The development of Tarim passive continental margin in Kokshaal (South Tien-Shan) through Devonian to Early Carboniferous consists of submergence episodes connected with magmatic and possible rift events or eustatic transgressions (D2?, D3f, C1t, C1v2-3) and periods of intensive sedimentation on the continental rise (D3fm1, locally C1v1-2) owing to regressions upon shelf. -English summary

Translated title of the contributionKokshaal' passive margin of Tarim continent in Middle Paleozoic
Original languageRussian
Pages (from-to)68-71
Number of pages4
JournalВЕСТНИК САНКТ-ПЕТЕРБУРГСКОГО УНИВЕРСИТЕТА. СЕРИЯ 7: ГЕОЛОГИЯ, ГЕОГРАФИЯ
Volume4
StatePublished - 1 Jan 1992

    Scopus subject areas

  • Geology
  • Earth and Planetary Sciences(all)

ID: 49959874