Faroe shetland basin
WebThe Faroe–Shetland Basin (FSB), located west of the Shetland Isles on the NE Atlantic continental margin (), is one of the only remaining significant exploration frontiers on the UK Continental Shelf (UKCS), and will also arguably be one of the most important areas to contribute to indigenous oil and gas supply in the next 40 years (Austin et al. 2014; Ellis … WebCoverage over the Faroe-Shetland Basin; Pre-Stack Time Migrated (PSTM) Rona Ridge. 2,174 km 2 3D multi-client seismic survey; Coverage over the West Shetland Basin; Pre …
Faroe shetland basin
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WebSep 1, 2013 · The Faroe-Shetland Basin is a NE–SW trending basin located between the Shetland Islands and Faroe Islands. It developed as the result of several rift phases in Late Palaeozoic and Mesozoic times with the dominant basin forming faults being of NE–SW to N–S orientation ( Doré et al., 1999 ; Roberts et al., 1999 ). WebThe NE-trending features are the most numerous, though they are mainly restricted to the NE Faroe–Shetland Basin where an inherited Caledonian structural grain is most …
Webcontinental crust of the Mesozoic Faroe-Shetland Basin in the southeast. The major stratigraphic features are marked on the profile in Fig. 2. The red line marks the … WebApr 1, 2024 · The Faroe-Shetland Basin (FSB) is located between the Shetland and Faroe Islands on the NE Atlantic Margin (Fig. 1). The basin can be sub divided into a series of …
WebJul 19, 2016 · This study presents an appraisal of the Cretaceous tectonostratigraphical development of the Faroe–Shetland region. It combines details of the rock record with seismic stratigraphical information, and the resulting stratigraphic framework provides constraints on the timing and nature of sedimentary basin development in the … WebJan 17, 2024 · Assessed the Hydrocarbon Prospectivity of the West Faroe-Shetland Basin using 2D and 3D seismic data and well data. The …
WebIn the Faroe–Shetland Basin, the internal seismic character Notwithstanding the uncertain spatial and temporal extent of the K2 megasequence is commonly obscured by high- of the late Campanian unconformity, the Rona High became amplitude reflections associated with Paleocene sills that largely submerged during this interval. have intruded ...
The Faroe–Shetland Channel is stretch of the North Atlantic lying between the two island groups of Shetland and the Faroe Islands. The channel is a rift basin that separates the Scottish and the Faroese continental shelves, and has a maximum depth of 1900 m, compared to the surrounding seabed which mostly lies at 200 m. It was first noted by Charles Wyville Thomson during the mid-nin… langley air force base financeWebThe Faroe-Shetland Basin is a sedimentary basin formed by mainly Mesozoic rifting that lies between the Faroe Islands and the Shetland Islands.[1] It has been the site of … hempfield bandWebImproved seismic imaging of the deep structures in the Faroe–Shetland Basin has revealed a complex Mesozoic rift system with shifting block polarity along the West Shetland Platform. Newly acquired seismic data has led to the focus of hydrocarbon exploration on structurally defined Mesozoic traps and has re-opened exploration in the … langley agency boca ratonWebSelect search scope, currently: articles+ all catalog, articles, website, & more in one search; catalog books, media & more in the Stanford Libraries' collections; articles+ journal articles & other e-resources langley air force base address zip codeWeb67 The Faroe-Shetland Basin (FSB) is located on the NE Atlantic Margin, between Shetland and 68 the Faroe Islands (Fig. 1a). The FSB consists of a collection of southwest-northeast trending 69 sub-basins of Mesozoic to recent basin fill, bounded by intra-basinal highs of Precambrian hempfield baseball paWebThe NE-trending features are the most numerous, though they are mainly restricted to the NE Faroe–Shetland Basin where an inherited Caledonian structural grain is most prevalent. Limited evidence exists for late Paleocene and early Eocene activity along the Wyville Thomson Ridge, whereas mid–late Eocene and Oligocene fold growth is more ... langley agents crook limitedWeb558 Faroe-Shetland Basin became a larger, more integrated depocentre (Fig. 9b). The Judd, Foula . 559 and Flett sub-basins accumulated predominantly marine mudstones of the Valhall, Carrack, 560 Cruiser and Rødby formations, fringed by coarse clastic deposits, including basal . langley air force base hospital address