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Structural Geometry, Tectonic History And
STRUCTURALGEOMETRY, TECTONIC HISTORY AND DEFORMATIONMECHANISMS IN THE MOINETHRUST ZONENEAR ULLAPOOL N. W. SCOTLAND D.A. WINTER B. Sc. M.Sc. DIC Thesis submitted for the degree of Doctor of Philosophy at the University of Edinburgh 1984 The laboratory work for Chapter 6 was carried out at St. Andrews University by Dr. G. Oliver, the remainder of the thesis is all my own work. Signed. A-W CONTENTS PAGE ABSTRACT. 1 ACKNOWLEDGMENTS. 2 CHAPTER13 INTRODUCTION. 3 STRATIGRAPHY. 4 1.1.1. THE LEWISIAN GNEISS COMPLEX. 4 1.1.2. THE "TORRIDONIAN" SEDIMENTS. 5 1.1.3. THE CAMBRO-ORDOVICIANSEDIMENTS. 6 1.1.4. THE MOINE METASEDIMENTS. 7 1.2. THRUSTTECTONICS AND CURRENTRESEARCH IN THE 9 MOINE THRUSTZONE CHAPTERTWO THE STRUCTURALGEOMETRY OF THE MOINE THRUSTZONE BETWEEN LOCH BROOMAND THE ASSYNTCULMINATION 2.1. INTRODUCTION 11 2.1.1 NOMENCLATURE 12 2.2. STRUCTURALGEOMETRY: THE MOINE THRUST 13 2.2.1 LATE MOVEMENTON THE MOINE THRUST: THE EVIDENCEOF AN 15 EXTENSIONALMOINE THRUST 2.3. THE LOCH BROOMTHRUST SHEET 18 2.3.1 STRUCTURALGEOMETRY OF LOCH BROOMTHRUST SHEET 18 2.3.2 DISPLACEMENTON THE LOCH BROOMTHRUST 19 2.4. THE ULLAPOOLTHRUST SHEET 21 2.4.1 DISPLACEMENTON THE ULLAPOOLTHRUST 22 2.5. SHEETIV 22 2.5.1 STRUCTURALGEOMETRY OF SHEETIV 23 2.5.1.1 BEDDINGPLANE GEOMETRY AND ITS STRUCTURAL IMPORTANCEIN SHEETIV 23 2.5.1.2 FOLDINGIN SHEETIV 24 2.5.1.3 FAULTSAND TECTONIC VEINS 26 2.5.1.3a THE NE-SWSET OF EXTENSIONFAULTS 26 2.5.1.3b THE NW-SESET OF EXTENSIONFAULTS 27 2.5.1.3c THE STRIKE-SLIP FAULTS 28 2.5.1.4 TECTONICVEINS 29 2.5.1.5 CLASSIFICATIONOF THE EXTENSIONFAULTS 31 2.6. -
Structural, Petrological, and Tectonic Constraints on the Loch Borralan and Loch Ailsh Alkaline Intrusions, Moine Thrust Zone, GEOSPHERE, V
Research Paper GEOSPHERE Structural, petrological, and tectonic constraints on the Loch Borralan and Loch Ailsh alkaline intrusions, Moine thrust zone, GEOSPHERE, v. 17, no. 4 northwestern Scotland https://doi.org/10.1130/GES02330.1 Robert Fox and Michael P. Searle 24 figures Department of Earth Sciences, Oxford University, South Parks Road, Oxford OX1 3AN, UK CORRESPONDENCE: [email protected] ABSTRACT during ductile shearing. The minerals pseudomor- Grit Members of the An t-Sron Formation) and the phing leucites show signs of ductile deformation Ordovician Durness Group dolomites and lime- CITATION: Fox, R., and Searle, M.P., 2021, Structural, petrological, and tectonic constraints on the Loch Bor- During the Caledonian orogeny, the Moine indicating that high-temperature (~500 °C) defor- stones (Woodcock and Strachan, 2000; Strachan ralan and Loch Ailsh alkaline intrusions, Moine thrust thrust zone in northwestern Scotland (UK) mation acted upon pseudomorphed leucite crystals et al., 2010; British Geological Survey, 2007). zone, northwestern Scotland: Geosphere, v. 17, no. 4, emplaced Neoproterozoic Moine Supergroup rocks, that had previously undergone subsolidus break- The hinterland of the Caledonian orogenic p. 1126– 1150, https:// doi.org /10.1130 /GES02330.1. meta morphosed during the Ordovician (Grampian) down. New detailed field mapping and structural wedge comprises schists of the Moine Super- and Silurian (Scandian) orogenic periods, westward and petrological observations are used to constrain group with structural inliers of Lewisian basement Science Editor: Andrea Hampel Associate Editor: Robert S. Hildebrand over the Laurentian passive margin in the north- the geological evolution of both the Loch Ailsh gneisses and intrusive Caledonian granites (Geikie, ern highlands of Scotland. -
Geodiversity Audit and Action Plan 2013 - 2016
GEODIVERSITY AUDIT AND ACTION PLAN 2013 - 2016 THIS PROJECT IS BEING PART FINANCED BY THE SCOTTISH GOVERNMENT AND THE EUROPEAN COMMUNITY HIGHLAND LEADER 2007-2013 PROGRAMME. CONTENTS FOREWORD.................................................................................................................. 1 ROCKS FROM THE DAWN OF TIME……………………………………………………….2 INTRODUCTION............................................................................................................ 3 The North West Highlands Geopark........................................................................... 3 The Geology and Geological Structure of the NWHG................................................. 3 The Purpose of the Audit and Action Plan .................................................................. 5 Geodiversity................................................................................................................ 5 Part 1 – THE GEODIVERSITY AUDIT........................................................................... 7 North West Highland Geopark : Location Maps ............................................................. 9 NWHG REF. 001 - BEN HUTIG................................................................................ 13 NWHG REF. 002 - CLEIT AN T-SEABHAIG ............................................................ 15 NWHG REF. 003 - ERIBOLL.................................................................................... 17 NWHG REF. 004 - AN T-SRON .............................................................................. -
Geological Notes and Location Descriptions for Field Excursions
Inverness: 30 April - 7 May Inverness: 30 Geological notes and location descriptions for field excursions Deformation mechanisms, Rheology and Tectonics 2017 Deformation mechanisms, Rheology and Tectonics 1 Geological notes* The crustal evolution and geology of NW Scotland can be considered with reference to the Palaeozoic Caledonian orogeny. This major episode of crustal reworking was associated with the formation of a North Atlantic Craton – suturing the Proterozoic and older crustal blocks of Laurentian and Baltica (together with Avalonia, further south). NW Scotland contains part of the western margin of this orogen (or at least its more intense parts), a tectonic feature termed the Moine Thrust Belt. The foreland to the thrust belt preserves much older geology, exhumed from up to 35-40km depth, that give insight to processes that form, rework and reassemble the continental crust. The Caledonian rocks allow us to follow a transect from exhumed middle crustal sections within the orogen out into the foreland. Collectively these outcrops provide arrays of analogues for crustal geology and deformation structures, and we can use these to promote discussion of their geophysical characteristics when targeted in situ. However, the Caledonian crust, together with its foreland, has seen later deformation associated with the formation of sedimentary basins, chiefly in the immediate offshore. We can also access basin faults and examine not only their individual characteristics but also debate how they may have been influenced by pre-existing structures. Pre-Caledonian geology The Lewisian. The Lewisian forms the oldest basement to the British Isles and has classic Laurentian geology. The key geological markers in the field used to build up a sequence of geological events are a suite of NW-SE-trending metabasic sheets – the Scourie dykes. -
Hiking Scotland's Western Isles
Hiking Scotland’s Western Isles July 11 - 21, 2015 (11 days) , with Carleton Professor Clint Cowan 83 © AAWH © AAWH © AAWH Dear Carleton College Alumni and Friends, Gearrannan Dun Carloway I invite you to join Carleton College geologist Clint Cowan ’83 on this ISLE OF LEWIS wonderful hiking adventure amid the wealth of geological and archaeologi- ISLE OF HARRIS cal sites in Scotland’s western Highlands and Islands. The rocks tell the whole stornoway story, going back 2.7 million years, as you travel from the Isle of Mull in the Cotland Tarbert Callanish south, along the western edge of highland Scotland, to the Isle of Lewis in the s Outer Hebrides, sometimes along the mainland coast, but more often across incomparably beautiful, fascinating islands. Rodel Uig To fully enjoy and visit all the sites on this itinerary, you must be reasonably ISLE OF SKYE fit and enjoy hiking. The daily hikes will be easy to moderate in difficulty, and their duration (and elevation gained) for each day is estimated within the itin- Talisker Distillery Western erary. You will not rush, but you will hike up to six miles per day, sometimes Loch Coruisk uphill and/or over uneven ground. Elgol Mallaig Two minibuses, each with an expert local driver/guide, will accompany the Glenfinnan group. Your guides will explain in advance the difficulty of each day’s walk(s) and, if you prefer, you can opt out of any walking excursion and be driven to Kilchoan Fingal’s Cave the next stop (but, bear in mind that some sites can only be visited if you walk to them). -
The Neoproterozoic to Mid-Devonian Evolution of Scotland: a Review and 7 Unresolved Issues
1 1 2 3 Article-type: Article 4 5 6 The Neoproterozoic to Mid-Devonian evolution of Scotland: a review and 7 unresolved issues. 8 9 John F. Dewey1*, Ian W. D. Dalziel2, R. John Reavy3, and Rob A. Strachan4 10 11 1 University College, High Street, Oxford OX1 4BH, UK 12 2 Institute for Geophysics, Jackson School of Geosciences, The University of Texas at Austin, 13 Austin TX 78758, USA 14 3 School of Biological, Earth, and Environmental Sciences, University College Cork, Cork, 15 Ireland 16 4 School of Environmental Sciences, University of Portsmouth, Portsmouth, UK 17 18 *Correspondence ([email protected]) 19 20 r/head: Tectonic evolution of Scottish Caledonides 21 22 Abstract: The purpose of this review paper is to identify and outline some critical questions 23 about the geology and tectonic evolution of the Scottish Caledonides in their wider 24 Caledonian/Appalachian context. We outline what we think we know and what we perceive to be 25 some important problems from about 1. 0 Ga (Grenville Orogeny) to Middle Devonian (Acadian 26 Orogeny). We do not attempt in-depth analyses of any terrain or tectonic topic in this review but, 27 mainly, pose questions. Scotland is considered in the context of the Irish Caledonides and the 28 Northern Appalachians, especially Newfoundland, so we make reference to these areas where 29 appropriate. Each section is intended as “stand-alone”, not dependent upon prior or subsequent 30 sections; the sequence of sections, roughly in time order, has a historical narrative thread. We 31 have not included cross-sectional cartoons because we do not have a clear picture of plate 2 32 boundary zone and terrane arrangements in the Caledonides. -
Timing of Regional Deformation And
1 Timing of regional deformation and development of the Moine 2 Thrust Zone in the Scottish Caledonides: constraints from the U-Pb 3 geochronology of alkaline intrusions 4 K. M. Goodenough1, I. Millar2, R.A. Strachan3, M. Krabbendam1, and J.A. Evans2 5 1 British Geological Survey, West Mains Road, Edinburgh EH9 3LA (contact e-mail: 6 [email protected]) 7 2 NERC Isotope Geoscience Laboratory, Kingsley Dunham Centre, Keyworth, 8 Nottingham NG12 5GG 9 3 School of Earth & Environmental Sciences, University of Portsmouth, Burnaby 10 Road, Portsmouth PO1 3QL 11 12 Abstract 13 The Moine Thrust Zone in the Scottish Highlands developed during the Scandian 14 Event of the Caledonian Orogeny, and now forms the boundary between the 15 Caledonian orogenic belt and the undeformed foreland. The Scandian Event, and the 16 formation of the Moine Thrust Zone, have previously been dated by a range of 17 isotopic methods, and relatively imprecise ages on a suite of alkaline intrusions 18 localised along the thrust zone have provided the best age constraints for deformation. 19 Recent BGS mapping has improved our understanding of the structural relationships 20 of some of these intrusions, and this work is combined with new U-Pb dates in this 21 paper to provide significantly improved ages for the Moine Thrust Zone. Our work 22 shows that a single early intrusion (the Glen Dessarry Pluton) was emplaced within 23 the orogenic belt to the east of the Moine Thrust Zone at 447.9 ± 2.9 Ma. A more 24 significant pulse of magmatism centred in the Assynt area, which temporally 25 overlapped movement in the thrust zone, occurred at 430.7 ± 0.5 Ma. -
OUGS Journal 33
Open University Geological Society Journal Volume 33 (1) 2012 Stirling Symposium Issue Editor: Dr David M. Jones e-mail: [email protected] The Open University Geological Society (OUGS) and its Journal Editor accept no responsibility for breach of copyright. Copyright for the work remains with the authors, but copyright for the published articles is that of the OUGS. ISSN 0143-9472 © Copyright reserved OUGS Journal 33 (1) Edition 2012, printed by Hobbs the Printers Ltd, Totton, Hampshire Committee of the Open University Geological Society 2012 Society Website: ougs.org Executive Committee President: Dr Nick Rogers, Department of Earth Sciences, The Open University, Milton Keynes MK7 6AA Chairman: Linda Fowler Secretary: Sue Vernon Treasurer: John Gooch Membership Secretary: Phyllis Turkington Newsletter Editor: Karen Scott Events Officer: Chris Arkwright Information Officer: Pauline Kirtley Branch Organisers East Anglia (EAn): Wendy Hamilton East Midlands (EMi): Don Cameron East Scotland (ESc): Stuart Swales Ireland (Ire): John Leahy London (Lon): John Lonergan Mainland Europe (Eur): Elisabeth d'Eyrames Northumbria (Nor): Paul Williams North West (NWe): Jane Schollick Oxford (Oxf): Sally Munnings Severnside (Ssi): Janet Hiscott South East (SEa): Elizabeth Boucher South West (SWe): Chris Popham Walton Hall (WHa): Tom Miller Wessex (Wsx): Sheila Alderman West Midlands (WMi): Mr A Farquharson West Scotland (WSc): Cliff Probert Yorkshire (Yor): Ricky Savage Other officers (non-OUGSC voting unless otherwise indicated) Sales Administrator (voting OUGSC member): Ian Lancaster Administrator: Don Cameron Minutes Secretary: Linda McArdell Journal Editor: Dr David M. Jones Archivist/Reviews: Jane Michael Webmaster: Stuart Swales Deputy Webmaster: Martin Bryan Gift Aid Officer: Ann Goundry OUSA Representative: Bill Willows OUSA Deputy Representative: vacant at time of going to press Branch Organisers Representative: Jane Schollick Vice Presidents Dr Evelyn Brown, Dr Michael Gagan and Norma Rothwell Past Presidents 1973–74 Prof. -
Proceedings of the Geological Society Of
PROCEEDINGS OF THE GEOLOGICAL SOCIETY OF GLASGOW Session 148 2005 – 06 1 SESSION 148 (2005 – 2006) Members of Council 2 Reports Membership 3 Library 3 Scottish Journal of Geology 3 Publications 4 Website 4 Strathclyde RIGS Group 5 Treasurer 6 Meetings Secretary’s report 8 Lectures 8 Members’ Night 17 Excursions Secretaries’ Reports 19 Garrell Burn & Corrieburn, 6 May 19 Wandel Burn, 3 June 20 Glenshiel, 23 – 26 June 22 St Monan’s, Fife, 15 July 32 BGS Core Store, Edinburgh, Friday 28 July 34 Highland Boundary Ophiolite and Dalradian Rocks of Cowal, 19 August 35 Assynt and Wester Ross, 14 –18 September 36 General Information 42 Obituary 43 2 SESSION 148 (2005– 2006) Members of Council President Dr Chris J. Burton Vice Presidents Dr Colin J. R. Braithwaite Dr Mike C. Keen Mr Charles M. Leslie Honorary Secretary Dr Iain Allison Treasurer Mr Mervyn H. Aiken Membership Secretary Dr Robin A. Painter Minutes Secretary Mrs Margaret L. Greene Meetings Secretary Dr J.M. Morrison Publications Mr Roy Smart Librarian Dr Chris J. Burton Asst Librarian & Hon Archivist Mrs Seonaid Leishman Proceedings Editor Miss Margaret Donnelly Publicity Dr Neil D.L.Clark (web) Dr R. A. Painter (meetings etc) Excursion Secretaries Mrs Carolyn Mills (Saturdays) Mr David McCulloch (Residential) Strathclyde RIGS Chairperson Dr Brendan Hamill Strathclyde RIGS Secretary vacant Rockwatch Representative vacant Junior Member Ms R. Farthing/ Ms L. Munro Journal Editors Dr Colin J.R. Braithwaite Dr R.M. Ellam Ordinary Members Miss Karen Baillie Mrs N.G. Hornibrook Mrs Rosemary McCusker, Dr A.W. Owen. vacancy vacancy Auditors Dr Ben Browne Miss Sally Rowan 3 MEMBERSHIP At end 148 At end 147 30 Sep., 2006 30 Sep., 2005 Honorary Members 5 5 Ordinary Members 300 302 Associate Members 67 58 Junior Members 23 18 TOTAL Members 395 383 New Members 23 Memberships Closed 10 Ordinary Membership has remained fairly static, with solid growth in the numbers of Associate and Junior Members leading to an overall growth in total membership of 3%. -
1Department of Earth Sciences, University of Liverpool, Liverpool
Journal of the Geological Society, London, Vol. 152, 1995, pp. 907-910, 3 figs. Printed in Northern Ireland metamorphosed late Proterozoic Torridonian mudstones, siltstones and sandstones and Cambrian-early Ordovician Late-orogenic extensional tectonics at the NW siliciclastic and carbonate sediments. The eastern part of margin of the Caledonides in Scotland the Moine Thrust Belt.is dominated by recumbent fold nappes which involve both basement and cover. These nappes were carried and cut by thrusts which are associated G.J. POTTS 1, R.H. HUNTER 1, with mylonite. In general, the mylonitic foliations dip gently A.L. HARRIS 1 & F.M. FRASER 2 towards the ESE and display a down-dip grain shape 1Department of Earth Sciences, University of lineation. Liverpool, Liverpool L69 3BX, UK The Moine Thrust, carrying the Moine Nappe, is the 2Argyll Hotel, Iona, UK westernmost, lowest and youngest of three major thrusts (Fig. 1), the others being the Knoydart and Sgurr Beag (highest and oldest) thrusts, carrying respectively the Knoydart and Sgurr Beag nappes (Barr et al. 1986). Eastwards and upwards across the nappe boundaries A major ductile extensional structure throwing down several metamorphic grade increases such that the different nappes kilometres to the ESE probably marks the southern portion of the NW Caledonian orogenic margin in Scotland. This structure, the have distinguishing metamorphic characteristics. Moine Sound of lona Fault, is probably related to the intensely mylonitized Nappe metasediments are largely at the greenschist to low zones that cut the Lewisian and adjacent lona Group (?Torr- amphibolite facies of metamorphism, the Knoydart Nappe idonian) metasedimentary cover on Iona. -
Installation of Tidal Turbine Array at Kyle Rhea, Scotland: Scoping Study
Installation of tidal turbine array at Kyle Rhea, Scotland Scoping Study Marine Current Turbines 22 March 2010 Final Report 9V5627 i 10 Bernard Street Leith Edinburgh EH6 6PP United Kingdom +44 (0)131 555 0506 Telephone Fax [email protected] E-mail www.royalhaskoning.com Internet Document title Installation of tidal turbine array at Kyle Rhea, Scotland Scoping Study Document short title Status Final Report Date 22 March 2010 Project name Project number 9V5627 Client Marine Current Turbines Reference 9V5627/R/303719/Edin Drafted by Gemma Bedford, David Tarrant & Jennifer Trendall Checked by Jennifer Trendall & Frank Fortune Date/initials check …………………. …………………. Approved by Frank Fortune Date/initials approval …………………. …………………. CONTENTS 1 INTRODUCTION 1 1.1 Background 1 1.2 Project Description 1 2 POLICY AND LEGISLATION 5 2.1 Renewable energy policy in Scotland 5 2.2 Planning Legislation 5 2.1 Appropriate Assessment 6 2.2 Conservation Legislation 6 3 PHYSICAL ENVIRONMENT 8 3.1 Physical processes and geomorphology 8 3.2 Water/ sediment quality 11 4 BIOLOGICAL PARAMETERS 13 4.1 Ecological Designated sites 13 4.2 Marine Ecology (including benthic and intertidal) 14 4.3 Ornithology 16 4.4 Terrestrial Ecology 17 4.5 Marine Mammals and Reptiles 19 4.6 Natural fish and shellfish 20 5 HUMAN ACTIVITIES 26 5.1 Seascape / landscape 26 5.2 Commercial fisheries 26 5.3 Shipping and Navigation 30 5.4 Onshore Traffic and Transport 32 5.5 Military Activity 32 5.6 Archaeology and Cultural Heritage 33 5.7 Noise 35 5.8 Tourism and recreation 35 5.9 Air traffic 46 5.10 Socio-economics 46 6 CONCLUSION 47 7 FUTURE PROGRAMME / CONSULTATION 49 7.1 EIA process 49 7.2 Consultation strategy 50 8 REFERENCES 52 A1 ECOLOGICAL MONITORING PLAN 55 9V5627/R/303719/Edin Final Report - i - 22 March 2010 1 INTRODUCTION The basic requirement for cost-effective power generation from tidal streams is a mean spring peak 1.1 Background velocity exceeding about 2.5 metres per second (m/s). -
Back Matter (PDF)
Index Note: Page numbers denoted in italics indicate figures and those in bold indicate tables. Abbott, D., 760 separating two distinct terranes, 114–116 Acadian Events, 183 terranes juxtaposition, 116–117 Acceleration-strain tensor, 745 Archibald Don. A Memoir (Sayle), 46 Arcuate thrust toe Precambrian Mylonite Zone, Ard gneiss 715–736 Ialltaig, 56–57 Achiniver Zone, 528 Loch Maree Group, 63 Achmelvich, 56 Ardnamurchan, 239 Achnashellach area, 16 Ardnish Achness Falls, 368 pegmatites, 242 Achness Nappe, 371 Rb–Sr muscovite ages, 239 Achness Thrust, 363, 369, 371 Arenig, 21 Cassley Folds, 365 Argentine Precordillera, 192, 199, 841 geological maps, 368 Marathon-Solitario basin, 201 ACM. See Attico-Cycladic Massif proto-Appalachian margin, 193 (ACM, Internal Hellenides, Greece) Argentine–Texan tectonic interaction, 203 Adams, F. D., 520 Argyll Group, 127 Africa Arkle, 10–11 inversion v. simple extension or strike-slip, 839 Arnaboll sector cross-section, 325 Mesozoic–Cenozoic rift system, 836 Arnaboll Thrust, 10, 291, 323 rift system, 838, 839 distribution deformation, 330 AFTA studies, 817 faults, 292 Alkali metasomatism, 64 plane, 327 Allison, I., 475, 478, 479 Arnaboll Thrust Sheet, 324 Allochthonous unit, 775–776 basement, 329 Allochthon unmetamorphosed rocks, 217 deformation, 327–329, 445–449, 479–480, 508–509, Allt Ealag, 29 514–517 Allt nan Sleach quartzites, 489 ductility, 330–332 Allt Rugaidh area fault rocks, 328, 445–449, 508–509, 514–517, 524–526 geological map, 368 foliation form lines, 326 Alps, 3, 31, 34, 36, 42, 222, 311,