scholarly journals Thermal history and oil charge on the UK Atlantic margin

2005 ◽  
Vol 11 (2) ◽  
pp. 99-112 ◽  
Author(s):  
J. Parnell ◽  
P.F. Green ◽  
G. Watt ◽  
D. Middleton
Author(s):  
M.K. Lee ◽  
R.M. Carruthers ◽  
Z.K. Dabek ◽  
I.F. Smith ◽  
J.W.f. Edwards ◽  
...  

Author(s):  
J.W. Gallagher ◽  
J. Bingham ◽  
R.W. Simm
Keyword(s):  
The Uk ◽  

1999 ◽  
Author(s):  
T.P.D. Smith ◽  
G. Pettigrew ◽  
M.T.C. Worsley ◽  
B.R. Walls ◽  
E. Clark ◽  
...  
Keyword(s):  
The Uk ◽  

2020 ◽  
Vol 52 (1) ◽  
pp. 990-1002 ◽  
Author(s):  
M. V. Ward ◽  
T. Primmer ◽  
E. Laws ◽  
K. Macgregor ◽  
T. Harpley ◽  
...  

AbstractThe Schiehallion subsea development comprises two fields, Schiehallion and Loyal, which are located approximately 200 km to the west of the Shetland Islands in the UK Continental Shelf. The Schiehallion and Loyal fields were discovered in late 1993 and 1994, respectively, with a combined oil-in-place of more than 2.3 Bbbl. The fields are developed under waterflood and were on production from 1998 to 2013. After an extended shut-in, the fields were brought back on line in 2017, through new floating production facilities.Most of the production to date has been from the Paleocene Vaila Formation deep-water turbidite, in the T31 and T34 reservoir intervals. The ongoing Quad 204 redevelopment drilling programme commenced in April 2015, has drilled and completed 21 wells to date, and is expected to continue for several more years. The campaign includes new producer–injector pairs and stand-alone wells to support existing well stock, targeting stacked turbidite reservoir intervals, including the youngest T35–T34 interval, the main T31 interval and the previously under-developed T28–T25 fairway.In addition to an active drilling programme, a 4D seismic survey was acquired and processed in 2018, and its interpretation is key to unlocking further potential sources of value in this mature field.


First Break ◽  
2003 ◽  
Vol 21 (4) ◽  
Author(s):  
R.W. Gatliff ◽  
H. Johnson ◽  
J.D. Ritchie ◽  
K. Hitchen
Keyword(s):  
The Uk ◽  

2020 ◽  
Vol 52 (1) ◽  
pp. 967-979 ◽  
Author(s):  
J. Clark ◽  
P. Matthews ◽  
C. Parry ◽  
M. Rowlands ◽  
A. Tessier

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 saturated oil rim. Seismic reservoir characterization is a key to the field development where differentiation of fluid type proved challenging. Both fields came on stream in 2016 as part of the Greater Laggan area development scheme.


2020 ◽  
Vol 52 (1) ◽  
pp. 931-951 ◽  
Author(s):  
A. G. Robertson ◽  
M. Ball ◽  
J. Costaschuk ◽  
J. Davidson ◽  
N. Guliyev ◽  
...  

AbstractThe Clair Field is a giant oilfield containing in the region of 6–7 Bbbl of stock tank oil initially in place, located approximately 75 km west of the Shetland Islands. As such, it represents the single biggest hydrocarbon accumulation on the UK Continental Shelf. Clair was discovered in 1977, but first production did not occur from Phase 1 until 2005, after a lengthy appraisal period. The major appraisal milestone occurred in 1991 after well 206/8-8 proved up fractured clastic red beds of the Devonian Lower Clair Group. This was followed up with an extended well test on 206/8-10Z, which demonstrated the longer-term performance of the reservoir. Further appraisal on Clair Ridge led to the sanction of the Clair Ridge, which came on stream in November 2018. Following the Greater Clair appraisal programme in 2013–15, development options are currently being worked for Clair South, which will develop the Lower Clair Group reservoirs together with overlying shallow-marine reservoirs of the Cretaceous and Jurassic.


1999 ◽  
Vol 5 (1) ◽  
pp. 349-357 ◽  
Author(s):  
P. F. GREEN ◽  
I. R. DUDDY ◽  
K. A. HEGARTY ◽  
R. J. BRAY

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