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Paleozoic Petroleum Systems on the NCS – Fake, Fiction Or Reality?
Extended Abstract Paleozoic Petroleum Systems on the NCS – Fake, Fiction or Reality? What is presently Known & What Implications May such Source Rock Systems Have – Today - in terms of Exploration? SWOT Prof. Dr. Dag A. Karlsen, Univ of Oslo The Jurassic source rock systems continue to form the backbone for exploration on the Norwegian Continental Shelf NCS), with hitherto only 5 oil accumulations proven to be from Cretaceous source rocks, and with Triassic source rock contributions mainly occurring in the Barents Sea. At the “other end of the stratigraphy” we have the Paleozoic rocks. Paleozoic source rocks were recognized early in Scandinavia, e.g. the Alum shale, which we today know to have generated petroleum during the Caledonian Orogeny (Foreland Basin), bitumen found now in odd-ball places in Sweden e.g. at Østerplane and at the Silje Crater Lake and also in Norway. It took until 1995 until we could, via geochemical analytical work on migrated bitumen from the Helgeland Basin (6609/11-1), with some certainty point to migrated oil from a possible Devonian source (affinity to Beatrice & the Orkney shales). Also around 1995, we could suggest bitumen from the 7120/2-1, later realized as one of the wells in the Alta Discovery v.200m dolomite Ørn/Falk Fm) to be of a non-Mesozoic origin, and possibly from a Paleozoic source, and geologist at RWE-Dea and later Lundin started to consider the Paleozoic reservoir systems at Loppa High and also the possibility of Triassic and Permian source rocks as a play model. Why did it take the scientific and exploration environment in Norway so long time to consider source rock systems outside the Jurassic as important? Part of the reason is the great success of the Jurassic Plays on the NCS. -
Proceedings of the Ussher Society
Proceedings of the Ussher Society Research into the geology and geomorphology of south-west England Volume 6 Part 3 1986 Edited by G.M Power The Ussher Society Objects: To promote research into the geology and geomorphology of south- west England and the surrounding marine areas; to hold Annual Conferences at various places in South West England where those engaged in this research can meet formally to hear original contributions and progress reports and informally to effect personal contacts; to publish, proceedings of such Conferences or any other work which the Officers of the Society may deem suitable. Officers: Chairman Dr. C.T. Scrutton Vice-Chairman Dr. E. B. Selwood Secretary Mr M.C. George Treasurer Mr R.C. Scrivener Editor Dr. G.M. Power Committee Members Dr G. Warrington Mr. C. R. Morey Mr. C.D.N. Tubb Mr. C. Cornford Mr D. Tucker Membership of the Ussher Society is open to all on written application to the Secretary and payment of the subscription due on January lst each year. Back numbers may be purchased from the Secretary to whom correspondence should be directed at the following address: Mr M. C. George, Department of Geology, University of Exeter, North Park Road, Exeter, Devon EX4 4QE Proceedings of the Ussher Society Volume 6 Part 3 1986 Edited by G.M. Power Crediton, 1986 © Ussher Society ISSN 0566-3954 1986 Typeset, printed and bound bv Phillips & Co., The Kyrtonia Press, 115 High Street, Crediton, Devon EXl73LG Set in Baskerville and Printed by Photolithography Proceedings of the Ussher Society Volume 6, Part 3, 1986 Papers D.L. -
Structural and Stratigraphic Evolution of the Mid North Sea High Region of the UK Continental Shelf
Downloaded from http://pg.lyellcollection.org/ by guest on March 31, 2020 Accepted Manuscript Petroleum Geoscience Structural and Stratigraphic Evolution of the Mid North Sea High Region of the UK Continental Shelf Rachel E. Brackenridge, John R. Underhill, Rachel Jamieson & Andrew Bell DOI: https://doi.org/10.1144/petgeo2019-076 This article is part of the Under-explored plays and frontier basins of the UK continental shelf collection available at: https://www.lyellcollection.org/cc/under-explored-plays-and-frontier-basins- of-the-uk-continental-shelf Received 30 May 2019 Revised 25 November 2019 Accepted 23 January 2020 © 2020 The Author(s). This is an Open Access article distributed under the terms of the Creative Commons Attribution 4.0 License (http://creativecommons.org/licenses/by/4.0/). Published by The Geological Society of London for GSL and EAGE. Publishing disclaimer: www.geolsoc.org.uk/pub_ethics To cite this article, please follow the guidance at https://www.geolsoc.org.uk/~/media/Files/GSL/shared/pdfs/Publications/AuthorInfo_Text.pdf?la=en Manuscript version: Accepted Manuscript This is a PDF of an unedited manuscript that has been accepted for publication. The manuscript will undergo copyediting, typesetting and correction before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain. Although reasonable efforts have been made to obtain all necessary permissions from third parties to include their copyrighted content within this article, their full citation and copyright line may not be present in this Accepted Manuscript version. -
North Sea Geology
Technical Report TR_008 Technical report produced for Strategic Environmental Assessment – SEA2 NORTH SEA GEOLOGY Produced by BGS, August 2001 © Crown copyright TR_008.doc Strategic Environmental Assessment - SEA2 Technical Report 008 - Geology NORTH SEA GEOLOGY Contributors: Text: Peter Balson, Andrew Butcher, Richard Holmes, Howard Johnson, Melinda Lewis, Roger Musson Drafting: Paul Henni, Sheila Jones, Paul Leppage, Jim Rayner, Graham Tuggey British Geological Survey CONTENTS Summary...............................................................................................................................3 1. Geological history and petroleum geology including specific SEA2 areas ......................5 1.1 Northern and central North Sea...............................................................................5 1.1.1 Geological history ........................................................................................5 1.1.1.1 Palaeozoic ....................................................................................5 1.1.1.2 Mesozoic ......................................................................................5 1.1.1.3 Cenozoic.......................................................................................8 1.1.2 Petroleum geology.......................................................................................9 1.1.3 Petroleum geology of SEA2 Area 3 .............................................................9 1.2 Southern North Sea...............................................................................................10 -
Dinantian Carbonate Development and Related Prospectivity of the Onshore Northern Netherlands
Dinantian carbonate development and related prospectivity of the onshore Northern Netherlands Nynke Hoornveld, 2013 Author: Nynke Hoornveld Supervisors: Bastiaan Jaarsma, EBN Utrecht Prof. Dr. Jan de Jager, VU University Amsterdam Master Thesis: Solid Earth, (450199 and 450149) 39 ECTS. VU University Amsterdam 01-06-2013 Dinantian carbonate development and related prospectivity of the onshore Northern Netherlands Nynke Hoornveld, 2013 Contents Contents……………………………………………………………………………………………………………………………………………..2 Abstract…………………………………………………………………………………………….………………………………………………..3 Introduction…………………………………………………………………………………………………………….…………………….……4 Geological History of the Netherlands relating to Dinantian development…………………………..……………..7 Tectonic history…………………………………………………………………………………………………………………………..9 Stratigraphy of the Carboniferous…………………………………………………………………………………………….16 Stratigraphic Nomenclature of the Netherlands……………………………………………………………….………23 Methods……………………………………………………………………………………………………………………………………….…..26 Seismic interpretation…………………………………………………………………………………………………………….…27 Time-depth conversion…………………………………………………………………………………………………….……...35 Well correlation……………………………………………………………………………………………………………………..…38 Carbonate production, precipitation and geometries, with a focus on the Dinantian……….………40 Results………………………………………………………………………………………………………………………………….…………..57 Well information, evaluation and reservoir development………………………………………………………..58 Geometry of the Dinantian carbonate build-ups in the Dutch Northern onshore…………..……….75 The geological history -
Master's Thesis
Faculty of Science and Technology MASTER’S THESIS Study program/ Specialization: Spring semester, 2013 Industrial Economics/ Project Management and Risk Management Open access Writer: Sunniva Landmark Bjørnstad ………………………………………… (Writer’s signature) Faculty supervisor: Roy Endré Dahl External supervisor: Johan Magne Sollie, Statoil ASA Title of thesis: Pricing and Risk Management of Spread Options on Brent and West Texas Intermediate Oil Futures Markets Credits (ECTS): 30 Key words: Oil Futures Markets, Spread Options, Pages: 108 Monte Carlo Simulations, Option Pricing, Delta Hedging + enclosure: 8 Stavanger, June 13th 2013 Front page for master thesis Faculty of Science and Technology Decision made by the Dean October 30th 2009 Pricing and Risk Management of Spread Options on Brent and West Texas Intermediate Oil Futures Markets Sunniva Landmark Bjørnstad June 13, 2013 Abstract This thesis investigates the price spread between futures on Brent oil from the Intercontinental Exchange and West Texas Intermediate oil from the New York Mercantile Exchange. Historical futures data is calibrated to a multi-factor forward curve model based on Clewlow and Strickland (2000), and the model is fitted, based on Sollie (2013)'s approach, to al- low for non-constant volatility. An asymmetric generalized autoregressive heteroskedastic model based on Nelson (1991), and principal component analysis is performed to find key common factor explaining the forward curve dynamics. The model is used to draw realisations of the forward curves for Brent and West Texas Intermediate (WTI) crude oils, and three selected realisations are further analysed. Sensitivity analysis is performed on the expected prices at Day 1, and options are priced on the Brent/WTI futures spread with Monte Carlo Simulations. -
A Deep-Dive Into the Ocean
360 Report $CompanySectorName$ $StoryName$$ReportType$ Blue Economy Screener Thematic & Impact Investing 31 March 2017 A deep-dive into the Ocean What’s it all about? Our in-depth assessment of the decline in ocean health shows that the tides are turning. The sectors that most jeopardise the resources provided by the sea, such as shipping, wild-catch fisheries, and offshore oil & gas, face mounting pressure to shift their model towards a more sustainable Main author trajectory, which results in a new wave of risks and opportunities, paving Samuel Mary the way to a potential recovery. Our blue economy framework looks to ESG Research identify the best practices among fast-growing ocean-related industries [email protected] and likely winners and losers across our universe. Offshore-wind, +44 207 621 5190 aquaculture and ship-equipment plays are well placed to provide resource- efficient and climate-friendly solutions, while emerging themes such as ESG research team the reduction of plastic pollution are gathering steam. Biographies at the end of the report IMPORTANT. Please refer to the last page of this report for keplercheuvreux.com “Important disclosures” and analyst(s) certifications. This research is the product of Kepler Cheuvreux, which is authorised and regulated by the Autorité des Marché Financiers in France. Thematic & Impact Investing 360 in 1 minute A sea change for the ocean The swift rise of innovation-driven and renewable resource-based sectors, such as offshore wind and aquaculture, coincides with a policy clampdown on the negative environmental impact of ocean-based industries, such as seaborne trade and wild-catch fisheries. -
Copyright by Sandra Milena Wiegand 2011
Copyright by Sandra Milena Wiegand 2011 The Thesis Committee for Sandra Milena Wiegand Certifies that this is the approved version of the following thesis: An Analysis to the Main Economic Drivers for Offshore Wells Abandonment and Facilities Decommissioning APPROVED BY SUPERVISING COMMITTEE: Supervisor: Steve Nichols Manas Gupta An Analysis to the Main Economic Drivers for Offshore Wells Abandonment and Facilities Decommissioning by Sandra Milena Wiegand, B.S. Thesis Presented to the Faculty of the Graduate School of The University of Texas at Austin in Partial Fulfillment of the Requirements for the Degree of Master of Science in Engineering The University of Texas at Austin August 2011 Dedication This thesis is dedicated to the two most important people in my life: my wonderful father, Hugo Torres and my dear husband, Michael Wiegand. To my father who taught me the meaning of unconditional love. Thank you for giving me the best you had and helping me succeed in life and instilling in me the confidence that I am capable of doing anything I put my mind to. I love you Daddy !. And to my husband, my soul mate and confidant, for always being there for me. Thank you for you endless love, support and patience as I went through this journey. I could not have made it through without you by my side. Acknowledgements I would like to express my gratitude to the following people: Dr. Robert Duvic, for his guidance throughout the first stage of my thesis process. To Dr. Farid Shecaira and Mr. Dalmo Barros for all their support as my managers during these last two years. -
The Quaternary Geology of the North Sea Basin
The Quaternary geology of the North Sea basin Emrys Phillips 1, David M. Hodgson 2 and Andy R. Emery 2 1. British Geological Survey, The Lyell Centre, Research Avenue South, Edinburgh EH14 4AP, UK ([email protected]) 2. School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK ([email protected]) Introduction – the Quaternary of the North Sea basin and its importance The North Sea is a shallow (~50 to 400 m deep), ~500 km wide marine embayment that separates the UK from Scandinavia and northern Europe (Figure 1). This epicontinental shelf area has had a long and complex geological history with its present‐day structural configuration largely being the result of rifting during the Jurassic–Early Cretaceous, followed by thermal subsidence (Glennie and Underhill, 1998; Zanella and Coward, 2003). Since the middle Cenozoic, the Central Graben region of the North Sea Basin has accumulated up to 3000 m of Oligocene to Holocene sediments, which locally includes more than 800 m of Quaternary sediments (Caston, 1977, 1979; Gatliff et al., 1994). Although a detailed understanding of the depositional history recorded by this sedimentary succession is yet to be fully established, these sediments preserve evidence for the advance and retreat of several ice sheets into the North Sea from the adjacent landmasses at different times during the Quaternary. These ice masses not only resulted in periodic erosion, but also made a significant depositional contribution to the infill of the basin. The traditional view of the Quaternary (Pleistocene) -
Palaeozoic Petroleum Systems of the Central North Sea/Mid North Sea High
CR/15/124; Draft 0.1 Last modified: 2016/03/30 17:22 Palaeozoic Petroleum Systems of the Central North Sea/Mid North Sea High Energy and Marine Geoscience Programme Commissioned Report CR/15/124 CR/15/124; Draft 0.1 Last modified: 2016/03/30 17:22 BRITISH GEOLOGICAL SURVEY ENERGY AND MARINE GEOSCIENCE PROGRAMME COMMISSIONED REPORT CR/15/124 Palaeozoic Petroleum Systems of the Central North Sea/Mid North Sea High A A Monaghan & S. Arsenikos, E Callaghan, R Ellen, C Gent, S The National Grid and other Hannis, A Henderson, G Leslie, K Johnson, M Kassyk, T Kearsey, Ordnance Survey data © Crown Copyright and database rights A Kim, G Kimbell, M Quinn, W McLean, D Millward, T Pharaoh, 2015. Ordnance Survey Licence M Sankey, N Smith, C Ugana, C Vane, C Vincent, P Williamson No. 100021290 EUL. Keywords Palaeozoic; CNS, petroleum systems. Front cover Core from well 43/17- 2 at 3170 m in sandstone and mudstone of the Millstone Grit Formation. BGS©NERC. All Rights Reserved 2016 Bibliographical reference MONAGHAN A A AND THE PROJECT TEAM. 2015. Palaeozoic Petroleum Systems of the Central North Sea/Mid North Sea High. British Geological Survey Commissioned Report, CR/15/124. 105pp. Copyright in materials derived from the British Geological Survey’s work is owned by the Natural Environment Research Council (NERC) and/or the authority that commissioned the work. You may not copy or adapt this publication without first obtaining permission. Contact the BGS Intellectual Property Rights Section, British Geological Survey, Keyworth, e-mail [email protected]. You may quote extracts of a reasonable length without prior permission, provided a full acknowledgement is given of the source of the extract. -
Worldwide Oil and Gas Platform Decommissioning: a Review of Practices and T Reefing Options ∗ Ann Scarborough Bull , Milton S
Ocean and Coastal Management 168 (2019) 274–306 Contents lists available at ScienceDirect Ocean and Coastal Management journal homepage: www.elsevier.com/locate/ocecoaman Worldwide oil and gas platform decommissioning: A review of practices and T reefing options ∗ Ann Scarborough Bull , Milton S. Love Marine Science Institute, University of California, Santa Barbara, CA, 93016, USA ARTICLE INFO ABSTRACT Keywords: Consideration of whether to completely remove an oil and gas production platform from the seafloor or to leave Decommissioning the submerged jacket as a reef is an imminent decision for California, as a number of offshore platforms in both Offshore platforms state and federal waters are in the early stages of decommissioning. Laws require that a platform at the end of its Rigs-to-reefs production life be totally removed unless the submerged jacket section continues as a reef under state spon- Artificial reefs sorship. Consideration of the eventual fate of the populations of fishes and invertebrates beneath platforms has led to global reefing of the jacket portion of platforms instead of removal at the time of decommissioning. The construction and use of artificial reefs are centuries old and global in nature using a great variety ofmaterials. The history that led to the reefing option for platforms begins in the mid-20th century in an effort forgeneral artificial reefs to provide both fishing opportunities and increase fisheries production for a burgeoning U.S. population. The trend toward reefing platforms at end of their lives followed after the oil and gas industry installed thousands of standing platforms in the Gulf of Mexico where they had become popular fishing desti- nations. -
Salt-Influenced Normal Faulting Related to Salt-Dissolution And
SALT-INFLUENCED NORMAL FAULTING RELATED TO SALT-DISSOLUTION AND EXTENSIONAL TECTONICS: 3D SEISMIC ANALYSIS AND 2D NUMERICAL MODELING OF THE SALT VALLEY SALT WALL, UTAH AND DANISH CENTRAL GRABEN, NORTH SEA by Mohammad Naqi Copyright by Mohammad Naqi 2016 All Rights Reserved i A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Doctor of Philosophy (Geology). Golden, Colorado Date _________________________ Signed: _______________________ Mohammad Naqi Signed: _______________________ Dr. Bruce Trudgill Thesis Advisor Golden, Colorado Date _________________________ Signed: _______________________ Dr. M. Stephen Enders Professor and Department Head Department of Geology and Geological Engineering ii ABSTRACT The northeastern Paradox basin is characterized by a series of salt cored anticlines (salt walls) trending NW-SE. The crestal areas of the salt cored anticlines are breached and cut by faults, forming downthrown valleys, created by the subsidence of the crestal overburden. There has been a prolonged debate on the causative mechanism of subsidence of the anticline crests. Some researchers, based on field observations favor salt-dissolution of the salt forming the core of the anticlines as the main mechanism for the crestal subsidence. Others based on physical modeling favor extensional tectonics as the main mechanism that triggered subsidence. A wider variety of salt structural styles are present in the Danish Salt Dome Province of the Danish Central Graben, ranging from salt diapirs that penetrate their overlying sedimentary cover, to gentle, non-penetrating salt-cored anticlines. Salt structures present as pillows (e.g. the Kraka salt pillow), diapirs (e.g.