Across the United Kingdom, there is substantial evidence of our geological past from different time periods displaying their formations, structures and fossil content, able to provide information on past climates and biodiversity in our environments. One key region of the UK displaying various geological features is the Peak District to the north of …
— The Carboniferous Limestone Series of West Cumberland - Volume 59 Issue 2. 12th August 2024: digital purchasing is currently unavailable on Cambridge Core. Due to recent technical disruption affecting our publishing operation, we are experiencing some delays to publication. We are working hard to restore services as soon as possible and ...
Outcrop of the Dinantian and Namurian rocks in the region. (P948961) Comparative vertical sections of the Carboniferous Limestone in the Avon Gorge area, Bristol and at Burrington Combe, Mendip Hills to illustrate the relationship between the lithostratigraphical and chronostratigraphical classifications of the rocks. (P948962) North–south sections …
— Carboniferous Limestone - Volume 4 Issue 12. To save this article to your Kindle, first ensure coreplatform@cambridge is added to your Approved Personal Document E-mail List under your Personal Document Settings on the Manage Your Content and Devices page of your Amazon account.
— The Lower Khuff Member (up to 325 m, 1,066 ft thick) is interpreted as three depositional sequences (DS P17-19) that are Wordian and younger in age. DS P19 contains the Khuff Marker Limestone (KML) that is interpreted as Maximum Flooding Interval MFI P19; it provides a semi-regional datum in the red bed-dominated Lower …
— The Khuff Formation of the Akhdar Group reaches a maximum thickness of 1,110 m (3,641 ft) in northern Oman, where it is dominated by carbonates with very little …
— The glaciogenic Al Khlata Formation (Late Carboniferous – Early Permian) contains important reservoir and seal intervals in oil fields in southern Oman. Here we …
— The limestones and dolomites of the Ruhaiya Formation in southeast Saudi Arabia represent the cap carbonate facies and correlates with the Haushi Limestone of …
cludes a dating older than latest Carboniferous. A bioclastic limestone interval conformably overlying the sequence contain ... fore, the Permo-Carboniferous glaciation in Oman could serve
— The Carboniferous Yanghugou Formation in the western margin of the Ordos Basin exhibits significant potential for oil and gas exploration. However, due to the influence of complex tectonic activities, …
— The Dales as they are today were primarily formed by glaciation and the natural weathering of the carboniferous limestone that characterises much of the area. The limestone itself is a sedimentary rock and it was formed during the Carboniferous Period around 340 million years ago. The Yorkshire Dales at that time were to be found …
— In the UK, the Carboniferous Limestone is proven as a productive aquifer, hosting the circulation of deep hydrothermal fluids responsible for the thermal springs in Bath (Figure 3), Bristol, the Taff Valley and Buxton. The advantage of the Carboniferous Limestone as a resource is that it covers large areas of the UK subsurface and coincides ...
— The Upper Carboniferous-Early Permian Haushi Group is equivalent to the Arabian Plate Megasequence 5 (AP5) and comprises Al-Khlata and Gharif Formations. …
The lowermost and hence oldest rocks from the Carboniferous period are the Carboniferous Limestones which form a 1-3km wide belt of country running from west to east across the southern slopes of the Black …
— Carboniferous Period - Fossils, Coal, Shallow Seas: The Mississippian is characterized by shallow-water limestones deposited on broad shelves occupying most continental interiors, particularly in the Northern Hemisphere. Turbidite facies, deep-water sandstones, and shales deposited as submarine fans by ocean floor currents formed in …
Carboniferous Limestone outcrop in southwest Britain and stratigraphic cross-section showing major lithofacies types (A) South Dyfed; (B) Gower and Vale of Glamorgan (west of Cardiff); (C) northern limb, northeast of Merthyr Tydfil. The Lower Limestone Shale Group (Stage I) represents a 'start-up' phase. The Ivorian to Arundian period (Stage II ...
— The Permo-Carboniferous (Latest Visean-Latest Sakmarian) Gondwana continental glaciation is known from the outcrops of Oman, Yemen and Southern Saudi Arabia and in the subsurface of Central …
— Following late Precambrian rifting that formed salt basins in Oman and the Arabian Gulf region, the Cambrian-Devonian sequences were deposited on a …
— West Central Oman is a relatively underexplored area where the hydrocarbons found to date occur mainly within the Early-Late Permian Gharif Formation. Structural definition of the low relief closures is hampered by seismic velocity variations caused by dune terrain. Recent exploration activity resulted in several Gharif …
— Carboniferous Period - Rocks, Climate, Life: The Carboniferous System is divided into two subsystems—the Mississippian and Pennsylvanian—and seven depositional stages that also correspond to time units (ages) of the same names. The Mississippian Subsystem is made up of the Tournaisian (deposited 358.9 to 346.7 …
Carboniferous Limestone is a collective term for the succession of limestones occurring widely throughout Great Britain, Ireland, France and Belgium that were deposited during the Dinantian Epoch of the Carboniferous Period.These rocks formed between 363 and 325 million years ago. Within England and Wales, the entire limestone succession, which …
— This work presents an overview of the surface and subsurface carbon capture and storage (CCS) opportunities, and their associated risks, in Oman. Oman's …
— Brosse M, Bucher H, Baud A, Frisk ÅM, Goudemand N, Hagdorn H, Nützel A, Ware D, Hautmann M (2019) New data from Oman indicate benthic high biomass productivity coupled with low taxonomic diversity in the aftermath of the Permian–Triassic Boundary mass extinction. ... (1979) Paleomagnetic studies of the early Carboniferous …
— The arthropleurid trackway Diplichnites cuithensis has previously been described from Scotland from the Upper Carboniferous Serpukhovian Limestone Coal Formation on the Isle of Arran and the Lower Carboniferous Visean Pittenweem and Anstruther Formations on the East Fife coast. Here we describe a new west coast single …
— The Al-Khlata Formation, which spans the late Carboniferous to Early Permian time, thickens from ~100 m in outcrops along the Huqf uplift to over 800 m in the Interior Oman basins (Osterloff et al., 2004), which suggests that it on-lapped the Oman-Hadhramaut Arch, and was confined within the flanking Hercynian basin and salt …
— The fold axis of the Upper Carboniferous limestone is similar to that of the Middle Jurassic one, likely indicating a post-Middle Jurassic folding. Our paleomagnetic sampling was carried out on both limbs …
The evolution of the early Carboniferous Limestone province in southwest Britain - Volume 124 Issue 5 Skip to main content Accessibility help We use cookies to distinguish you from other users and to provide you with a better experience on our websites.
— However, in order to improve our understanding of the glacially-related reservoirs depositional facies and diagenetic history, this study focuses on examining the outcropping Late Carboniferous-Early Permian glaciogenic Al Khlata Formation sediments of the Haushi Group in Wadi Daiqa of Oman Mountains (Fig. 1 A–D).The lately …
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The Carboniferous Limestone has been folded and faulted by massive Earth movements which can be seen by the fact that the rocks are now above sea-level and no longer horizontal. The rocks generally dip (slope) gently eastwards and, in some places, clear folds in the rock can be seen especially at the Great Orme and Bryn Alyn (Denbighshire). ...
CARBONIFEROUS LIMESTONE, ISLE OF MAN 105 Fig. 8. Boulder limestone overlying lower black beds. The hammer is 40cm long. Poyllvaaish Formation at the bottom of the scarp (Figs 6, 7). Locally these beds have a maximum dip of 55°, apparently as a result of compactional over-steepening
— The Carboniferous Limestone cropping out near Wellington and near Newport in the Wrekin district has hitherto received little attention. One or two references to the Lower Carboniferous rocks of the area are made in Geology in the Field, in which the limestone is referred to the Dibunophyllum zone, and the intrusive material underlying …