Zobrazeno 1 - 10
of 31
pro vyhledávání: '"ALAN P. HEWARD"'
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 128, Iss 3 (2022)
Permian brachiopods from Oman are well-known as valuable tools for correlation and palaeobiogeographical and palaeoclimatic reconstructions. Here, we describe a new brachiopod fauna from the Qarari Unit of the allochthonous Batain Group in northeast
Externí odkaz:
https://doaj.org/article/5d894bcb6d174887bb74eca24d4bf6e7
Publikováno v:
Proceedings of the Geologists' Association. 133:154-161
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0fb61e55283eb5b280a04df6926b65c8
https://doi.org/10.1016/j.pgeola.2022.02.005
https://doi.org/10.1016/j.pgeola.2022.02.005
Autor:
ERNST JA. LEVEN, ALAN P. HEWARD
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 119, Iss 2 (2013)
The Batain Group of the northeastern coastal plain of Oman consists of offshore and deeper water deposits that accumulated in the Batain Basin and which were subsequently obducted onto the eastern margin of Oman. The oldest deposits of the Batain Gro
Externí odkaz:
https://doaj.org/article/cc44fdd37b5046a3959d4ebfb18c5098
Publikováno v:
Geological Magazine. 156:1357-1374
The Middle Shale Member of the Amdeh Formation is interpreted to be of Early Ordovician age based on its trace fossils, stratigraphic context and a newly discovered fauna of conodonts. The member abruptly overlies the Lower Quartzite Member, which ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::00629db4b69beac3380b411a329c0629
https://doi.org/10.1017/s0016756818000729
https://doi.org/10.1017/s0016756818000729
Publikováno v:
Journal of Systematic Palaeontology. 16:571-593
Reports of Ordovician conodonts from the Arabian region of the Gondwanan margin are extremely rare. Here we provide a description of the apparatus of two new conodont genera and species, Aldridgeognathus manniki and Omanognathus daiqaensis, based on
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::924ea5cdbdbc30d824eaaa703b117901
https://doi.org/10.1080/14772019.2017.1314985
https://doi.org/10.1080/14772019.2017.1314985
The Amdeh Formation is a 3.4 km stack of sparsely fossiliferous quartzites and shales which crops out in the Al Hajar mountains near Muscat. Here we describe the uppermost member (Am5) that can be dated biostratigraphically as Darriwilian and which i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40c3953855bbac95a78f7a48d16ca842
http://hdl.handle.net/10141/622331
http://hdl.handle.net/10141/622331
Publikováno v:
ResearcherID
The Rann Formation occurs as unique ‘exotic’ rafts in front of the Semail Ophiolite in the northern Oman Mountains. Its Ordovician age has been poorly constrained and it is often associated with the Ayim rock unit, which has been considered Devon
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::346964dddb3a122a0eea12e233626432
https://doi.org/10.2113/geoarabia1604127
https://doi.org/10.2113/geoarabia1604127
Publikováno v:
Palaeontology. 54:525-533
Early and early Middle Ordovician crinoids are rare globally, and are best known from North America and the British Isles. The first Arenig crinoid from the Arabian Peninsula is Iocrinus sp. cf. I. subcrassus (Meek and Wor- then), known from two near
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d932cf0175a74176498d19c642928b6b
https://doi.org/10.1111/j.1475-4983.2011.01042.x
https://doi.org/10.1111/j.1475-4983.2011.01042.x
Publikováno v:
GeoArabia. 15:81-120
Graptolites and their associated acritarch floras and chitinozoan faunas are described from three localities in Oman and the United Arab Emirates (UAE). They are characteristic of intervals of deeper water sediments in the Floian – Dapingian (Areni
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad191a75b0e4319c3d1d100c90bbe63d
https://doi.org/10.2113/geoarabia150481
https://doi.org/10.2113/geoarabia150481
Publikováno v:
Petroleum Geoscience. 9:295-307
Rotliegend Auk Formation sandstones form the second most productive reservoir in the 30/24 fields and the major source of aquifer pressure support. In the Argyll Field, where the Zechstein oversteps beyond the Rotliegend on to Devonian continental sa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43030216e7caf37ae18f96040a5df9d5
https://doi.org/10.1144/1354-079303-578
https://doi.org/10.1144/1354-079303-578