Permian-Triassic magmatism and Ag-Sb mineralization in southeastern Altai and northwestern Mongolia

G. G. Pavlova*, A. S. Borisenko, V. A. Goverdovskii, A. V. Travin, I. A. Zhukova, I. G. Tret'yakova

*Corresponding author for this work

Research output: Contribution to journalArticle

27 Citations (Scopus)

Abstract

In the 1980s, Ag-Sb deposits were discovered in a new ore cluster of the Delyun-Yustyd back-arc rift basin in southeastern Altai and northwestern Mongolia. The Delyun-Yustyd basin is filled with up to 9 km thick Devonian volcanosedimentary and terrigenous rocks lying over Vendian-Cambrian carbonate-terrigenous strata. Volcanosedimentary rocks are intruded by D3-C1 granites of the Yustyd complex, as well as by pre-granite mafic rocks, post-granite gabbro-diabase, diabase porphyry dikes, and younger lamprophyre dikes of the Chuya complex (245-236 Ma Ar-Ar biotite age). Ag-Sb ores in the Yustyd cluster formed at the Early Mesozoic stage at 240±1.6 Ma (Early-Middle Triassic boundary) and were thus nearly coeval with the Chuya lamprophyre intrusion. The age of Cu-Ag-Sb-Hg mineralization is about 234.4±1.0 Ma (Ar-Ar, sericite). Sb-Hg mineralization is the latest in the province (231.5±1.0 Ma, Ar-Ar, sericite). Gradual change of Ag-Sb (siderite-tetrahedrite) ores to complex Cu-Ag-Sb-Hg (Hg-Ag-tetrahedrite) and Sb-Hg (cinnabar with Sb sulfosalts and stibnite) mineralization along the Kurai-Kobdo and Terekta-Tolbonur large faults is interpreted as development of stage metallogenic zoning along major ore-controlling faults.

Original languageEnglish
Pages (from-to)545-555
Number of pages11
JournalRussian Geology and Geophysics
Volume49
Issue number7
DOIs
Publication statusPublished - Jul 2008
Externally publishedYes

Keywords

  • Ag-Sb deposits
  • age of mineralization
  • Altai
  • lamprophyre dikes
  • mineralization zoning
  • Mongolia

Fingerprint Dive into the research topics of 'Permian-Triassic magmatism and Ag-Sb mineralization in southeastern Altai and northwestern Mongolia'. Together they form a unique fingerprint.

Cite this