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Boro-Nuruu , Govi-Altai Province, Mongolia
Mindat.org Locality Page | Govi-Altai Province, Mongolia |
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Lat/Long (Decimal) | 46.3,93.8 |
Co-ordinates Derivation | based on political unit |
Given Location | Govi-Altai, Mongolia |
Mindat.org Region (for given coordinates) | Govi-Altai Province, Mongolia |
Collections
Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
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Boro-Nuruu (Outcrop 239/3) | Popov Y. (1986) | Gurvan-Eren | The deposits are divided into three strata: 1) pribortovyh psephites of red, 2) the thickness of yellow sandstone, 3) cyclic fine-clastic strata and mostly gray-colored thin-bedded deposits, and 4) interbedded sandstone and yellow predominantly red-brown siltstone. The first sequence consists of brown konglomeratobrekchy the size of debris 3-30 cm, cement yellow-brown calcareous sandstone. Exposed only to the upper part of the column capacity of more than 50 meters further lies interbedde | "shale" | 125 - 113 Ma Early/Lower Cretaceous |
Boro-Nuruu (Outcrop 239/5) | Popov Y. (1986) | Gurvan-Eren | The deposits are divided into three strata: 1) pribortovyh psephites of red, 2) the thickness of yellow sandstone, 3) cyclic fine-clastic strata and mostly gray-colored thin-bedded deposits, and 4) interbedded sandstone and yellow predominantly red-brown siltstone. The first sequence consists of brown konglomeratobrekchy the size of debris 3-30 cm, cement yellow-brown calcareous sandstone. Exposed only to the upper part of the column capacity of more than 50 meters further lies interbedde | "shale" | 125 - 113 Ma Early/Lower Cretaceous |
Boro-Nuruu (Outcrop 239/7) | Popov Y. (1986) | Gurvan-Eren | The deposits are divided into three strata: 1) pribortovyh psephites of red, 2) the thickness of yellow sandstone, 3) cyclic fine-clastic strata and mostly gray-colored thin-bedded deposits, and 4) interbedded sandstone and yellow predominantly red-brown siltstone. The first sequence consists of brown konglomeratobrekchy the size of debris 3-30 cm, cement yellow-brown calcareous sandstone. Exposed only to the upper part of the column capacity of more than 50 meters further lies interbedde | "shale" | 125 - 113 Ma Early/Lower Cretaceous |
Recorded Fossils
Accepted Name | Hierarchy | Age |
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Pachyrhyphus jakovlevi species | Animalia : Arthropoda : Insecta : Diptera : Anisopodidae : Pachyrhyphus : Pachyrhyphus jakovlevi | 125 - 113 Ma Early/Lower Cretaceous |
Corixalia gutta species | Animalia : Arthropoda : Insecta : Hemiptera : Corixidae : Corixalia : Corixalia gutta | 125 - 113 Ma Early/Lower Cretaceous |
Corixonecta hosbayari species | Animalia : Arthropoda : Insecta : Hemiptera : Corixidae : Corixonecta : Corixonecta hosbayari | 125 - 113 Ma Early/Lower Cretaceous |
Cristocorixa gurvanica species | Animalia : Arthropoda : Insecta : Hemiptera : Corixidae : Cristocorixa : Cristocorixa gurvanica | 125 - 113 Ma Early/Lower Cretaceous |
Stichopterus popovi species | Animalia : Chordata : Actinopteri : Acipenseriformes : Peipiaosteidae : Stichopterus : Stichopterus popovi | 125 - 113 Ma Early/Lower Cretaceous |
References
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!