In Oman the zone has a range top well below the Haushi limestone which contains Sterlitamakian (Late Sakmarian) fusulinids (Angiolini et al., 2006), but its lower limit cannot be assessed independently because of the lack of paleontological or other radiometric evidence at this level.

Guadalupian Paleobiogeography across the Neotethys Ocean* Lucia Angiolini1, Giovanni Muttoni1, Gaia Crippa1, and Vincenzo Verna1 Search and Discovery Article #30225 (2012) Posted February 20, 2012 *Adapted from oral presentation at AAPG International Conference and Exhibition, Milan, Italy, October 23-29, 2011

The palaeontology of the Saiwan Formation (Lower Permian) of the Al-Huqf outcrop area, Central Oman, has been the subject of significant study, but that of approximately equivalent beds in the subsurface (the Haushi limestone and 'basal sandstones' of the lower Gharif member) has been unknown until now.

Abrupt environmental and climatic change during the deposition of the Early Permian Haushi limestone, Oman more. by flavio jadoul. During the late Sakmarian (Early Permian), the Haushi limestone was deposited in a shallow embayment of the Neotethys Ocean covering what is now north Oman and parts of southeast Saudi Arabia. The sea persisted ...

correlation with Australia and India [30]. In Oman this is followed by a marked hiatus with a carbonate sequence (the Lusaba Limestone or Formation) containing an Upper Permian fauna of Tethyan warm-water character, previously thought to be part of the Lower Permian and to immediately overlie the Haushi Formation [15].

Comment on "Aptian faulting in the Haushi-Huqf (Oman) and ... limestone is not a mudstone but a coarse grainstone comprising rudist debris, i.e. a material that is non-cohesive before lithification and with no plastic rheological behavior. Moreover, the small sinuous

correlation with Australia and India [30]. In Oman this is followed by a marked hiatus with a carbonate sequence (the Lusaba Limestone or Formation) containing an Upper Permian fauna of Tethyan warm-water character, previously thought to be part of the Lower Permian and to immediately overlie the Haushi Formation [15].

During her Earth Sciences BSc at SQU, Zainab conducted a final year project for Petroleum Development Oman Company of petrographic analysis and correlation of the Haushi Limestone member (Early Permian), the upper part of the lower Gharif Formation, in North and Central Oman.

In this case the abstract is more detailed than the research highlights, and both include hyperlinks that can make a timeline or the Gharif formation of Oman's record in the Paleobiology database appear in the right sidebar. The research highlights also include an animated figure, the print from some kind of analysis I am not familiar with.

Saiwan, Gharif and Khuff formations, Haushi-Huqf Uplift, Oman 163 more silty or sandy thr ough the top 15 m (49 ft) of the formation, immediately beneath the lowest

To the east, the Haushi limestone is absent in the Oman 3 mountains due either to erosion or non-deposition related to the rise of the Hawasina 4 Basin rift shoulder in the position of the present Oman mountains in the Early 5 Permian (Blendinger et al., 1990; Osterloff et al., 2004b).

Three Total Petroleum Systems each consisting of one assessment unit have been identified in the Ghaba and Fahud Salt Basin Provinces of north-central Oman. One Total Petroleum System and corresponding assessment unit, the North Oman Huqf/`Q'? Haushi(!) Total Petroleum System (201401) and Ghaba-Makarem Combined Structural Assessment Unit (20140101), were identified for the .

More than 3.5 billion bbl of oil in place have so far been discovered in reservoirs of the Al Khlata Formation of the Permian-Carboniferous lower Haushi Group in south Oman. Glacially striated pavements and boulders in exposures at Al Khlata in east-central Oman confirmed previous interpretations ...

Three Total Petroleum Systems each consisting of one assessment unit have been identified in the Ghaba and Fahud Salt Basin Provinces of north-central Oman. One Total Petroleum System and corresponding assessment unit, the North Oman Huqf/?Q??Haushi(!) Total Petroleum System (201401) and Ghaba- Makarem Combined Structural Assessment Unit (20140101), were identified for the .

During the late Sakmarian (Early Permian), the Haushi limestone was deposited in a shallow embayment of the Neotethys Ocean covering what is now north Oman and parts of .

Abrupt environmental and climatic change during the deposition of the Early Permian Haushi limestone, Oman more. by Lucia Angiolini, fabrizio berra, and G. Gambacorta. Publication Date: 2008 ... Evolution of the Early Permian Haushi Sea of Oman and Comparison with Other Gondwanan Post-Glacial Marine Sequences more.

Haushi Group sediments At the base of the Haushi Group, the most important hiatus (Figure 2) is located within the sedimentary se- quence, reflecting the final phase of the Pan-African tectonic events, which affected Oman during most of the Upper Silurian to Lower Devonian (A1-Marjeby and Nash, 1986).

of the Arabian Peninsula for their participation in the preparation of a monograph on the geology of the Arabian Peninsula. Each author prepared a description of the geology of the area for which he was responsible, as shown in the sources of geologic compilation diagram on the peninsular map.

The palaeontology of the Saiwan Formation (Lower Permian) of the Al-Huqf outcrop area, Central Oman, has been the subject of significant study, but that of approximately equivalent beds in the subsurface (the Haushi limestone and 'basal sandstones' of the lower Gharif member) has been unknown until now.

in the Haushi-Huqf (Oman) and the tectonic evolution of the southeast Arabian platform-margin" ... Normal faulting post-lithification of the Aptian Qishn limestone Montenat et al. (2003) put forward sedimentological and tectonic observations to argue that faulting occurred prior to complete lithification of the carbonates of the Qishn Formation.

The area covered is the Oman Mountains, Southern Oman, offshore areas, and the wider tectonic context of Iran and the Indian ocean. The volume follows an International Discussion Meeting held at the Royal Society of Edinburgh, from March 29-31, 1988, convened by A. H. F. Robertson, M. P. Searle, J. D. Smewing and A. C. Ries.