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Journal articles on the topic 'Shetland Basin'

Author: Grafiati

Published: 4 June 2021

Last updated: 14 February 2022

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1

ASHCROFT, W. A., A. HURST, and C. J. MORGAN. "Reconciling gravity and seismic data in the Faeroe–Shetland Basin, West of Shetland." Geological Society, London, Petroleum Geology Conference series 5, no. 1 (1999): 595–600. http://dx.doi.org/10.1144/0050595.

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2

GRANT, N., A. BOUMA, and A. McINTYRE. "The Turonian play in the Faeroe–Shetland Basin." Geological Society, London, Petroleum Geology Conference series 5, no. 1 (1999): 661–73. http://dx.doi.org/10.1144/0050661.

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3

TURNER, J. D., and R. A. SCRUTTON. "Subsidence patterns in western margin basins: evidence from the Faeroe–Shetland Basin." Geological Society, London, Petroleum Geology Conference series 4, no. 1 (1993): 975–83. http://dx.doi.org/10.1144/0040975.

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4

Lee, D. K., Y. K. Jin, Y. Kim, and S. H. Nam. "Seismicity and tectonics around the northern Antarctic Peninsula from King Sejong station data." Antarctic Science 12, no. 2 (2000): 196–204. http://dx.doi.org/10.1017/s0954102000000250.

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Local earthquakes recorded at the King Sejong station (62° 13′31″S, 58° 47′07″W) from 1995–96 have been analysed to study the seismicity and tectonics around the northern Antarctic Peninsula. The nature of shallow-focused normal fault earthquakes along the South Shetland Platform is still unclear. Dominant normal fault earthquakes and minor strike-slip earthquakes in the Eastern Bransfield Basin suggest 1) ongoing extension, and 2) transtensional stress transmitted from the Antarctic–Scotia transform boundaries, the South Scotia Ridge and the Shackleton Fracture Zone. A lack of seismicity in t

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5

Larsen, Michael, Christian Knudsen, Dirk Frei, Martina Frei, Thomas Rasmussen, and Andrew G. Whitham. "East Greenland and Faroe–Shetland sediment provenance and Palaeogene sand dispersal systems." Geological Survey of Denmark and Greenland (GEUS) Bulletin 10 (November 29, 2006): 29–32. http://dx.doi.org/10.34194/geusb.v10.4899.

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The sedimentation and basin evolution of the Kangerlussuaq Basin, southern East Greenland has gained renewed interest with the licensing rounds offshore the Faroe Islands in 2000 and 2005, as it forms an important analogy to the Faroese geological setting. The Faroes frontier area is in part covered by basalts and is a high-risk area with poorly known plays and sedimentary basins. It is therefore essential to obtain as much information as possible on the evolution of sedimentary basins on the rifted volcanic margins closest to the Faroese Islands margin. Plate reconstructions of the North Atla

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6

DEAN, KEVIN, KEVIN McLACHLAN, and ALAN CHAMBERS. "Rifting and the development of the Faeroe-Shetland Basin." Geological Society, London, Petroleum Geology Conference series 5, no. 1 (1999): 533–44. http://dx.doi.org/10.1144/0050533.

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7

Carr, A. D., and I. C. Scotchman. "Thermal history modelling in the southern Faroe–Shetland Basin." Petroleum Geoscience 9, no. 4 (2003): 333–45. http://dx.doi.org/10.1144/1354-079302-494.

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8

Solari, M. A., F. Hervé, J. Martinod, J. P. Le Roux, L. E. Ramírez, and C. Palacios. "Geotectonic evolution of the Bransfield Basin, Antarctic Peninsula: insights from analogue models." Antarctic Science 20, no. 2 (2008): 185–96. http://dx.doi.org/10.1017/s095410200800093x.

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AbstractThe Bransfield Strait, located between the South Shetland Islands and the north-western end of the Antarctic Peninsula, is a back-arc basin transitional between rifting and spreading. We compiled a geomorphological structural map of the Bransfield Basin combining published data and the interpretation of bathymetric images. Several analogue experiments reproducing the interaction between the Scotia, Antarctic, and Phoenix plates were carried out. The fault configuration observed in the geomorphological structural map was well reproduced by one of these analogue models. The results sugge

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9

Pearson, M. J. "Clay mineral distribution and provenance in Mesozoic and Tertiary mudrocks of the Moray Firth and northern North Sea." Clay Minerals 25, no. 4 (1990): 519–41. http://dx.doi.org/10.1180/claymin.1990.025.4.10.

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AbstractClay mineral abundances in Mesozoic and Tertiary argillaceous strata from 15 exploration wells in the Inner and Outer Moray Firth, Viking Graben and East Shetland Basins of the northern North Sea have been determined in <0·2 µm fractions of cuttings samples. The clay assemblages of more deeply-buried samples cannot be unambiguously related to sedimentary input because of the diagenetic overprint which may account for much of the chlorite and related interstratified minerals. Other sediments, discussed on a regional basis and related to the geological history of the basins, are inter

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10

Fliedner, Moritz M., and Robert S. White. "Depth imaging of basalt flows in the Faeroe-Shetland Basin." Geophysical Journal International 152, no. 2 (2003): 353–71. http://dx.doi.org/10.1046/j.1365-246x.2003.01833.x.

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11

BOOTH, J., T. SWIECICKI, and P. WILCOCKSON. "The tectono-stratigraphy of the Solan Basin, west of Shetland." Geological Society, London, Petroleum Geology Conference series 4, no. 1 (1993): 987–98. http://dx.doi.org/10.1144/0040987.

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12

LEE, M. J., and Y. J. HWANG. "Tectonic evolution and structural styles of the East Shetland Basin." Geological Society, London, Petroleum Geology Conference series 4, no. 1 (1993): 1137–49. http://dx.doi.org/10.1144/0041137.

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13

HERRIES, R., R. PODDUBIUK, and P. WILCOCKSON. "Solan, Strathmore and the back basin play, West of Shetland." Geological Society, London, Petroleum Geology Conference series 5, no. 1 (1999): 693–712. http://dx.doi.org/10.1144/0050693.

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14

BARTON, P. J., S. HUGHES, C. ZELT, and R. MASOTTI. "Exploring the Shetland–Faeroes Basin using wide-angle seismic technology." Geological Society, London, Petroleum Geology Conference series 5, no. 1 (1999): 1253. http://dx.doi.org/10.1144/0051253.

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15

SELL, I., G. POUPEAU, J. M. GONZÁLEZ-CASADO, and J. LÓPEZ-MARTÍNEZ. "A fission track thermochronological study of King George and Livingston islands, South Shetland Islands (West Antarctica)." Antarctic Science 16, no. 2 (2004): 191–97. http://dx.doi.org/10.1017/s0954102004001907.

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This paper reports the dating of apatite fission tracks in eleven rock samples from the South Shetland Archipelago, an island arc located to the north-west of the Antarctic Peninsula. Apatites from Livingston Island were dated as belonging to the Oligocene (25.8 Ma: metasediments, Miers Bluff Formation, Hurd Peninsula) through to the Miocene (18.8 Ma: tonalites, Barnard Point). Those from King George Island were slightly older, belonging to the Early Oligocene (32.5 Ma: granodiorites, Barton Peninsula). Towards the back-arc basin (Bransfield Basin), the apatite appears to be younger. This allo

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16

Clark, J., C. Parry, M. Rowlands, A. Tessier, and D. Mazzuchelli. "The Glenlivet Field, Block 214/30a, UK Atlantic Margin." Geological Society, London, Memoirs 52, no. 1 (2020): 958–66. http://dx.doi.org/10.1144/m52-2018-24.

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AbstractThe Glenlivet Field, located in Block 214/30a within the Faroe–Shetland Basin, was put on production in August 2017. It lies approximately 70 km NW of the Shetland Islands, in a water depth of c. 440 m. The development consists of two subsea wells that produce gas condensate from the Paleocene Vaila Formation, which comprises deep-water turbidite deposits with excellent petrophysical properties. It is part of a joint development scheme along with the Edradour Field that sees the commingled multiphase production transported to the Shetland Gas Plant via tie-back to the pre-existing Lagg

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17

Clark, J., P. Matthews, C. Parry, M. Rowlands, and A. Tessier. "The Laggan and Tormore fields, Blocks 206/1 and 205/5, UK Atlantic Margin." Geological Society, London, Memoirs 52, no. 1 (2020): 967–79. http://dx.doi.org/10.1144/m52-2018-25.

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AbstractThe Laggan and Tormore fields are found within the Flett sub-basin of the Faroe–Shetland Basin. Situated 120 km west of the Shetland Islands in 600 m water depth, they are part of the deepest subsea development in the UK to date with a 143 km subsea tie-back to onshore facilities.The reservoirs are found within the T35 biostratigraphic sequence of the Paleocene Vaila Formation and comprise sand-rich turbiditic channelized lobes with good reservoir properties, separated by metric to decimetric shale packages. Laggan is a gas-condensate field, whereas Tormore fluid is a richer gas with a

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18

Spray, John G. "Thrust-related metamorphism beneath the Shetland Islands oceanic fragment, northeast Scotland." Canadian Journal of Earth Sciences 25, no. 11 (1988): 1760–76. http://dx.doi.org/10.1139/e88-167.

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A ≤400 m thick metamorphic sequence showing thermal inversion is present beneath a dismembered ultrabasic–basic complex in the Shetland Islands of northeast Scotland. The metamorphic grade changes from upper amphibolite facies in metabasites at the top of the sequence to low greenschist facies in metasediments at the base. Garnet–clinopyroxene thermometry yields temperatures of ~ 750 °C (at 300 MPa) for the highest grade assemblage. There is no evidence for high pressures of metamorphism, and maximum overburden may never have exceeded the original thickness of the overlying ultrabasic–basic co

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19

Watson, Peter. "Industry – inputs to the environment." Proceedings of the Royal Society of Edinburgh. Section B. Biological Sciences 103 (1995): 21–29. http://dx.doi.org/10.1017/s0269727000005911.

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Sullom Voe Terminal has been in operation since November 1978, processing crude oil from the East Shetland Basin. Gas processing was initiated in April 1981, with full LPG production commencing in May 1982. The terminal is operated by BP Exploration, while port operations are controlled by Shetland Islands Council. This paper will summarise both terminal and port operations, to highlight those areas which involve a discharge or emission to the environment. Variation of the discharges with time will also be indicated to provide a background against which the results of the environmental monitor

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20

Hansen, Bogi, Turið Poulsen, Karin Margretha Húsgarð Larsen, et al. "Atlantic water flow through the Faroese Channels." Ocean Science 13, no. 6 (2017): 873–88. http://dx.doi.org/10.5194/os-13-873-2017.

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Abstract. Through the Faroese Channels – the collective name for a system of channels linking the Faroe–Shetland Channel, Wyville Thomson Basin, and Faroe Bank Channel – there is a deep flow of cold waters from Arctic regions that exit the system as overflow through the Faroe Bank Channel and across the Wyville Thomson Ridge. The upper layers, in contrast, are dominated by warm, saline water masses from the southwest, termed Atlantic water. In spite of intensive research over more than a century, there are still open questions on the passage of these waters through the system with conflicting

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21

Fletcher, Rosie, Nick Kusznir, Alan Roberts, and Robert Hunsdale. "The formation of a failed continental breakup basin: The Cenozoic development of the Faroe-Shetland Basin." Basin Research 25, no. 5 (2013): 532–53. http://dx.doi.org/10.1111/bre.12015.

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22

Clark, J., D. Mazzuchelli, M. Rowlands, N. Jebara, and C. Parry. "The Edradour Field, Block 206/4a, UK Atlantic Margin." Geological Society, London, Memoirs 52, no. 1 (2020): 952–57. http://dx.doi.org/10.1144/m52-2018-23.

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AbstractThe Edradour Field, located in Licence P1453 on Block 206/4a of the Faroe–Shetland Basin, was put on production in August 2017. It lies c. 50 km NW of the Shetland Islands in a water depth of c. 300 m, and consists of one subsea well that produces gas condensate from the Albian Black Sail Member of the Commodore Formation. It is part of a joint development scheme along with the Glenlivet Field that sees the commingled multiphase production transported to the Shetland Gas Plant via tieback to the pre-existing Laggan–Tormore flowlines. The Edradour single well development has reserves of

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23

Marshall, J. E. A. "Devonian miospores from Papa Stour, Shetland." Transactions of the Royal Society of Edinburgh: Earth Sciences 79, no. 1 (1988): 13–18. http://dx.doi.org/10.1017/s0263593300014073.

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ABSTRACTDevonian miospores have been discovered in the previously poorly dated Old Red Sandstone volcanic sequence of Papa Stour. They occur at two sites in minor sedimentary deposits between the lavas, and fossil fish remains are also present. The age range of the miospores is mid Eifelian to early Givetian, probably more specifically late Eifelian and from a position close to the Achanarras horizon. This allows a correlation of the Papa Stour volcanic sequence with that of the Upper Stromness Flags of Orkney and not the tuffaceous horizons in the Eday Sandstones. The good preservation and co

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24

ANDERTON, R. "Sedimentation and basin evolution in the Paleogene of the Northern North Sea and Faeroe–Shetland basins." Geological Society, London, Petroleum Geology Conference series 4, no. 1 (1993): 31. http://dx.doi.org/10.1144/0040031.

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25

Heath, Michael R., Peter R. Boyle, Astthor Gislason, et al. "Comparative ecology of over-wintering Calanus finmarchicus in the northern North Atlantic, and implications for life-cycle patterns." ICES Journal of Marine Science 61, no. 4 (2004): 698–708. http://dx.doi.org/10.1016/j.icesjms.2004.03.013.

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Abstract Data from plankton net and Optical Plankton Counter sampling during 12 winter cruises between 1994 and 2002 have been used to derive a multi-annual composite 3-D distribution of the abundance of over-wintering Calanus finmarchicus in a swath across the North Atlantic from Labrador to Norway. Dense concentrations occurred in the Labrador Sea, northern Irminger Basin, northern Iceland Basin, eastern Norwegian Sea, Faroe–Shetland Channel, and in the Norwegian Trench of the North Sea. A model of buoyancy regulation in C. finmarchicus was used to derive the lipid content implied by the in

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26

Scotchman, Iain C., Anthony G. Doré, and Anthony M. Spencer. "Petroleum systems and results of exploration on the Atlantic margins of the UK, Faroes & Ireland: what have we learnt?" Geological Society, London, Petroleum Geology Conference series 8, no. 1 (2016): 187–97. http://dx.doi.org/10.1144/pgc8.14.

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AbstractThe exploratory drilling of 200 wildcat wells along the NE Atlantic margin has yielded 30 finds with total discovered resources of c. 4.1×109 barrels of oil equivalent (BOE). Exploration has been highly concentrated in specific regions. Only 32 of 144 quadrants have been drilled, with only one prolific province discovered – the Faroe–Shetland Basin, where 23 finds have resources totalling c. 3.7×109 BOE. Along the margin, the pattern of discoveries can best be assessed in terms of petroleum systems. The Faroe–Shetland finds belong to an Upper Jurassic petroleum system. On the east flan

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27

Fliedner, Moritz M., and Robert S. White. "Sub-basalt imaging in the Faeroe-Shetland Basin with large-offset data." First Break 19, no. 5 (2001): 247–52. http://dx.doi.org/10.1046/j.0263-5046.2001.00156.x.

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28

White, Robert S., John R. Smallwood, Moritz M. Fliedner, Brian Boslaugh, Jenny Maresh, and Juergen Fruehn. "Imaging and regional distribution of basalt flows in the Faeroe-Shetland Basin." Geophysical Prospecting 51, no. 3 (2003): 215–31. http://dx.doi.org/10.1046/j.1365-2478.2003.00364.x.

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29

Champion, M. E. Shaw, N. J. White, S. M. Jones, and J. P. B. Lovell. "Quantifying transient mantle convective uplift: An example from the Faroe-Shetland basin." Tectonics 27, no. 1 (2008): n/a. http://dx.doi.org/10.1029/2007tc002106.

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30

Crawford, Wayne C., and Satish C. Singh. "Sediment shear properties from seafloor compliance measurements: Faroes-Shetland basin case study." Geophysical Prospecting 56, no. 3 (2008): 313–25. http://dx.doi.org/10.1111/j.1365-2478.2007.00672.x.

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31

Bell, Brian, and Helen Butcher. "On the emplacement of sill complexes: evidence from the Faroe-Shetland Basin." Geological Society, London, Special Publications 197, no. 1 (2002): 307–29. http://dx.doi.org/10.1144/gsl.sp.2002.197.01.12.

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32

Larsen, M., T. Rasmussen, and L. Hjelm. "Cretaceous revisited: exploring the syn-rift play of the Faroe–Shetland Basin." Geological Society, London, Petroleum Geology Conference series 7, no. 1 (2010): 953–62. http://dx.doi.org/10.1144/0070953.

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33

Morgan, Richard, and Colm Murphy. "The Use of Potential Fields in the Search for Potential Fields in the Faroe-Shetland Area." SPE Reservoir Evaluation & Engineering 1, no. 05 (1998): 476–84. http://dx.doi.org/10.2118/51828-pa.

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This paper (SPE 51828) was revised for publication from paper SPE 38503, first presented at the 1997 SPE Offshore Europe Conference, Aberdeen, 9-12 September. Original manuscript received for review 9 September 1997. Revised manuscript received 6 July 1998. Paper peer approved 10 July 1998. Summary Fundamental geological and environmental differences exist between the basins of the North Sea and the basins of the northwest European continental margin, and strategies for success in the North Sea have not necessarily transferred directly to the continental margin. As a result, exploration outcom

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34

Zemko, Karol, Krzysztof Pabis, Jacek Siciński, and Magdalena Błażewicz. "New records of isopod species of the Antarctic Specially Managed Area No. 1, Admiralty Bay, South Shetland Islands." Polish Polar Research 38, no. 3 (2017): 409–19. http://dx.doi.org/10.1515/popore-2017-0017.

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AbstractAdmiralty Bay (King George Island) is an Antarctic Specially Managed Area and one the most thoroughly studied small-scale marine basins in the Southern Ocean. Our study provides new data on the isopod fauna in this glacially affected fjord. Twelve species of isopods were recorded in this basin for the first time. Six of them were found for the first time in the region of the South Shetland Islands. The highest number of species new for Admiralty Bay were found in the families Munnopsidae (4 species) and Munnidae (3 species).

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35

Barclay, A. H., W. S. D. Wilcock, and J. M. Ibáñez. "Bathymetric constraints on the tectonic and volcanic evolution of Deception Island Volcano, South Shetland Islands." Antarctic Science 21, no. 2 (2008): 153–67. http://dx.doi.org/10.1017/s0954102008001673.

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AbstractDeception Island is the largest volcano in the actively extending Bransfield Basin, a marginal basin situated behind the extinct South Shetland Islands arc. Deception Island has been well studied but its submerged flanks have not. A multibeam bathymetry survey was conducted around the island in 2005. Data from the flooded caldera show no evidence for recent localized resurgence. The gently-sloped bottom of the caldera basin is consistent with either a broad zone of resurgence on its east side associated with trap door deformation or with higher rates of sediment supply from the east si

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36

Hughes, Stephen, Penny J. Barton, and David Harrison. "Exploration in the Shetland‐Faeroe Basin using densely spaced arrays of ocean‐bottom seismometers." GEOPHYSICS 63, no. 2 (1998): 490–501. http://dx.doi.org/10.1190/1.1444350.

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Recent exploration activity in the peripheral regions of the Shetland‐Faeroe Basin, offshore northwest Scotland, has led to the discovery of some of the largest oil reserves on the United Kingdom (UK) continental shelf. We present results from two ocean‐bottom seismometer profiles acquired by Mobil North Sea Ltd. across the center of the Shetland‐Faeroe Basin. These data provide a powerful tool for delineating long‐wavelength velocity variations and thus have potential for reducing the nonuniqueness associated with conventional seismic exploration methods. Analysis of the first‐arrival travelt

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37

Schofield, Nick, and David W. Jolley. "Development of intra-basaltic lava-field drainage systems within the Faroe–Shetland Basin." Petroleum Geoscience 19, no. 3 (2013): 273–88. http://dx.doi.org/10.1144/petgeo2012-061.

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38

Watson, Douglas, Nick Schofield, David Jolley, et al. "Stratigraphic overview of Palaeogene tuffs in the Faroe–Shetland Basin, NE Atlantic Margin." Journal of the Geological Society 174, no. 4 (2017): 627–45. http://dx.doi.org/10.1144/jgs2016-132.

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39

NAYLOR, P. H., B. R. BELL, D. W. JOLLEY, P. DURNALL, and R. FREDSTED. "Palaeogene magmatism in the Faeroe–Shetland Basin: influences on uplift history and sedimentation." Geological Society, London, Petroleum Geology Conference series 5, no. 1 (1999): 545–58. http://dx.doi.org/10.1144/0050545.

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40

Haszeldine, R. S., J. D. Ritchie, and K. Hitchen. "Seismic and well evidence for the early development of the Faeroe–Shetland Basin." Scottish Journal of Geology 23, no. 3 (1987): 283–300. http://dx.doi.org/10.1144/sjg23030283.

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41

Ritchie, J. Derek, Howard Johnson, Martyn F. Quinn, and Robert W. Gatliff. "The effects of Cenozoic compression within the Faroe-Shetland Basin and adjacent areas." Geological Society, London, Special Publications 306, no. 1 (2008): 121–36. http://dx.doi.org/10.1144/sp306.5.

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42

KANARIS-SOTIRIOU, RAYMOND, and FERGUS G. F. GIBB. "Short Paper: Plagiogranitic differentiates in MORB-type sills of the Faeroe–Shetland Basin." Journal of the Geological Society 146, no. 4 (1989): 607–10. http://dx.doi.org/10.1144/gsjgs.146.4.0607.

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43

Turrell, W. "Hydrography of the East Shetland Basin in relation to decadal North Sea variability." ICES Journal of Marine Science 53, no. 6 (1996): 899–916. http://dx.doi.org/10.1006/jmsc.1996.0112.

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44

Warrender, John. "The Murchison Field, Block 211/19a, UK North Sea." Geological Society, London, Memoirs 14, no. 1 (1991): 165–73. http://dx.doi.org/10.1144/gsl.mem.1991.014.01.21.

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AbstractThe Murchison oil field forms part of the Brent oil province in the East Shetland Basin, northern North Sea. The field, which straddles the UK-Norway international boundary, was discovered in 1975 and began production with Conoco (UK) Ltd as Operator, in 1980. Like many oil accumulations in the East Shetland Basin the trap consists of a northwesterly dipping rotated fault block of Jurassic-Triassic age sourced and sealed by unconformable Upper Jurassic shales. The productive reservoir consists of Middle Jurassic Brent Group sandstones which represent the south to north progradation of

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45

Fyfe, Laura-Jane C., Nick Schofield, Simon Holford, et al. "Geology and petroleum prospectivity of the Sea of Hebrides Basin and Minch Basin, offshore NW Scotland." Petroleum Geoscience 27, no. 4 (2021): petgeo2021–003. http://dx.doi.org/10.1144/petgeo2021-003.

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The Sea of Hebrides Basin and Minch Basin are late Paleozoic–Mesozoic rift basins located to the NW of the Scottish mainland. The basins were the target of small-scale petroleum exploration from the late 1960s to the early 1990s, with a total of three wells drilled within the two basins between 1989 and 1991. Although no commercially viable petroleum discoveries were made, numerous petroleum shows were identified within both basins, including a gas show within the Upper Glen 1 well in Lower Jurassic limestones. Organic-rich shales have been identified throughout the Jurassic succession within

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46

Duncan, Louise J., C. J. Dennehy, P. M. Ablard, and D. W. Wallis. "The Rosebank Field, Blocks 213/27a, 213/26b, 205/1a and 205/2a, UK Atlantic Margin." Geological Society, London, Memoirs 52, no. 1 (2020): 980–89. http://dx.doi.org/10.1144/m52-2018-42.

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AbstractThe Rosebank Field is located primarily in Block 213/27a in the Faroe–Shetland Basin, c. 130 km west of the Shetland Islands in water depths of c. 1100 m (3600 ft). Hydrocarbons are trapped within an elongate, SW–NE-trending four-way anticlinal structure. The principal Colsay Sandstone Member reservoir consists of several vertically stacked, Late Paleocene to Early Eocene fluvial and deltaic reservoirs separated by volcanic sequences. Well log and core data indicate that reservoir quality is high, with porosities in the range of 19–23% and average permeability of c. 3 D. Oil quality is

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47

Mudge, D. C., and J. P. Bujak. "Biostratigraphic evidence for evolving palaeoenvironments in the Lower Paleogene of the Faeroe–Shetland Basin." Marine and Petroleum Geology 18, no. 5 (2001): 577–90. http://dx.doi.org/10.1016/s0264-8172(00)00074-x.

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48

Ritchie, J. D., H. Johnson, and G. S. Kimbell. "The nature and age of Cenozoic contractional deformation within the NE Faroe–Shetland Basin." Marine and Petroleum Geology 20, no. 5 (2003): 399–409. http://dx.doi.org/10.1016/s0264-8172(03)00075-8.

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Taylor, Frederick W., Michael G. Bevis, Ian W. D. Dalziel, et al. "Kinematics and segmentation of the South Shetland Islands-Bransfield basin system, northern Antarctic Peninsula." Geochemistry, Geophysics, Geosystems 9, no. 4 (2008): n/a. http://dx.doi.org/10.1029/2007gc001873.

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Morton, Andrew C., J. Douglas Boyd, and David F. Ewen. "Evolution of Paleocene sediment dispersal systems in the Foinaven Sub-basin, west of Shetland." Geological Society, London, Special Publications 197, no. 1 (2002): 69–93. http://dx.doi.org/10.1144/gsl.sp.2002.197.01.04.

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