Research output: Contribution to journal › Article › peer-review
Региональная геологическая позиция карбонат-фтанитовых отложений богамбирской свиты (верхний докембрий, хребет Северный Нуратау, Узбекистан). / Porshnyakov, G. S.; Fidaev, D.; Biske, Y. S.
In: ВЕСТНИК ЛЕНИНГРАДСКОГО УНИВЕРСИТЕТА. СЕРИЯ: ГЕОЛОГИЯ И ГЕОГРАФИЯ, Vol. 7, No. 4, 01.12.1998, p. 56-59.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Региональная геологическая позиция карбонат-фтанитовых отложений богамбирской свиты (верхний докембрий, хребет Северный Нуратау, Узбекистан)
AU - Porshnyakov, G. S.
AU - Fidaev, D.
AU - Biske, Y. S.
PY - 1998/12/1
Y1 - 1998/12/1
N2 - Carbonate-phtanite sediments of Bogambir suite (Uppermost Precambrian, Northern Nuratau Mountains, Uzbekistan) are to be discriminated from Ordovician and Silurian in the imbricated Variscian structure of Bogambir range. The phtanites show partly late metasomatic origin. Bogambir suite together with synchronous and similar black cherts and carbonates of Kyzylkum, Tamerlan Gates etc. presents the early rift phtanite formation in Tien-Shan. Posterior phtanite sedimentation in Cambrian-Early Silurian emerged locally.
AB - Carbonate-phtanite sediments of Bogambir suite (Uppermost Precambrian, Northern Nuratau Mountains, Uzbekistan) are to be discriminated from Ordovician and Silurian in the imbricated Variscian structure of Bogambir range. The phtanites show partly late metasomatic origin. Bogambir suite together with synchronous and similar black cherts and carbonates of Kyzylkum, Tamerlan Gates etc. presents the early rift phtanite formation in Tien-Shan. Posterior phtanite sedimentation in Cambrian-Early Silurian emerged locally.
UR - http://www.scopus.com/inward/record.url?scp=0032232622&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:0032232622
VL - 7
SP - 56
EP - 59
JO - Вестник Санкт-Петербургского университета. Науки о Земле
JF - Вестник Санкт-Петербургского университета. Науки о Земле
SN - 1812-9323
IS - 4
ER -
ID: 49957271