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Structure and Emplacement of High-Level Magmatic Systems - Special Publication no 302 (Geological Society) PDF

234 Pages·2008·6.66 MB·English
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There are continual rounds of annual conferences, special sessions and other symposia that provide ample opportunity for researchers to convene and discuss igneous processes. However, the origins of laccoliths and sills continue to inspire and confound geologists. In one sense, this is surprising. After all, don’t we know all we need to know about these rocks by now? As testified by the diverse range of topics covered in this volume, the answer is clearly ‘no’. This book contains contributions on physical geology, igneous petrology, volcanology, structural geology, crustal mechanics and geophysics that cover the entire gambit of geological processes associated with the shallow emplacement of magma. High-level intrusions in sedimentary basins can also act as hydrocarbon reservoirs and as sources for thermal maturation. In drawing together a diversity of perspectives on the emplacement of sills, laccoliths and dykes we hope to advance further our understanding of their behaviour. Structure and Emplacement of High-Level Magmatic Systems The Geological Society of London Books Editorial Committee ChiefEditor BOB PANKHURST (UK) SocietyBooksEditors JOHN GREGORY (UK) JIM GRIFFITHS (UK) JOHN HOWE (UK) PHIL LEAT (UK) NICK ROBINS (UK) JONATHAN TURNER (UK) SocietyBooksAdvisors MIKE BROWN (USA) ERIC BUFFETAUT(FRANCE) JONATHANCRAIG(ITALY) RETO GIERE´ (GERMANY) TOM MCCANN (GERMANY) DOUG STEAD (CANADA) RANDELL STEPHENSON (NETHERLANDS) Geological Society books refereeing procedures TheSocietymakeseveryefforttoensurethatthescientificandproductionqualityofitsbooksmatchesthat ofitsjournals.Since1997,allbookproposalshavebeenrefereedbyspecialistreviewersaswellasbythe Society’sBooksEditorialCommittee. Ifthe refereesidentify weaknesses inthe proposal,these mustbe addressedbeforetheproposalisaccepted. Once the book is accepted, the Society Book Editors ensure that the volume editors follow strict guidelineson refereeingand qualitycontrol.Weinsistthatindividualpaperscanonlybeacceptedafter satisfactoryreviewbytwoindependentreferees.Thequestionsonthereviewformsaresimilartothosefor JournaloftheGeologicalSociety.Thereferees’formsandcommentsmustbeavailabletotheSociety’s BookEditorsonrequest. Althoughmanyofthebooksresultfrommeetings,theeditorsareexpectedtocommissionpapersthat werenotpresentedatthemeetingtoensurethatthebookprovidesabalancedcoverageofthesubject.Being acceptedforpresentationatthemeetingdoesnotguaranteeinclusioninthebook. MoreinformationaboutsubmittingaproposalandproducingabookfortheSocietycanbefoundonits website:www.geolsoc.org.uk. Itisrecommendedthatreferencetoallorpartofthisbookshouldbemadeinoneofthefollowingways: THOMSON K.&PETFORD N.(eds)2008.StructureandEmplacementofHigh-LevelMagmaticSystems. GeologicalSociety,London,SpecialPublications,302. ABLAY,G.J.,CLEMENS,J.D.&PETFORD,N.Large-scalemechanicsoffracture-mediatedfelsicmagma intrusion driven by hydraulic inflation and buoyancy pumping. In: THOMSON K. & PETFORD N. (eds) Structure and Emplacement of High-Level Magmatic Systems. Geological Society, London, Special Publications,302,3–29. GEOLOGICAL SOCIETY SPECIAL PUBLICATION NO.302 Structure and Emplacement of High-Level Magmatic Systems EDITED BY K. THOMSON University of Birmingham, UK and N. PETFORD Bournemouth University, UK 2008 Published by The Geological Society London THE GEOLOGICAL SOCIETY TheGeologicalSocietyofLondon(GSL)wasfoundedin1807.Itistheoldestnationalgeologicalsociety intheworldandthelargestinEurope.ItwasincorporatedunderRoyalCharterin1825andisRegistered Charity210161. TheSocietyistheUKnationallearnedandprofessionalsocietyforgeologywithaworldwideFellowship(FGS)of over9000.TheSocietyhasthepowertoconferCharteredstatusonsuitablyqualifiedFellows,andabout2000ofthe Fellowship carry the title (CGeol). Chartered Geologists may also obtain the equivalent European title, European Geologist(EurGeol).OnefifthoftheSociety’sfellowshipresidesoutsidetheUK.TofindoutmoreabouttheSociety, logontowww.geolsoc.org.uk. TheGeologicalSocietyPublishingHouse(Bath,UK)producestheSociety’sinternationaljournalsandbooks,and actsasEuropeandistributorforselectedpublicationsoftheAmericanAssociationofPetroleumGeologists(AAPG), theIndonesianPetroleumAssociation(IPA),theGeologicalSocietyofAmerica(GSA),theSocietyforSedimentary Geology (SEPM) and the Geologists’ Association (GA). Joint marketing agreements ensure that GSL Fellows may purchase these societies’ publications at a discount. The Society’s online bookshop (accessible from www.geolsoc.org.uk)offerssecurebookpurchasingwithyourcreditordebitcard. TofindoutaboutjoiningtheSocietyandbenefitingfromsubstantialdiscountsonpublicationsofGSLandother societiesworldwide,consultwww.geolsoc.org.uk,orcontacttheFellowshipDepartmentat:TheGeologicalSociety, Burlington House, Piccadilly, London W1J 0BG: Tel. þ44 (0)20 7434 9944; Fax þ44 (0)20 7439 8975; E-mail: [email protected]. ForinformationabouttheSociety’smeetings,consultEventsonwww.geolsoc.org.uk.Tofindoutmoreaboutthe Society’sCorporateAffiliatesScheme,[email protected]. PublishedbyTheGeologicalSocietyfrom: TheGeologicalSocietyPublishingHouse,Unit7,BrassmillEnterpriseCentre,BrassmillLane,BathBA13JN,UK (Orders:Tel.þ44(0)1225445046,Faxþ44(0)1225442836) Onlinebookshop:www.geolsoc.org.uk/bookshop Thepublishersmakenorepresentation,expressorimplied,withregardtotheaccuracyoftheinformationcontainedin thisbookandcannotacceptanylegalresponsibilityforanyerrorsoromissionsthatmaybemade. # The Geological Society of London 2008. All rights reserved. No reproduction, copy or transmission of this publicationmaybemadewithoutwrittenpermission.Noparagraphofthispublicationmaybereproduced,copiedor transmittedsavewiththeprovisionsoftheCopyrightLicensingAgency,90TottenhamCourtRoad,LondonW1P9HE. UsersregisteredwiththeCopyrightClearanceCenter,27CongressStreet,Salem,MA01970,USA:theitem-feecode forthispublicationis0305-8719/08/$15.00. BritishLibraryCataloguinginPublicationData AcataloguerecordforthisbookisavailablefromtheBritishLibrary. ISBN978-1-86239-256-4 TypesetbyTechsetCompositionLtd.,Salisbury,UK PrintedbyMPGBooksLtd.,Bodmin,UK Distributors NorthAmerica Fortradeandinstitutionalorders: TheGeologicalSociety,c/oAIDC,82WinterSportLane,Williston,VT05495,USA Orders: Tel.þ1800-972-9892 Faxþ1802-864-7626 [email protected] Forindividualandcorporateorders: AAPGBookstore,POBox979,Tulsa,OK74101-0979,USA Orders: Tel.þ1918-584-2555 Faxþ1918-560-2652 [email protected] Websitehttp://bookstore.aapg.org India AffiliatedEast-WestPressPrivateLtd,MarketingDivision,G-1/16AnsariRoad,DaryaGanj,NewDelhi110002,India Orders: Tel.þ91112327-9113/2326-4180 Faxþ91112326-0538 E-mailaffi[email protected] Preface LASI II (Laccoliths, Sills and Dykes) washeld on at the interface between geophysics and physical the Island of Skye, Scotland, on 1–3 April 2006. geology, as applied to the nature and geometry of Building on the success of LASI I held in 2002 sillsandotherintrusions.Hisworkwasinterdisci- at TU BergakademieFreiberg, Germany,40 parti- plinary, thought-provoking and colourful, often cipants from around the world descended on bestenjoyedthroughpaper-framedspectacleswith Portree for a combined workshop and field trip to green and red plastic lenses! Ken provided a examine the classic Paleocene sill complexes, led conduit linking two subject areas distinguished by Donny Hutton, Ken Thomson and students largely by their historical lack of cross-over, from Birmingham University. Papers from the namely reflection seismology and volcanology. In LASI I meeting in Freiberg, Germany were pub- pioneering the transfer of knowledge between the lishedbytheGeologicalSocietyin2004(Geologi- two, Ken was at the forefront of a research area calSociety,London,SpecialPublication234edited set to become increasingly relevant as the need to byC.Breitkreuz&N.Petford). understand better the role of high-level intrusions LASI II provided an opportunity to discover in thermal maturation, storage and trapping of how the study of high-level magmatic systems hydrocarbonsgrows. had developed over the 4 years since Freiberg. Tragically,KenThomsondiedon18April2007, With contributions on physical geology, igneous justasthefirstrevisionsfromauthorswerearriving petrology, volcanology, structural geology, crustal atBirmingham.Ken’shandrunsdeepthroughthis mechanics and geophysics, the 43 presentations volume and I know he was proud of the work put attheSkyeworkshopcoveredtheentiregambitof intotheassembledpapersbyauthorsandreviewers geological processes associated with the shallow alike, and grateful of support from the Geological emplacement of magma. Arrangements for Society, the Volcanic and Magmatic Studies LASI III, to be hosted by Italian colleagues on Group, and the IAVCEI commissions on granites Elba island, are already well underway (http:// and volcanogenic sediments. This Special Publi- www.dst.unipi.it/dst/rocchi/LASI3/Home.html). cationisdedicatedtohim. LASIII(thedifficultsecondmeeting)wouldnot Ken is sadly no longer with us. But LASI havehappenedwithouttheorganizationaldriveand liveson. hardworkofKenThomson.Ken’sspecialismwas NICK PETFORD Obituary: Dr Ken Thomson 1966–2007 It was a huge shock to us all when Ken Thomson His enthusiasm for geology was abundant and died suddenly while at work in April 2007. Ken hisresearcheclectic.Hewasbestknowninvolca- wasafamiliarfaceinvolcanologycircles,andco- nology and igneous circles for using oil industry organizedthehighlysuccessfulLASIIIconference offshore three-dimensional (3D) seismic data to (theinspirationforthisSpecialPublication).Itisa pioneer the development of sophisticated high- greatshamethatthegeologicalcommunityhaslost resolution3Dimagesofburiedvolcanicfieldsand suchafreethinker. sillcomplexes.Herealizedthatthiskindofvisual- izationwouldgiveunprecedentedaccesstothegeo- metryandarchitectureofunexposedsillcomplexes, and help us in understand their emplacement and associated magma flow. This led to a number of key breakthroughs including a paper published in 2004 looking at the emplacement of saucer- shaped sills from the NW Atlantic Margin, which showed that sills emplaced as a series of lobes similar to those seen in lava flows. His work was clearly beginning to provide significant insights and was tackling some long-standing issues in emplacement of sill complexes. The final major paper before his death gave very convincing evi- dence for an interconnected plumbing system of sills and dykes feeding past fissure eruptions in the now submerged approximately 60Ma flood basaltsoftheNWAtlanticMargin. The innovations of Ken’s research were not restrictedtoigneousintrusions.Usingthevisualiza- tiontechniqueshedevelopedforigneousbodiesand making use of the otherwise unexploited top few tensofmetresofseismicdata,hewasabletohelp the Institute of Archaeology and Antiquity at the University of Birmingham to reconstruct a vast submergedlandscapeinthesouthernNorthSea.It is a particular tragedy that Ken’s death came just a week before the work he pioneered was the subjectofa‘TimeTeamSpecial’onChannel4. KenbeganhiscareerasamedicatManchester, KenwasproudofhisDoncasterroots.Hehasbeen but realized his true calling and transferred described,andwillberemembered,asanarchetypal toGeology,graduatingin1990.Hethenmovedto Yorkshireman and a traditionalist. His mild- Edinburgh, where his PhD thesis concentrated on manneredunassumingpersonaanduniquesenseof basindynamicsoftheMorayFirth.Aftercomplet- humourendearedhimtoagreatnumberofpeople. inghisPhDhetookupapositionattheUniversity Heisgreatlymissed,asbothagoodfriendand of Oxford as the BP Exploration Junior Research colleague. Fellow in Geophysics, before moving on to a NICK SCHOFIELD, lectureship in petroleum geology at Durham in CARL STEVENSON 1995,andthenfinallytoBirminghamin1999. &DONNY HUTTON

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There are continual rounds of annual conferences, special sessions and other symposia that provide ample opportunity for researchers to convene and discuss igneous processes. However, the origin of laccoliths and sills continue to inspire and confound geologists.In one sense, this is surprising. Aft
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