Submitting Institution
University of CambridgeUnit of Assessment
Earth Systems and Environmental SciencesSummary Impact Type
TechnologicalResearch Subject Area(s)
Earth Sciences: Geology, Geophysics, Oceanography
Summary of the impact
Approximately 70% of the continental margins contain significant volcanic
flows, created when continents broke apart. Because large quantities of
hydrocarbons may be trapped in sediments beneath the lava flows the
ability to image through the basalt layers is of tremendous commercial
value. However, these lava flows impede conventional seismic imaging by
scattering energy, thus blocking the view of what lies beneath. Professor
White and his team developed a technique, based on work in the 1990's,
for imaging through the lava flows which differs radically from the
conventional commercial approach. Professor White's technique
has been widely adopted by the oil industry and has had a dramatic global
impact, particularly for companies expanding exploration into deeper
waters, including the north-west margin of Europe, the South American
coast, particularly off Brazil and the continental margins of India. This
approach has now become the norm having been adopted by oil companies
globally.
Underpinning research
Professor White's research has focused on using seismic methods to
understand the Earth's subsurface crust. In the 1990's Prof White and his
team developed methods, utilising seismic energy propagating at much
larger angles than conventionally recorded, for imaging through lava flows
in order to study the interactions between rifting and outbursts of
massive volumes of molten rock. An essential part of the work has involved
the development of ocean bottom seismometers and the new software
necessary for processing and modelling wide-angle seismograms recorded at
sea. The key insights to successful imaging through basalts which came out
of this academic research were:
- To acquire seismic data at large offsets using either very long
hydrophone streamers towed behind a ship or fixed ocean bottom
seismometers on the seabed.
- To use a broad-band seismic source with a large bandwidth including
low frequency (below 10Hz) energy because higher frequencies are
scattered by the basalts and do not penetrate them.
In the 1990s the oil industry moved into the exploration of new frontiers
on the continental margins. In 1995, having become aware of Prof White's
work on volcanism caused by rifting of the North Atlantic, the oil company
Amerada Hess approached him for help with their exploration of the
Faroe-Shetland region which contained large volcanic flows.
Since that time the research has been considerably extended,
significantly increased in scope and breadth, and continues to the present
day. For example, drawing on his experience in academic surveys of
obtaining large offset profiles by using two ships instead of one, Prof
White designed a large two-ship experiment on the Faroes shelf which was
acquired in 1996, using well-equipped commercial vessels. Results showing
successful sub-basalt imaging were announced in October 1997 at the
prestigious 4-yearly conference on the Petroleum Geology of the NW
European shelf by the CEO of Amerada Hess. As a result of the success of
this 1996 survey, Professor White continued to refine the technique,
working with Amerada Hess to design another survey which was shot in 1998.
This recognition led in 2001 to setting up a large academic consortium
(called iSIMM, for `integrated Seismic Imaging and Modelling of Margins'),
jointly with another HEI (Prof N.J. Kusznir of Liverpool University) and
two contractor companies, Badleys and Schlumberger Cambridge Research Ltd
(SCR). This attracted 8 oil companies to sign up, WesternGeco donated £1
million of ship time and processing to acquire long-offset data (12000
metre streamer) across the Faroes shelf and continental margin.
The survey parameters were designed by Dr Phil Christie (SCR) and Prof
White. In addition to a long offset streamer, they deployed 85 3-component
ocean bottom seismometers to obtain offsets out to 120 km. The source
design focussed on generating low frequencies because work, directed by
Prof White, on seismics recorded down boreholes had shown that low
frequencies were required to propagate through basalts. The actual source
wavelet was recorded in deep water using a vertical array of hydrophones
deployed for the purpose, and compared to the theoretical modelled
waveform. SCR subsequently took out a patent on an aspect of modelling the
signature from the novel source design (UK patent 2 425 838, in 2007; US
patent 7,551,515, in 2010) and another (US Patent 7,961,549, which was
granted on 14 June 2011) describing low frequency data acquisition and
processing approaches for seismic in applications of sub-salt and
sub-basalt exploration.
Much of the research was done during 2002-2010 by a team which included
several early career researchers, many of whom now work in the UK
hydrocarbon or commercial sectors (see section 5). Members of the group
working on this project and acting as co-authors on publications have
included: Professor White, (Cambridge academic staff: 1981-present),
Professor McKenzie (Cambridge academic staff 1969-2012), Dr Jon Smallwood
(Cambridge 1993-1997 and later employed by Amerada Hess), Dr Jenny Maresh
(Cambridge 2000-2004), Dr Zoe Lunnon (Cambridge 2001-2005), Dr Lindsey
Smith (Cambridge 2002-2006), Dr Alan Roberts (Cambridge 2002-2008), Dr
Jennifer Eccles (Cambridge 2004-2008), Dr Helen Lau (Cambridge 2006-2009),
Dr Moritz Fliedner (Cambridge 1997-2001), Dr Roman Spitzer (Cambridge
2002-2006). External Collaborators include: Prof N.J.
Kusznir (of Liverpool University, who developed margin subsidence
software), Dr Phil Christie (of Schlumberger Cambridge Research Ltd, who
holds patents connected with this work), Dr B Boslaugh (of Amerada Hess,
who arranged seismic acquisition at sea).
References to the research
Those which best indicate the quality of the underpinning research are
indicated (*)
White, R. S. & McKenzie, D. (1995). Mantle plumes and flood basalts.
Journal of Geophysical Research, 100, 17,543-17,585,
doi:10.1029/95JB01585. [sets out the reasons for massive volcanism on
rifted margins: 292 citations to date]
* Fruehn, J., Fliedner, M. M. & White, R. S. (2001). Integrated
wide-angle and near-vertical subbasalt study using large-aperture seismic
data from the Faeroe-Shetland region. Geophysics, 66, 1340-1348, doi:
10.1190/1.1487079. [results from two-ship profiles which show large
offsets are required for sub-basalt imaging]
White, R. S., Smallwood, J. R., Fliedner, M. M., Boslaugh, B., Maresh, J.
& Fruehn, J. (2003). Imaging and regional distribution of basalt flows
in the Faroe-Shetland Basin. Geophysical Prospecting, 51, 215-231, doi:
10.1046/j.1365-2478.2003.00364.x. [regional application of our
methods, widely used as a base map for exploration]
Maresh, J., White, R. S. Hobbs, R.W. & Smallwood, J.R. (2006).
Seismic attenuation of Atlantic margin basalts: observations and modeling,
Geophysics, 71, B211-B221, doi: 10.1190/1.2335875 [demonstration of
why low frequency sources are required to penetrate basalt flows]
* White, R. S., Smith, L. K., Roberts, A. W., Christie, P. A. F.,
Kusznir, N. J. & iSIMM Team. (2008). Lower-crustal intrusion on the
North Atlantic continental margin, Nature, 452, 460-464 plus supplementary
information at www.nature.com,
doi:10.1038/nature06687 [results from applying methods for deep
sub-basalt imaging]
* Lau, K. W. H., White, R. S. & Christie, P. A. F. (2010).
Integrating streamer and ocean-bottom seismic data for sub-basalt imaging
on the Atlantic Margin, Petroleum Geoscience, 16, 349-366, doi:
10.1144/1354-0793/10-023 [shows benefits for sub-basalt imaging of
combining an academic-developed approach to velocity modelling from OBS
with industry processing]
Peer reviewed grants:1/ (Kusznir, White, Roberts &
Christie) iSIMM: integrated Seismic Imaging and Modelling of Margins (NERC
LINK plus DTI and 8 oil companies) (2001-2005) £1,304,173 + seatime +
Western Geco acquisition (£1.3 million) = £2.6 million total 2/
(Japsen, White, Worthington) Petrophysical and seismic properties of
Faroes basalts (Sindri - a group comprising oil companies working in
Faroes sector) (2002-2005) 10,680,610 DKK (c. £ 1.2M). Other
Grants: (White) P- and S-wave characterisation of subsurface
properties (Schlumberger Cambridge Research Ltd) (2005-2010) £427,500
Details of the impact
The main impact of our research has been the widespread acceptance that
sub-basalt imaging can be greatly improved by a combination of using long
offsets and a low frequency broad-band source. The major beneficiaries
have been oil companies exploring for hydrocarbons in frontier areas such
as the northwest margin of Europe, the Brazilian margin of South America
and the continental margins of India. Approximately 70% of all continental
margins contain significant volcanic flows, so as oil exploration extends
into deeper waters of frontier areas the techniques discussed here have
become increasingly important.
The process by which our research has been disseminated was initially by
presentations at regular one-day meetings with the oil companies who
contributed to the iSIMM project. This gave the participating oil
companies advance knowledge of progress, and thus a commercial edge and
which some incorporated into their exploration programmes. Exchange of
personnel between companies, and the way so many expensive exploration
activities like drilling wells are often joint enterprises, means that a
6-month lead is often all they expect or need to obtain a commercial
advantage. Our results from the Faroes-Shetland Basin were used in the 3rd
Faroes Licensing Round in November 2008 at which companies bid for
exploration rights, and continue to be used by oil companies to help plan
drilling targets. The Director of the Faroese Earth and Energy
Directorate (Jarðfeingi) will verify "that several
companies bidding for exploration rights have applied this approach and
these techniques continue to play an important role in the hydrocarbon
exploration effort in the Faroese region".
The other main route of dissemination to a wider audience was through
presentations at conferences, and particularly those attended by oil
companies. These oral presentations often preceded the formal publication
in international refereed journals, which often took 12 months, and we
typically gave talks on results as fast as they became available. None of
our work was restricted from publication in any way, and we believe that
this led rapidly to its becoming widely known and used. On several
occasions oil companies (specifically Shell, Amerada Hess, Total), having
seen presentations of our results, directed the seismic contractors
acquiring data under contract to use the same parameters as we worked out
for iSIMM. Many other companies have also adopted the same principles we
developed in planning their surveys. Schlumberger
Cambridge Research will attest that this work "motivated
clients to purchase proprietary acquisition by Schlumberger of at least
5,000 line-km of low-frequency, long-offset seismic data in the
basalt-covered regions of the Atlantic Margin" and will provide
evidence of the impact of our work on sub-basalt imaging, the importance
of the patents taken out, and the connection with US Patent 7,961,549,
which was granted on 14 June 2011, describing low frequency data
acquisition and processing approaches for seismic acquisition in areas of
sub-salt and sub- basalt exploration.
The benefits of improved survey design were clear in subsequent surveys
shot by oil companies from 2003 onwards. Since 2008 the long-offset, low
frequency strategy is now widely used as standard in surveys on
volcanically-dominated continental shelves, and new acquisition
technologies continue to be developed to generate and record
low-frequency, broad-band data. Further advances also come in improved
methods of processing, modelling and inverting the data. This is seen
already from the fact that older seismic surveys, albeit with shorter
maximum offsets (typically only 2.4 km) have been reprocessed commercially
by oil companies to bring out the low frequency information, with
noticeable improvement in the sub-basalt image. The Exploration
Team Leader at GDF-Suez will corroborate that "broad-spectrum
seismic sources as developed for sub-basalt imaging by the Cambridge
group and related seismic processing techniques have gone on to be
applied widely across other areas of the UK including the Central North
Sea where the additional frequency content can reduce risk on the
exploration process" and that "Several wildcat exploration wells
costing £50M + have been drilled in areas where the sub-basalt imaging
techniques pioneered by the Cambridge group have been applied, for
example Lagavulin (217/15-1 in 2010/2011)."
The precise financial value of the work is difficult to quantify but the
typical licencing costs for broadband 3D seismic surveys are now in the
range of £10,000 per km2 (with a typical survey being
200-1000km2). It is estimated that over 8,000 km of
low-frequency 2D long-offset data, directly informed by the techniques we
developed, have been acquired on the northwest European continental margin
alone, with revenue of $80 million for the seismic contractors. Worldwide,
the sub-basalt imaging market is much greater with important basins
offshore South America, West Africa, Greenland and India. On land the
Siberian Traps, Karoo, Columbia River and Parana basins have major
sub-basalt prospectivity. The ability to image beneath basalts developed
by this research has led to increased industrial activity to exploit
sub-basalt oil reservoirs.
A further important benefit has been the supply of trained researchers
into industry. Many oil companies tell us that this is of equally great
importance to the research results we obtain. Three out of four postdocs
employed on this research at Cambridge University now work in the
hydrocarbon industry and are still active in sub-basalt research. This has
led to continued interaction between the industry and academics. The oil
companies and contractors have benefitted from the much longer periods of
time and more focussed effort that the academic postgraduate and
postdoctoral researchers are able to devote to a single study, free from
the commercial deadlines in a corporate setting which require industry
workers to move on to other projects. The academic research has benefitted
from access to state-of-the-art seismic acquisition systems owned by oil
company contractors, which are otherwise out of their reach.
Destinations of researchers after they left the Department of Earth
Sciences, Cambridge University: OMV; PriceWaterhouse Coopers; Universities
of Auckland, Cambridge and Durham; Dalhousie; Statoil; BP; GXT;
WesternGeco; 3DGeo; UK Civil Service (Environment).
Sources to corroborate the impact
The impact of this work can be corroborated by: a) The Director of
the Faroese Earth and Energy Directorate (Jarðfeingi), b) the
Exploration Team Leader at GDF-Suez and c) Schlumberger
Cambridge Research.
- Dr Philip Christie, past-President of the European Association of
Geoscientists & Engineers, can corroborate impact and also published
a paper on the benefits of joint academic-industry projects, focusing on
this work: Christie, PAF (2009) A Bumpy Road? European Union Public
Service Review vol. 18, pp 524-527, published by PSCA
International.
- Statoil put out in 2011 an appeal on their web site for innovative
ways to improve sub-basalt imaging: a large number of the references and
illustrations in their background material and presentation were to
research by the Cambridge research group, showing the impact on this
area of work. See: http://innovate.statoil.com/challenges/Pages/Challenge.aspx
-
Patents: "Source signature deconvolution method" by Phil
Christie and Zoe Lunnon, filed as US patent 7,551,515, in 2010 and
as UK Patent Application 29 April 2005, granted as UK patent 2,425,838
on 27 June 2007 are directly derived from this work [Phil Christie is
an industry collaborator at Schlumberger Cambridge Research and Zoë
Lunnon was at Cambridge (2001-2005) and played an active part in the
iSIMM project].