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Haushi Uplift OL53, Ad Dakhiliyah Governorate, Oman
| Lat/Long (Decimal) | 21.05,57.688 |
|---|---|
| Co-ordinates Derivation | stated in text |
| Mindat.org Region (for given coordinates) | Ad Dakhiliyah Governorate, Oman |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| Haushi Uplift OL51, Section 7bis | Angiolini L., Bucher H. (1999) | Khuff - 4 | Composite section built on five sections. Khuff is part of an unconformable second mega-sequence, which consists of the fluvial terrigenous Gharif Fm., overlain by marine marls and bioclastic limestones of the Khuff Fm. Top unconformably truncated by continental sandstones and siltstones of the Triassic to Jurassic Minjur Formation. | marl | 268.8 - 265.1 Ma Permian |
| Haushi Uplift OL52, Section 7bis | Angiolini L., Bucher H. (1999) | Khuff - 4 | Composite section built on five sections. Khuff is part of an unconformable second mega-sequence, which consists of the fluvial terrigenous Gharif Fm., overlain by marine marls and bioclastic limestones of the Khuff Fm. Top unconformably truncated by continental sandstones and siltstones of the Triassic to Jurassic Minjur Formation. | "limestone" | 268.8 - 265.1 Ma Permian |
| Haushi Uplift OL53, Section 7bis | Angiolini L., Bucher H. (1999) | Khuff - 4 | Composite section built on five sections. Khuff is part of an unconformable second mega-sequence, which consists of the fluvial terrigenous Gharif Fm., overlain by marine marls and bioclastic limestones of the Khuff Fm. Top unconformably truncated by continental sandstones and siltstones of the Triassic to Jurassic Minjur Formation. | "limestone" | 268.8 - 265.1 Ma Permian |
| Haushi Uplift OL57, Section 7bis | Angiolini L., Bucher H. (1999) | Khuff - 4 | Composite section built on five sections. Khuff is part of an unconformable second mega-sequence, which consists of the fluvial terrigenous Gharif Fm., overlain by marine marls and bioclastic limestones of the Khuff Fm. Top unconformably truncated by continental sandstones and siltstones of the Triassic to Jurassic Minjur Formation. | "limestone" | 268.8 - 265.1 Ma Permian |
| Haushi Uplift OL60, Section 7bis | Angiolini L., Bucher H. (1999) | Khuff - 4 | Composite section built on five sections. Khuff is part of an unconformable second mega-sequence, which consists of the fluvial terrigenous Gharif Fm., overlain by marine marls and bioclastic limestones of the Khuff Fm. Top unconformably truncated by continental sandstones and siltstones of the Triassic to Jurassic Minjur Formation. | marl | 268.8 - 265.1 Ma Permian |
Recorded Fossils
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!
