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Lazurnaya Bay Fm , Primorsky Krai, Russia
| Lat/Long (Decimal) | 42.9167,132.333 |
|---|---|
| Co-ordinates Derivation | estimated from map |
| Mindat.org Region (for given coordinates) | Primorsky Krai, Russia |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| Lazurnaya Bay Fm (upper part) - South Primorye | Zakharov Y.D., Shigeta Y. (2000) | Lazurnaya Bay | STRATIGRAPHIC RELATIONS: Lower Triassic strata in region are lithostratigraphically divided into the Lazurnaya Bay and Zhitkov Formations in an upward sequence. The Lazurnaya Bay Fm unconformably overlies the Permian Abrek Fm. THICKNESS: The Lazurnaya Bay Fm is 57.9 m thick in the Abrek Bay region. AGE: Contains an assemblage that suggest the lower Olenekian (lower part of the Hedenstroemia bisphorensis Zone) in the upper part of the formation, overlying upper Induan age sediments. The Induan/Ol | sandstone | 251.2 - 247.2 Ma Early/Lower Triassic |
| Zhitkov Fm - South Primorye | Zakharov Y.D., Shigeta Y. (2000) | Zhitkov | STRATIGRAPHIC RELATIONS: Lower Triassic strata in region are lithostratigraphically divided into the Lazurnaya Bay and Zhitkov Formations in an upward sequence. The Zhitkov Fm overlies the lower Olenekian Lazurnaya Bay Fm. THICKNESS: The Zhitkov Fm is 87.3 m thick in the Abrek Bay region. AGE: Contains an assemblage that suggest an early Olenekian age (upper part of the Hedenstroemia bosphoremsos Zone). | siltstone | 251.2 - 247.2 Ma Early/Lower Triassic |
| Lazurnaya Bay Fm (lower part) - South Primorye | Zakharov Y.D., Shigeta Y. (2000) | Lazurnaya Bay | STRATIGRAPHIC RELATIONS: Lower Triassic strata in region are lithostratigraphically divided into the Lazurnaya Bay and Zhitkov Formations in an upward sequence. The Lazurnaya Bay Fm unconformably overlies the Permian Abrek Fm. THICKNESS: The Lazurnaya Bay Fm is 57.9 m thick in the Abrek Bay region. AGE: Contains an assemblage that suggest the upper Induan age, underlying lower Olenekian (lower part of the Hedenstroemia bisphorensis Zone) in the upper part of the formation. The Induan/Olenekian b | sandstone | 252.17 - 251.2 Ma Phanerozoic |
Recorded Fossils
References
| Zakharov Y.D., Shigeta Y. (2000) Gyronautilus, a new genus of Triassic Nautilida from South Primorye, Russia, Paleontological Research 4 4, 231-234 |
| Clapham M. E. (2015) Personal Opinions |
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
