Geochemistry data from the Toupugol volcanogenic complex

A large fragment of a paleovolcano of Silurian to Early Devonian age was discovered in the Voikar volcanic belt suggesting an ensimatic island are as its geodynamic environment. Formationally, the rocks under study are comparable to Pleistocene island arc volcanites and their paleo-analogues. The vo...

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Bibliographic Details
Main Authors: Silaev, Valeriy I, Sokerin, Mikhail Yu
Format: Dataset
Language:English
Published: PANGAEA 2001
Subjects:
Geological sample
GEOS
Paleovolcano
Toupugol
Polarforschung
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.728534
https://doi.org/10.1594/PANGAEA.728534
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.728534
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.728534 2023-05-15T18:02:52+02:00 Geochemistry data from the Toupugol volcanogenic complex Silaev, Valeriy I Sokerin, Mikhail Yu LATITUDE: 66.916000 * LONGITUDE: 66.450000 2001-10-13 application/zip, 3 datasets https://doi.pangaea.de/10.1594/PANGAEA.728534 https://doi.org/10.1594/PANGAEA.728534 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.728534 https://doi.org/10.1594/PANGAEA.728534 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Silaev, Valeriy I; Sokerin, Mikhail Yu (2001): Indications of an Ensimatic Island Arc of the Silurian-Early Devonian Paleo-Ocean in the Polar Urals. Polarforschung, 69, 137-141, hdl:10013/epic.29836.d001 Geological sample GEOS Paleovolcano Toupugol Dataset 2001 ftpangaea https://doi.org/10.1594/PANGAEA.728534 2023-01-20T07:31:33Z A large fragment of a paleovolcano of Silurian to Early Devonian age was discovered in the Voikar volcanic belt suggesting an ensimatic island are as its geodynamic environment. Formationally, the rocks under study are comparable to Pleistocene island arc volcanites and their paleo-analogues. The volcanites of the Toupugol complex underwent strong hydrothermal-metasomatic alteration: propylites, acid metasomatic rocks and quartz-carbonate veins, which must have resulted from hydrothermal-metasomatic alteration of andesitoids. Both volcanites and apovolcanic hydrothermal rocks in Toupugol were found to host noble metal mineralisation. It is found in close association with sulphides, particularly pyrite. Free gold was discovered in all investigated volcanites and hydrothermal rocks and is characterised by low mercury content and an unusual set of microimpurities (Pt, Pd, Cu, Fe, S) suggesting its links to the mantle substrate. Dataset Polarforschung PANGAEA - Data Publisher for Earth & Environmental Science Toupugol ENVELOPE(66.705,66.705,66.699,66.699) ENVELOPE(66.450000,66.450000,66.916000,66.916000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Geological sample
GEOS
Paleovolcano
Toupugol
spellingShingle Geological sample
GEOS
Paleovolcano
Toupugol
Silaev, Valeriy I
Sokerin, Mikhail Yu
Geochemistry data from the Toupugol volcanogenic complex
topic_facet Geological sample
GEOS
Paleovolcano
Toupugol
description A large fragment of a paleovolcano of Silurian to Early Devonian age was discovered in the Voikar volcanic belt suggesting an ensimatic island are as its geodynamic environment. Formationally, the rocks under study are comparable to Pleistocene island arc volcanites and their paleo-analogues. The volcanites of the Toupugol complex underwent strong hydrothermal-metasomatic alteration: propylites, acid metasomatic rocks and quartz-carbonate veins, which must have resulted from hydrothermal-metasomatic alteration of andesitoids. Both volcanites and apovolcanic hydrothermal rocks in Toupugol were found to host noble metal mineralisation. It is found in close association with sulphides, particularly pyrite. Free gold was discovered in all investigated volcanites and hydrothermal rocks and is characterised by low mercury content and an unusual set of microimpurities (Pt, Pd, Cu, Fe, S) suggesting its links to the mantle substrate.
format Dataset
author Silaev, Valeriy I
Sokerin, Mikhail Yu
author_facet Silaev, Valeriy I
Sokerin, Mikhail Yu
author_sort Silaev, Valeriy I
title Geochemistry data from the Toupugol volcanogenic complex
title_short Geochemistry data from the Toupugol volcanogenic complex
title_full Geochemistry data from the Toupugol volcanogenic complex
title_fullStr Geochemistry data from the Toupugol volcanogenic complex
title_full_unstemmed Geochemistry data from the Toupugol volcanogenic complex
title_sort geochemistry data from the toupugol volcanogenic complex
publisher PANGAEA
publishDate 2001
url https://doi.pangaea.de/10.1594/PANGAEA.728534
https://doi.org/10.1594/PANGAEA.728534
op_coverage LATITUDE: 66.916000 * LONGITUDE: 66.450000
long_lat ENVELOPE(66.705,66.705,66.699,66.699)
ENVELOPE(66.450000,66.450000,66.916000,66.916000)
geographic Toupugol
geographic_facet Toupugol
genre Polarforschung
genre_facet Polarforschung
op_source Supplement to: Silaev, Valeriy I; Sokerin, Mikhail Yu (2001): Indications of an Ensimatic Island Arc of the Silurian-Early Devonian Paleo-Ocean in the Polar Urals. Polarforschung, 69, 137-141, hdl:10013/epic.29836.d001
op_relation https://doi.pangaea.de/10.1594/PANGAEA.728534
https://doi.org/10.1594/PANGAEA.728534
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.728534
_version_ 1766173555922305024

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