Back Matter (PDF)

Total Page:16

File Type:pdf, Size:1020Kb

Back Matter (PDF) Index Page numbers in italics refer to Figures. Page numbers in bold refer to Tables. Achmelvich Field 26, 27, 28 Andrew Formation 9, 11 Bacton Group 193, 220, 285 Acorn Field 10, 349 Lomond Field 511 Bacton Terminal 119, 120 cross-section 351 Moira Field 875 Bains Field 321, 322, 335 database 353 Morag Field 898 location map 308 development 349 Andrew Sandstone Member 10 Balder Formation 12 exploration history 349 Alba Field 639, 639 Catcher Field 399, 408 location map 350 Merganser Field 600 Chestnut 416 porosity v. permeability 356 Renee Field 779 Donan Field 724 production history and resources Rubie Field 790, 792, 793, 794, 796 Gryphon area fields 841, 842, 843 356–357 Shearwater satellites 592 Howe and Bardolino fields 471, 473 regional context 349–352 Stella Field 609, 610, 611, 612, 613, 614 Mariner Field 889 reservoir and petrophysics 353–355 Angus Field 489, 490 Rubie Field 793, 795, 797 seismic data 353 Ann Field 21 Tullich Field 837 stratigraphy 351 Ansdell Mudstone Member 309, 312, 324 Balek Field 658–662 summary 358 Apollo Field 262 Ballindalloch Field trap 353 Appleby Group 64, 324 development 839 Agar Field 863 Appleton Field 489 exploration history and appraisal 837–838 Alba Field 10, 637, 664, 718 Arbroath Field 21, 391 location map 838 core photographs 644 location map 480 summary 848 database 640–643 Ardmore Field 4, 11, 489, 490, 899 Balloch Field 11, 717 development plan 637 see also Alma Field cross-section 718 exploration history and appraisal 637 Argyll Field 4, 11, 21, 23, 360, 489, 490, development 724 location map 638, 665 491, 492, 899 exploration history and appraisal 720 porosity–permeability 646 chronostratigraphy 491 location map 718 production history and reserves see also Alma Field production history and reserves 645–649, 646 Arkwright Field 391 735–737, 736 regional context 639 location map 480 regional context 724–725 reservoir and petrophysics 643–645 Artemis Field 262 reservoir and petrophysics 731–733 seismic section 638, 641, 647 Arundel Field 448 seismic line 728 stratigraphy 638 Athena Field 768 summary 737–738 summary 649 Atlantic Field 652, 668, 740 well correlation 732 trap 639–640 Atlantic Margin fields 12–13 Balmoral Field 12, 718 Alba Sands 637 Auk Field 23, 489, 490, 899 Balmoral Sandstone 793 Alba Field 639 Auk Formation Donan Field 718, 726 Albury Field 75 Alma Field 362, 362, 364 Lochranza Field 715 Albuskjell Field 489 facies associations 493 MacCulloch Field 729 Alder Field 664, 665, 680 Morag Field 898 Balmoral Tuffite 793, 798 Aller Halite Formation 152, 220 porosity/permeability 367 Banff Sub-Basin 652 Alligin Field 23, 980 reservoir properties 494 Banquo accumulation 916, 917 Alma (formerly Argyll/Ardmore) Field 4, Austen Field 383 Bardolino Field 10 11, 489, 490, 899 Austrian Orogeny 665, 666 compartmentalization 477 database 365–366 Aviat Field 479, 479 database 469 exploration history 360–361 location map 413, 480 development 468, 474 location 360, 361 Avington Field 75 exploration history 468 production history and reserves location map 469, 480 368, 368 Babbage Field 8 production history 476–477 regional context 361–362 database 108 regional context 468–469 reservoirs 366–368 seismic data 108–109 reservoir and petrophysics 469, 471–472 stratigraphy 362, 365 seismic sections 112 seismic section 475 structure 361–362 wells 108 structural elements 471, 475 summary 369–370 development 98 summary 478 well correlations 363, 364 exploration history 97–98 trap 472 Alpha Field 479, 479 map 97 Barque Field 21 Alpine faults 229 porosity/permeability data 106 Barra Field 25, 907 Alpine Orogeny 124, 194, 290, 336 production history and reserves Basalanhydrite Formation 124, 193, 220 diapir growth 593 106–107, 107 Base Cretaceous Unconformity (BCU) 375, Alpine Orogeny inversion 277 regional context 98–100 377, 420, 740, 797 Alton Sandstone 133, 135, 139 reservoir and petrophysics 102–105 Acorn/Beechnut Field 352, 430 Alvheim Field 838, 863 reservoir pressure 106 Buchan Field 684 Alwyn Field 12, 863 stratigraphy 105 Dunlin Field 819 Amethyst East Field 218 summary 107–108 Edradour Field 953 Amethyst Field 218 trap 101–102 Gryphon area fields 841 Amethyst West Field 218 well correlation 99 Hutton Field 854 Andrew Field 668 Bacchus Field 470, 479, 479 Jura discovery 720 location map 413 location map 413, 480 Maria Field 879 1064 INDEX Base Cretaceous Unconformity (BCU) Blane Field 10, 12, 382 Brenda Field 718 (Continued) database 383 Brent Field 9, 21, 815 Penguins cluster 910, 921 development 382 location map 851, 917 Perth Field 774 exploration history 382 Brent Formation 19 Wood, Cayley, Godwin, Shaw fields 618, location map 383 Brent Group 12, 816 620 oil–water contact 383–384 Dunlin Cluster 820, 822, 823 Base Ketch Unconformity (BKU) 152 porosity v. permeability 387 Hutton Field 850, 852, 852, 853 Base Permian Unconformity (BPU) 8, 86, production history and reserves Pelican Field 906, 907, 907, 908, 909, 158, 231, 263, 264, 266, 292 386–388, 388 909, 910, 913 depth map 242, 244 regional context 382 Penguins cluster 916, 918, 919, 922, 922, Base Quaternary Unconformity 339, 340 reservoir and petrophysics 384–386 923, 924 Beaconhill Flags 57, 58 seismic section 385 Brent Province 11 Beauly Field 12, 718 stratigraphy 384 Brent Sandstone 814 Beauly Formation, Gryphon area fields 841 summary 389 Brent Spar 24, 26 Beechnut Field 10 trap 383 Bressay Field 863 reservoir and petrophysics 355–356 well correlations 387 Bressay granite 868, 869 summary 358–359 Blenheim Field 718 Brigg–Glandford–Broughton High 55 well correlations 357 Bleo Holm 651 Brimmond Field 479, 479 Bel Air well 27 Bletchingley Field 75 Britannia Field 11, 664, 668, 718 Bentley Field 863 Block 6 Field 814, 815 Aptian palaeogeography 670 Beryl Embayment Bluebeard Field 863 database 666–668 palaeogeography of Paleocene 843 Blythe Field 21 development 664 stratigraphy 840 Boa Field 863 exploration history and appraisal 665 structural map 840 Boatswain Field 863 location map 413, 652, 665, 680 turbidity currents 843 Bosun Field 664, 665, 668 porosity–permeability 672 Beryl Field 838, 863 Bothamsall Field 45 production facilities 666 Big Dotty Field 189, 191, 198 Bottlenose Field 560 production history and reserves 675–677, location map 189, 203 Boulby Formation 84 675, 676 see also Little Dotty Field Boulby Mine 899 regional context 664–666 Billingham Formation 84 Boulton Field reservoir and petrophysics 670, Birch Field 718 location map 226 672–673, 675 Birgitta (Fiddich) Field 10, 371 stratigraphy 227 seismic section 670, 671 database 375 Bowhead Field 560 source rock 666 development 371 Bowland Basin 64, 64 stratigraphy 667 exploration history 371 Bowland Shale Formation summary 677–678 location map 371, 391 Douglas Field 309 top reservoir depth map 665 regional context 371–372, 374–375 Elswick Field 62, 66 trap 668, 670 reservoir and petrophysics 376–379, 376 Hewett Field 192 well correlations 674 resources 379–380 Kilmar Field 245 well log 669 seismic section 374 Bowmore Field 768 Britannia Sandstone Formation 670 stratigraphy 373 Boyle Field 838 British Gas 23 summary 380–381 Braemar Field 838 British Gas Corporation 23 trap 375–376 Bravo Field 479, 479 British National Oil Corporation 22, 23 Bittern Sandstone Member, Catcher Field Breagh Field 7, 8, 22 Britoil 23 399, 400 database 113–114 Brockelschiefer Member 193, 220 Black Sail Member 953, 955 development 111–112 Brockham Field 75 Edradour Field 954, 955 exploration history 109–111 Brodgar Field 652, 668, 680 Blackpool Mudstone 324 introduction 109 location map 665 Bladon Field 718 map 110, 112 Brooks, John R.V. ix Blair Field 718 porosity–permeability plots 115 Broom Field 815 Blake Field (Blake Channel & Blake Flank) production history and reserves location map 851 11, 651, 668 115–116, 116 Broom Formation cross-section 657 regional context 112 Dunlin Cluster 823 database 654–655 reservoir and petrophysics 114–115 Pelican Field 910 development 651 seismic section 113 Penguins cluster 918 exploration history and appraisal 651 stratigraphy 111 Brotherton Formation 84 location map 652, 706 summary 116–117 Bruce Field 863 regional context 651–654 trap 114 Buchan Field 652, 679, 794 reservoir and petrophysics 656–658 well correlation 114 database 682–683 seismic line 656 well logs 113 development 681 stratigraphy 654, 655 Brechin Field 10, 390 exploration history 679, 681 structure map 652 database 392 fault framework 687 summary 662–663 development 390 location map 680 trap 568, 655–656 exploration history 390 porosity–permeability 687 well logs 659 location map 391, 480 production history and reserves Blakeney Field 10 porosity v. permeability 395 688–689, 688 database 564 production history and reserves regional context 681–682 exploration history 561 396, 397 reservoir and petrophysics 683–688, location map 560 regional context 391–392 686 reservoir and petrophysics 569–570 reservoir and petrophysics 392–394, 396 seismic section 684 seal 564 seismic section 393 stratigraphy 682, 685 stratigraphy 563 summary 397–398 summary 689–690 summary 571–572 thin sections 395 top reservoir map 680 trap 564 trap 392 trap 683 INDEX 1065 Buchan Formation 10 Caister Coal Formation 133, 151, 152, exploration history 399–401 Alma Field 360, 361, 362, 362, 363 152, 158 location map 400 Buchan Field 679 Kilmar Field 245 porosity v. permeability data 409 images 365 Wingate Field 288, 291, 294 production history and reserves 409–410 porosity/permeability 367 Caister Field 226 regional context 401–403 reservoir properties 366–367 Calder Field 321, 322, 335 reservoir and petrophysics
Recommended publications
  • 3-D Bedrock Geology Model of the Permo-Triassic of Yorkshire and East Midlands
    3-D Bedrock geology model of the Permo-Triassic of Yorkshire and East Midlands Geology and Landscape Southern Britain Programme Internal Report CR/06/091 BRITISH GEOLOGICAL SURVEY GEOLOGY AND LANDSCAPE SOUTHERN BRITAIN PROGRAMME INTERNAL REPORT CR/06/091 The National Grid and other Ordnance Survey data are used with the permission of the 3-D Bedrock geology model of Controller of Her Majesty’s Stationery Office. Licence No: 100017897/2006. the Permo-Triassic of Yorkshire Keywords and East Midlands Report; 3-D Model; Sherwood Sandstone Group; Mercia Mudstone Group; Sneinton Formation; Permian; Roxby Formation; Brotherton Ford, J., Napier, B., Cooper, A., Pharaoh, T., Vincent, C., Carney, Formation; Edlington Formation; J., Thorpe, S., Brayson, J. Cadeby Formation; Yellow Sands Formation; Basal Permian Breccia; Aquifer;. Front cover Model output showing faulted elevation grid for the base Sherwood Sandstone Group and the thickness of the Sherwood Sandstone Group Bibliographical reference FORD, J., NAPIER, B., COOPER, A., PHARAOH, T., VINCENT, C., CARNEY, J., THORPE, S., BRAYSON, J.. 2005. 3-D Bedrock geology model of the Permo-Triassic of Yorkshire and East Midlands. British Geological Survey Internal Report, CR/06/091. 39pp. 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.
    [Show full text]
  • Developing a Geological Framework
    21/2/12 GeolFrameworkPaper_postreview_v2acceptchanges_editorcomments New insights from 3D geological models at analogue CO2 storage sites in Lincolnshire and eastern Scotland, UK. Alison Monaghan1*, Jonathan Ford2, Antoni Milodowski2, David McInroy1, Timothy Pharaoh2, Jeremy Rushton2, Mike Browne1, Anthony Cooper2, Andrew Hulbert2 and Bruce Napier2 1 British Geological Survey, Murchison House, West Mains Road, Edinburgh, EH9 3LA, UK. 2 British Geological Survey, Kingsley Dunham Centre, Keyworth, Nottingham, NG12 5GG, UK. * Corresponding author (email [email protected] (Approx.15,600 words in total, 25 figures) SUMMARY: Subsurface 3D geological models of aquifer and seal rock systems from two contrasting analogue sites have been created as the first step in an investigation into methodologies for geological storage of carbon dioxide in saline aquifers. Development of the models illustrates the utility of an integrated approach using digital techniques and expert geological knowledge to further geological understanding. The models visualize a faulted, gently dipping Permo-Triassic succession in Lincolnshire and a complex faulted and folded Devono-Carboniferous succession in eastern Scotland. The Permo-Triassic is present in the Lincolnshire model to depths of -2 km OD, and includes the aquifers of the Sherwood Sandstone and Rotliegendes groups. Model-derived thickness maps test and refine Permian palaeogeography, such as the location of a carbonate reef and its associated seaward slope, and the identification of aeolian dunes. Analysis of borehole core samples established average 2D porosity values for the Rotliegendes (16%) and Sherwood Sandstone (20%) groups, and the Zechstein (5%) and Mercia Mudstone (<10%) groups, which are favourable for aquifer and seal units respectively. Core sample analysis has revealed a complex but well understood diagenetic history.
    [Show full text]
  • Devonian and Carboniferous Stratigraphical Correlation and Interpretation in the East Irish
    CR/16/040 Last modified: 2016/05/30 11:40 Carboniferous stratigraphical correlation and interpretation in the Irish Sea Energy and Marine Geoscience Programme Commissioned Report CR/16/040 CR/16/040 Last modified: 2016/05/30 11:40 BRITISH GEOLOGICAL SURVEY ENERGY AND MARINE GEOSCIENCE PROGRAMME COMMISSIONED REPORT CR/16/040 Carboniferous stratigraphical correlation and interpretation The National Grid and other Ordnance Survey data © Crown Copyright and database rights in the Irish Sea 2015. Ordnance Survey Licence No. 100021290 EUL. Keywords O. Wakefield, C. N. Waters and N. J. P Smith Report; Stratigraphy, Carboniferous, East Irish Sea. Front cover View of the Great Orme, Llandudno, North Wales, comprising thick carbonate platform successions typical of the Carboniferous Limestone Supergroup of the Irish Sea and adjacent areas (P007274). ©BGS NERC Bibliographical reference Wakefield, O. Waters, C.N. and Smith, N.J.P. 2016. Carboniferous stratigraphical correlation and interpretation in the Irish Sea. British Geological Survey Commissioned Report, CR/16/040. 82pp. 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
    [Show full text]
  • Garforth and Church Fenton
    High Speed Two Phase 2b ww.hs2.org.uk October 2018 Working Draft Environmental Statement High Speed Rail (Crewe to Manchester and West Midlands to Leeds) Working Draft Environmental Statement Volume 2: Community Area report | Volume 2 | LA16 LA16: Garforth and Church Fenton High Speed Two (HS2) Limited Two Snowhill, Snow Hill Queensway, Birmingham B4 6GA Freephone: 08081 434 434 Minicom: 08081 456 472 Email: [email protected] H27 hs2.org.uk October 2018 High Speed Rail (Crewe to Manchester and West Midlands to Leeds) Working Draft Environmental Statement Volume 2: Community Area report LA16: Garforth and Church Fenton H27 hs2.org.uk High Speed Two (HS2) Limited has been tasked by the Department for Transport (DfT) with managing the delivery of a new national high speed rail network. It is a non-departmental public body wholly owned by the DfT. High Speed Two (HS2) Limited, Two Snowhill Snow Hill Queensway Birmingham B4 6GA Telephone: 08081 434 434 General email enquiries: [email protected] Website: www.hs2.org.uk A report prepared for High Speed Two (HS2) Limited: High Speed Two (HS2) Limited has actively considered the needs of blind and partially sighted people in accessing this document. The text will be made available in full on the HS2 website. The text may be freely downloaded and translated by individuals or organisations for conversion into other accessible formats. If you have other needs in this regard please contact High Speed Two (HS2) Limited. © High Speed Two (HS2) Limited, 2018, except where otherwise stated. Copyright in the typographical arrangement rests with High Speed Two (HS2) Limited.
    [Show full text]
  • 1. Ripon, a City of Just Under 17,000 People, Is 54 Degrees N and 1.5 Degrees West and Sits Near to the Northern End of the Sout
    RIPON CITY PLAN Supporting Document: Sustainable Ripon Appendix A.n: Ripon’s Geodiversity Introduction 1. Ripon, a city of just under 17,000 people, is 54 degrees N and 1.5 degrees west and sits near to the northern end of the Southern Magnesian Limestone National Character Area (NCA 30) defined by the underlying Permian Zechstein Group, formerly known as the Magnesian Limestone. It creates a very long and thin area stretching from Thornborough in North Yorkshire to the outskirts of Nottingham. The limestones, marls and enclosed gypsum horizons create a ridge, or narrow belt of elevated land, running north–south and forming a prominent landscape feature. The geology has influenced the form of the landscape, the use of limestone for local building stone and mortar, the specialised limestone grasslands, and in Ripon’s case, and the villages to the north and south, produces unstable land and a particular topography that has defined its settlement history and has geographically limited development. 2. The key to the unique landscape and development of the settlement of Ripon is its geodiversity, defined as earth materials, landforms and processes that shape the Earth. The geodiversity is manifested as the rocks, minerals, soils, topography, rivers and landscape of the area. Ripon sits at 30m above sea level on fluvio-glacial and river terraces that form the higher land between the Ure, Laver and Skell valleys. In the recent past these rivers cut deeply into the underlying Permian deposits, especially to the west of the City, when the flow greatly increased with meltwater from the glaciers of the last Ice Age only 13,000 years ago.
    [Show full text]
  • A Lithostratigraphical Framework for the Carboniferous Successions of Northern Great Britain (Onshore)
    A lithostratigraphical framework for the Carboniferous successions of northern Great Britain (onshore) Research Report RR/10/07 HOW TO NAVIGATE THIS DOCUMENT Bookmarks The main elements of the table of contents are bookmarked enabling direct links to be followed to the principal section headings and sub- headings, figures, plates and tables irrespective of which part of the document the user is viewing. In addition, the report contains links: from the principal section and subsection headings back to the contents page, from each reference to a figure, plate or table directly to the corresponding figure, plate or table, from each figure, plate or table caption to the first place that figure, plate or table is mentioned in the text and from each page number back to the contents page. RETURN TO CONTENTS PAGE BRITISH GEOLOGICAL SURVEY The National Grid and other Ordnance Survey data are used RESEARCH REPOrt RR/10/07 with the permission of the Controller of Her Majesty’s Stationery Office. Licence No: 100017897/2011. Keywords Carboniferous, northern Britain, lithostratigraphy, chronostratigraphy, biostratigraphy. A lithostratigraphical framework Front cover for the Carboniferous successions View of Kae Heughs, Garleton Hills, East Lothian. Showing of northern Great Britain Chadian to Arundian lavas and tuffs of the Garleton Hills Volcanic Formation (Strathclyde Group) (onshore) exposed in a prominent scarp (P001032). Bibliographical reference M T Dean, M A E Browne, C N Waters and J H Powell DEAN, M T, BROWNE, M A E, WATERS, C N, and POWELL, J H. 2011. A lithostratigraphical Contributors: M C Akhurst, S D G Campbell, R A Hughes, E W Johnson, framework for the Carboniferous N S Jones, D J D Lawrence, M McCormac, A A McMillan, D Millward, successions of northern Great Britain (Onshore).
    [Show full text]
  • IAEG2006 Field Trip Guide Ripon 1 GYPSUM DISSOLUTION
    CORE Metadata, citation and similar papers at core.ac.uk Provided by NERC Open Research Archive IAEG2006 Field Trip Guide Ripon GYPSUM DISSOLUTION GEOHAZARDS AT RIPON, NORTH YORKSHIRE, UK Anthony H.Cooper1 1British Geological Survey, Keyworth, Nottingham, NG12 5GG, e-mail:[email protected] Abstract: This guide is for a one-day field excursion to examine gypsum dissolution geohazards at Ripon in North Yorkshire. Gypsum is a highly soluble rock and under suitable groundwater flow conditions it can dissolve forming caves and karstic features including collapse and suffosion dolines. These have the capability of causing subsidence damage of the type that affects much of the Ripon area. The guide details the processes involved, the localities visited and some of the remedial measures undertaken. Résumé: Ce guide concerne l'excursion d'une journée ayant pour but d'étudier les géo-aléas liés à la dissolution du gypse à Ripon dans la région du North Yorkshire. Le gypse est une roche hautement soluble et, dans des conditions adéquates d'écoulement de l'eau souterraine, pouvant se dissoudre et engendrer des grottes et formes karstiques telles qu'effondrements et dolines de suffosion. Celles-ci peuvent causer des dégâts de subsidence du type de ceux qui touchent la plupart des alentours de Ripon. Ce guide fournit des explications sur les phénomènes mis en jeu, les localités visitées et quelques-unes des mesures prises pour remédier à ces problèmes. Keywords: subsidence, evaporites, aquifers, cavities, collapse, urban geosciences. INTRODUCTION Gypsum, hydrated Calcium Sulphate (CaSO4.2H2O), is attractive as satin spar, beautiful as carved alabaster, practical as plasterboard (wallboard), but the cause of a geological hazard capable of swallowing houses and collapsing dams.
    [Show full text]
  • The Stratigraphic Nomenclature of the Irish Offshore Basins
    The Stratigraphic Nomenclature of the Irish Offshore Basins Published by the Department of the Environment, Climate and Communications gov.ie Front cover: Sheet-like basin floor sandstone beds in the Pennsylvanian Ross Sandstone Formation, Loop Head, Co. Clare. The dark, heterogeneous unit in the centre of the picture is a laterally-extensive slump deposit. (Photo: Pat Shannon) Published in Ireland by the Department of the Environment, Climate and Communications 29-31 Adelaide Road Dublin, D02 X285 ____________________________________________________________________ The Stratigraphic Nomenclature of the Irish Offshore Basins Patrick M. Shannon1, Kara L. English2,3 & Michael Hanrahan2, 4 1UCD School of Earth Sciences, University College Dublin, Belfield, Dublin, D04 V1W8, Ireland. 2Petroleum Affairs Division, Department of Communications, Climate Action and Environment, 29-31 Adelaide Road, Dublin, D02 X285, Ireland. 3Present address: Stellar Geoscience, Dublin, and UCD School of Earth Sciences, University College Dublin, Belfield, Dublin, D04 V1W8, Ireland. 4Present address: Geoscience Regulation Office, Department of the Environment, Climate and Communications, 29-31 Adelaide Road, Dublin D02 X285, Ireland. ________________________________________________________________________ Bibliographic reference The Stratigraphic Nomenclature of the Irish Offshore Basins Department of the Environment, Climate and Communications, PAD Special Publication 2/21. Table of Contents 1. INTRODUCTION .............................................................................................................
    [Show full text]
  • BRITISH GEOLOGICAL SURVEY Natural Environment Research Council
    BRITISH GEOLOGICAL SURVEY Natural Environment Research Council -CONFIDENTIAL UNTIL END OF 2005- TECHNICAL REPORT CR/00/94 Revised geological maps of Darlington based on new borehole information: explanation and description A H COOPER & J.GORDON Geographical index UK, County Durham, Darlington Subject index Geology, stratigraphy, boreholes, Permian, gypsum, dissolution, geohazards, subsidence Bibliographic Reference Cooper, A.H & J.Gordon. 2000. Revised geological maps of Darlington based on new borehole information: explanation and description. British Geological Survey Technical Report CR/00/94 ©NERC copyright 2000, Keyworth, British Geological Survey, 2000 SUMMARY The geology of the Darlington area has been revised based on the interpretation of new borehole information and a re-examination of archival data. The Permian Zechstein Group has been mapped through the district where it forms a series of easterly-dipping formations. These strata have been folded and an easterly-plunging syncline, faulted on its southern side, is mapped through the town of Darlington. This fold structure is partially modified by the dissolution of gypsum in the sequence resulting in the partial collapse and foundering of the strata. A series of maps is presented showing the revised geology, rockhead, drift thickness and the thickness of the gypsum sequence present at two horizons; the Hartlepool Anhydrite (present in the Edlington Formation) and the Billingham Anhydrite (present in the Roxby Formation). A series of five structure contour maps are presented
    [Show full text]
  • Triassic: Seasonal Rivers, Dusty Deserts and Saline Lakes
    Triassic: seasonal rivers, dusty deserts and saline lakes Ruffell, A., & Hounslow, M. (2006). Triassic: seasonal rivers, dusty deserts and saline lakes. In P. F. Rawson, & P. Brenchley (Eds.), The Geology of England & Wales. (pp. 295-325). Geological Society of London. Published in: The Geology of England &amp; Wales. Queen's University Belfast - Research Portal: Link to publication record in Queen's University Belfast Research Portal General rights Copyright for the publications made accessible via the Queen's University Belfast Research Portal is retained by the author(s) and / or other copyright owners and it is a condition of accessing these publications that users recognise and abide by the legal requirements associated with these rights. Take down policy The Research Portal is Queen's institutional repository that provides access to Queen's research output. Every effort has been made to ensure that content in the Research Portal does not infringe any person's rights, or applicable UK laws. If you discover content in the Research Portal that you believe breaches copyright or violates any law, please contact [email protected]. Download date:28. Sep. 2021 Triassic: seasonal rivers, 13 dusty deserts and saline lakes M. W. HOUNSLOW & A. H. RUFFELL The collision of Siberia and the Kazakstan microplate with European palaeoenvironmental signatures the eastern side of the Fennoscandia continent in the Permian amalgamated the last major continental fragments to produce The Permian witnessed the fragmentation of the core of the the supercontinent Pangaea, which persisted into the Jurassic Variscan Mountains into a number of separate areas, such as the Armorican, Bohemian and Iberian massifs (Fig.
    [Show full text]
  • BGS Report, Single Column Layout
    Doncaster Geodiversity Assessment Volume 1 – Report Geology and Landscape South Programme Commissioned Report CR/07/025N BRITISH GEOLOGICAL SURVEY GEOLOGY AND LANDSCAPE SOUTH PROGRAMME COMMISSIONED REPORT CR/07/025N Doncaster Geodiversity Assessment Volume 1 – Report S Engering and H F Barron The National Grid and other Ordnance Survey data are used with the permission of the Contributors Controller of Her Majesty’s Stationery Office. Licence No: 100017897/2007. Keywords Geodiversity; Doncaster. Editor Front cover A H Cooper Permian Bryozoan reef, North Cliff Quarry, Doncaster Bibliographical reference ENGERING, S & BARRON, H F. 2007. Doncaster Geodiversity Assessment. British Geological Survey Commissioned Report, CR/07/025N. 139pp. 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. Maps and diagrams in this report use topography based on Ordnance Survey mapping. © NERC 2007. All rights reserved Keyworth, Nottingham British Geological Survey 2007 BRITISH GEOLOGICAL SURVEY The full range of Survey publications is available from the BGS British Geological Survey offices Sales Desks at Nottingham, Edinburgh and London; see contact details below or shop online at www.geologyshop.com Keyworth, Nottingham NG12 5GG The London Information Office also maintains a reference 0115-936 3241 Fax 0115-936 3488 collection of BGS publications including maps for consultation.
    [Show full text]
  • Back Matter (PDF)
    PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY 355 INDEX TO VOLUME 47 prepared by A. S. HOWARD General Index Liesegang rings, origin 42 Boreholes magnetic survey, Tertiary dyke 200ff. Chronostratigraphy metalliferous deposits, mining of 1-2 Lithostratigraphy mica crystallinity, Skiddaw Group 327ff. Localities mineralisation, Northern Pennine Orefield Iff. Minerals molluscs, late Quaternary 127-129 New taxa MOSELEY, F., Sorby medallist 280-281 mylonites, Permo-Carboniferous, Shetland 339ff. Market Weighton anomaly 47ff. GENERAL INDEX Mid North Sea High, late Permian palaeogeography 313ff. Midland Valley, Lower Carboniferous stratigraphy 215ff. 150th Anniversary celebrations 96-102 Moore Medal 281-282 acritarchs, Ordovician 271-274 North Sea, late Permian palaeogeography 313ff. amygdales, Whin Sill 250-251 North Yorkshire, Craven Reef Belt 55ff. Annual Report 1988 277-279 North Yorkshire, Middle Jurassic palynostratigraphy 349ff. aplites, Whin Sill 251 North Yorkshire, Rhaetian 29ff. brachiopods, Lower Carboniferous I3ff., 55ff. North Yorkshire, Westbury Formation 29ff. brachiopods, functional morphology 18-19,59-62 North Yorkshire, field meeting 105-106 brachiopods, palaeoecology 62-63 North-east England, Upper Permian 33ff., 285ff. brachiopods, productoid 13ff., 55ff. North-east England, late Permian palaeogeography 285ff., 313ff. Borders Region, Tertiary dyke 199ff. North-west England, metamorphic history 325ff. cannon-ball concretions 35-36 North Pennine Orefield, mineralisation Iff. carbonate beds, Coal Measures 195-196 Northern Pennines, structural history 2-4 climatic change, late Quaternary 127ff. Northumberland, dolerite-pegmatites 249ff. coleoid cephalopods, late Jurassic 149ff. ostracods, late Quaternary 129-131 concretions, calcitization and compaction 35-40 palaeokarst, Dinantian 345ff. coralline concretions 37 palaeontology, Dinantian rugose corals 155ff., 233ff. corals, Dinantian 155ff. palaeontology, Dinantian trilobites 163ff. corals, Visean biostratigraphy of 233ff.
    [Show full text]