Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Fossil travertines and quasi-travertine in the Minusa basin (West Siberia) : structure, composition, and comparative analysis. / Fedoseev, G. S.; Vorontsov, A. A.; Orekhov, A. A.
в: Russian Geology and Geophysics, Том 58, № 8, 01.08.2017, стр. 922-934.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Fossil travertines and quasi-travertine in the Minusa basin (West Siberia)
T2 - structure, composition, and comparative analysis
AU - Fedoseev, G. S.
AU - Vorontsov, A. A.
AU - Orekhov, A. A.
PY - 2017/8/1
Y1 - 2017/8/1
N2 - We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite).
AB - We study a carbonate body looking like a classical fossil travertine which was discovered in the Chebaki-Balakhta basin within the Minusa trough (Khakassia, Russia) and called quasi-travertine. It is a thin layer sandwiched between a basalt-dolerite sill and calcareous siltstone. Comprehensive studies of the quasi-travertine and its comparison with Devonian fossil travertines located a few kilometers away in terms of structure and composition have made the basis for its formation model. According to this model, the quasi-travertine has had a two-stage history: deposition and subsequent hydrothermal metasomatism. Laminated limestone coexisting with calcareous siltstone of the Early Devonian Shunet Formation formed during the first stage and then experienced hydrothermal metasomatism with precipitation of secondary calcite, prehnite, and pyrobitumen (kerite).
KW - basalt
KW - dolerite
KW - fossil travertine
KW - Minusa basin
KW - prehnite
KW - quasi-travertine
KW - shallow sill
KW - sparite
KW - CARBONATES
KW - LATE QUATERNARY
KW - STROMATOLITES
KW - TROUGH
UR - http://www.scopus.com/inward/record.url?scp=85026896329&partnerID=8YFLogxK
U2 - 10.1016/j.rgg.2017.07.003
DO - 10.1016/j.rgg.2017.07.003
M3 - Article
AN - SCOPUS:85026896329
VL - 58
SP - 922
EP - 934
JO - Russian Geology and Geophysics
JF - Russian Geology and Geophysics
SN - 1068-7971
IS - 8
ER -
ID: 9965966