The Ore Potential of the Late Mesozoic Ariadnensky Massif of Ultramafic, Mafic, and Granitoid Rocks (Sikhote-Alin Orogenic Belt).

Saved in:
Bibliographic Details
Title: The Ore Potential of the Late Mesozoic Ariadnensky Massif of Ultramafic, Mafic, and Granitoid Rocks (Sikhote-Alin Orogenic Belt).
Authors: Khanchuk, A. I.1 (AUTHOR), Molchanov, V. P.1 (AUTHOR) vpol@mail.ru
Source: Russian Journal of Pacific Geology. Dec2023, Vol. 17 Issue 6, p517-530. 14p.
Subject Terms: *Copper, *Mesozoic Era, *Ultrabasic rocks, *Ores, *Mafic rocks, *Orogenic belts
Geographic Terms: East Asia
Abstract: In the south of the Russian Far East, a new promising type of source of strategic and critically important metals (titanium, gold, platinum, niobium, hafnium, copper, antimony, etc.) has been discovered: these are complex ores and placers that are spatially and genetically related to the Late Mesozoic (Cenomanian?) synorogenic intrusions of ultramafic–mafic rocks of the Sikhote-Alin orogenic belt. One example is the Ariadnensky massif of ultramafic, mafic and granitoid rocks with gold-titanium mineralization in its mafic part, gold-antimony mineralization at the exocontact, and gold-copper mineralization in the circum-intrusive zone. The main mineralogical and geochemical features of these ore formations have been determined. The typomorphic properties of native gold from ultramafic rocks have been revealed. It is shown that mantle and crustal processes were involved in the formation of different types of ore. The materials we obtained provide new opportunities for the reassessment of potential of strategic metal resources in Primorye. [ABSTRACT FROM AUTHOR]
Database: Energy & Power Source
Full text is not displayed to guests.
FullText Links:
  – Type: pdflink
Text:
  Availability: 1
Header DbId: enr
DbLabel: Energy & Power Source
An: 175137659
AccessLevel: 6
PubType: Academic Journal
PubTypeId: academicJournal
PreciseRelevancyScore: 0
IllustrationInfo
Items – Name: Title
  Label: Title
  Group: Ti
  Data: The Ore Potential of the Late Mesozoic Ariadnensky Massif of Ultramafic, Mafic, and Granitoid Rocks (Sikhote-Alin Orogenic Belt).
– Name: Author
  Label: Authors
  Group: Au
  Data: <searchLink fieldCode="AR" term="%22Khanchuk%2C+A%2E+I%2E%22">Khanchuk, A. I.</searchLink><relatesTo>1</relatesTo> (AUTHOR)<br /><searchLink fieldCode="AR" term="%22Molchanov%2C+V%2E+P%2E%22">Molchanov, V. P.</searchLink><relatesTo>1</relatesTo> (AUTHOR)<i> vpol@mail.ru</i>
– Name: TitleSource
  Label: Source
  Group: Src
  Data: <searchLink fieldCode="JN" term="%22Russian+Journal+of+Pacific+Geology%22">Russian Journal of Pacific Geology</searchLink>. Dec2023, Vol. 17 Issue 6, p517-530. 14p.
– Name: Subject
  Label: Subject Terms
  Group: Su
  Data: *<searchLink fieldCode="DE" term="%22Copper%22">Copper</searchLink><br />*<searchLink fieldCode="DE" term="%22Mesozoic+Era%22">Mesozoic Era</searchLink><br />*<searchLink fieldCode="DE" term="%22Ultrabasic+rocks%22">Ultrabasic rocks</searchLink><br />*<searchLink fieldCode="DE" term="%22Ores%22">Ores</searchLink><br />*<searchLink fieldCode="DE" term="%22Mafic+rocks%22">Mafic rocks</searchLink><br />*<searchLink fieldCode="DE" term="%22Orogenic+belts%22">Orogenic belts</searchLink>
– Name: SubjectGeographic
  Label: Geographic Terms
  Group: Su
  Data: <searchLink fieldCode="DE" term="%22East+Asia%22">East Asia</searchLink>
– Name: Abstract
  Label: Abstract
  Group: Ab
  Data: In the south of the Russian Far East, a new promising type of source of strategic and critically important metals (titanium, gold, platinum, niobium, hafnium, copper, antimony, etc.) has been discovered: these are complex ores and placers that are spatially and genetically related to the Late Mesozoic (Cenomanian?) synorogenic intrusions of ultramafic–mafic rocks of the Sikhote-Alin orogenic belt. One example is the Ariadnensky massif of ultramafic, mafic and granitoid rocks with gold-titanium mineralization in its mafic part, gold-antimony mineralization at the exocontact, and gold-copper mineralization in the circum-intrusive zone. The main mineralogical and geochemical features of these ore formations have been determined. The typomorphic properties of native gold from ultramafic rocks have been revealed. It is shown that mantle and crustal processes were involved in the formation of different types of ore. The materials we obtained provide new opportunities for the reassessment of potential of strategic metal resources in Primorye. [ABSTRACT FROM AUTHOR]
PLink https://search.ebscohost.com/login.aspx?direct=true&site=eds-live&db=enr&AN=175137659
RecordInfo BibRecord:
  BibEntity:
    Identifiers:
      – Type: doi
        Value: 10.1134/S1819714023060052
    Languages:
      – Code: eng
        Text: English
    PhysicalDescription:
      Pagination:
        PageCount: 14
        StartPage: 517
    Subjects:
      – SubjectFull: Copper
        Type: general
      – SubjectFull: Mesozoic Era
        Type: general
      – SubjectFull: Ultrabasic rocks
        Type: general
      – SubjectFull: Ores
        Type: general
      – SubjectFull: Mafic rocks
        Type: general
      – SubjectFull: Orogenic belts
        Type: general
      – SubjectFull: East Asia
        Type: general
    Titles:
      – TitleFull: The Ore Potential of the Late Mesozoic Ariadnensky Massif of Ultramafic, Mafic, and Granitoid Rocks (Sikhote-Alin Orogenic Belt).
        Type: main
  BibRelationships:
    HasContributorRelationships:
      – PersonEntity:
          Name:
            NameFull: Khanchuk, A. I.
      – PersonEntity:
          Name:
            NameFull: Molchanov, V. P.
    IsPartOfRelationships:
      – BibEntity:
          Dates:
            – D: 01
              M: 12
              Text: Dec2023
              Type: published
              Y: 2023
          Identifiers:
            – Type: issn-print
              Value: 18197140
          Numbering:
            – Type: volume
              Value: 17
            – Type: issue
              Value: 6
          Titles:
            – TitleFull: Russian Journal of Pacific Geology
              Type: main
ResultId 1