassium oxide
Praseodymium
Rubidium
Samarium
Sample code/label
Scandium
Selenium
Silicon dioxide
Silver
Sodium oxide
Strontium
Sulfur
total
Sum
Tantalum
Udoratina, Oxana V
Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals
topic_facet 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
FeO
Lanthanum
Lithology/composition/facies
Loss on ignition
Lutetium
Magnesium oxide
Manganese oxide
Neodymium
Nickel
Phosphorus oxide
polar_ural
Potassium oxide
Praseodymium
Rubidium
Samarium
Sample code/label
Scandium
Selenium
Silicon dioxide
Silver
Sodium oxide
Strontium
Sulfur
total
Sum
Tantalum
description 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
author Udoratina, Oxana V
author_facet Udoratina, Oxana V
author_sort Udoratina, Oxana V
title Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals
title_short Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals
title_full Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals
title_fullStr Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals
title_full_unstemmed Tab. 2: Geochemical composition of metasomatites and parent rocks from the Polar Urals
title_sort tab. 2: geochemical composition of metasomatites and parent rocks from the polar urals
publisher PANGAEA
publishDate 2001
url https://doi.pangaea.de/10.1594/PANGAEA.107281
https://doi.org/10.1594/PANGAEA.107281
op_coverage LATITUDE: 67.300000 * LONGITUDE: 65.900000 * MINIMUM ELEVATION: 0.0 m * MAXIMUM ELEVATION: 0.0 m
long_lat ENVELOPE(67.500,67.500,66.700,66.700)
ENVELOPE(65.900000,65.900000,67.300000,67.300000)
geographic Kharbey
geographic_facet Kharbey
genre Polarforschung
genre_facet Polarforschung
op_source Supplement to: Udoratina, Oxana V (2001): Alkali-Metasomatites from the Polar Urals. Polarforschung, 69, 143-148, hdl:10013/epic.29837.d001
op_relation https://doi.pangaea.de/10.1594/PANGAEA.107281
https://doi.org/10.1594/PANGAEA.107281
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.107281
_version_ 1766173520465756160

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