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A Selective Lamprophyre Bibliography

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A Selective Lamprophyre Bibliography Compilation This Bibliography includes most publications which: (a) contain the word lamprophyre (or one of the varieties named in Fig. 1.2 and Appendix B) either in the title or as a keyword; (b) devote significant attention to lamprophyres in terms of field, petrographical or petrological description; (c) contain analytical data on lamprophyres. Those in which lamprophyres are only very briefly mentioned, and sources prior to and including those compiled by Washington (1917), are not generally included unless giving information which is critical or otherwise unavailable. References to kimberlites are not exhaustively compiled - readers should refer for example to R.H.Mitchell (1986) or to the 7 International Kimberlite Conference (IKC) volumes. Abstracts and unpublished works are excluded, unless there is no other published information on the topic. This Bibliography has been compiled over a period of over 16 years by an exhaustive combination of traditional literature search (aided by Bibliography and Index of Geology, Bulletin Signa/etique, Dissertation Abstracts International and Mineralogical Abstracts), plus usage of the many computerized geological source and reference databases now available (specifically AESIS, GEOARCHIVES, GEOBASE, GEOREF and IGBA). Note that searches from these systems on the free-text strings "minette" and "spessartite" will also raise references to sedimentary rocks and to garnets (e.g. Siehl & Thein 1978). Available compilations dealing with alkaline rocks (e.g. Heinrich 1966; Tuttle & Gittins 1966; S(6rensen 1974; Fitton & Upton 1987; Woolley 1987; Bell 1989; Mem.Geol.SocJndial5) and the 7 IKC volumes have also been searched. The rate of acquisition has now slowed to the point where the Bibliography probably includes the vast majority of relevant references; coverage of Russian and Chinese publications is probably weakest. Ordering Titles using Roman script are given in their languages; all others are translated into English between [... ) Mac, Mc, St. and similar are listed in strict alphabetical order; 2 or multi-author papers by the same senior author are listed chronologically, then alphabetically. Spaces, apostrophes and similar are ignored. Symbols # indicates that some rocks are regarded as different lamprophyres from those named in the source reference (especially camptonites rather than "spessartites"; aillikites rather than "kimberlites" or vice-versa). , indicates that the reference almost certainly hides additional lamprophyres described under other rock-names (e.g. "mafic porphyry", "diabase", "biotite-nephelinite", "K-rich diorite", "mica-peridotite''). ? indicates that insufficient information is given to confirm or repudiate the rocks described as "lamprophyres" (or under one variety name); the rocks are therefore regarded as unconfirmed (Table C7). @ indicates that some or all of the rocks described as "lamprophyres" (or varieties) do not obey the defmitions in Streckeisen(1979) or this work; they are thus considered apochryphal (Table C8). * indicates that chemical data from the source have been incorporated into the database LAMPDA (App.D). t indicates that the reference is cited in a bibliographical database (e.g. Bibliography & Index of Geology) and is therefore believed correct, but has nevertheless proved to be unobtainable. *indicates that the reference is cited by a third party but could not be located in any bibliographical database or obtained directly; hence the veracity of the reference itself is not guaranteed. **************************************************************************************** Abdullaev, K.M. 1957. [Dykes and ore mineralization). In Russian. Moscow. Abraham, E.M. 1951. Geology of McElroy and part of Boston townships. Ontario Dept.Mines Geol.Rep. 59,66pp. * Acejev,B.N. & Harlass,E. 1968.Zum Probleme der Altersstellung von Lamprophyren im westlichen Erzgebirge.Geolo gie 17, 1178-1194. Acharyya, S.K. 1969. A note on the geology of Darjeeling coalfield and its bearing on the structure of the Eastern Himalayas. Rec.Geol.Survlndia 97, 91-101. Adams,CJ.D. 1976.Geochronology of the Channel Islands and adjacent French mainlandJ.Geol.SocLond. 132,233-250. 158 LAMPROPHYRES Aires Barros, L. 1%5. Sabre as rochas feldspat6idicas da regina de Zenza do Itombe (Angola). Garcia de Orta (Lisboa). 13, 425-434. * Akella,J., Rao,S.P., McCallister,RH., Boyd, F.R. & Meyer,H.A.O. 1979. Mineralogical studies on the diamondiferous kimberlite of the Wajrakjarur area, southern India In: Boyd & Meyer (1979a), qv, 172-179. AlbarMe,F. & Weisbrod,A. 1981. Hercynian synorogenic lamprophyres from the SE Massif Central (France): evidence for equilibrium of Nd isotopes and REE elements with surrounding granitic rocks. EOS 62. p.1076 (abstr). Alcock,FJ. 1935.Geology of the Chaleur Bay region.Mem.Geol.Surv.Can.183, 146pp. * Alderman, A.R 1929. Magmatic differentiation at Mannum, S.A. TrR.Soc.S.Aust. 53,249-257. * Alderton,D. 1988.Ag-Au-Te mineralization in the Ratagain complex, northwest Scotland. Tr.Inst.Ming. Metall. 97, BI71-180. *Aldrick, DJ., Brown, D.A., Harakai, J.K. & Armstrong, RL. 1987. Geochronology of the Stewart mining camp, BC. Ministry of Energy. Mines & Petroleum Resources GeolFieldwork 1986. Pap. 1987-1,81-92. * Alibert, C. & AlbarMe, F. 1988. Relationships between mineralogical, chemical and isotopic properties of some North American kimberlites. J.GeophysRes. 93, 7643-7671. Alibert.C., Michard, A. & AlbarMe, F. 1986. Isotope and trace element geochemistry of Colorado Plateau volcanics. Geochem. Cosmochim. Acta SO, 2735-2750. t Alietti,A. 1955.Su di una camptonite anfibolica di Val del FOsch presso Mezzavalle in Val di Fassa. Period. Mineral. 24,27-46. * Allan,J.F. & Carmichael,I.S.E. 1984.Lamprophyric lavas from the Colima graben,Mexico. Contrib. Mineral.Petrol. 88,203-216. • Allen,J.B. & Deans,T. 1965.Ultrabasic eruptives with alnOitic-kimberlitic affinities from Malaita,Solomon Islands. Mineral.Mag. 34.16-34. * Allen,J.E. & Balk,R 1954.Mineral resources of the Fort Defiance-Tohatchi Quadrangles.New Mexico Bur.Mines Res.Bul/.36, 192pp. Allen,J.R.L. 1%8.The Cambrian and Ordovician systems (post-Cambrian intrusive rocks). In: The Geology of the East Midlands(eds.Sylvester-Bradley,P.C. & Ford,T.D.),37-38, LeicesterUniv. Press, Leicester. Allsopp,M.L.,Bristow,J.W.,Skinner,E.M.W.,Scott Smith,B.H. & Danchin,R.V. 1985. Rb-Sr geochronology of some Miocene West Australian lamproites.Tr.Geol.Soc.S.A(r.88,341-346. ? Amodio,L. & Hieke Merlin,O. 1966.1 proetti inclusi nelle piroclastiti del Monte Vulture (Lucania). Mem.Ist.Geol. Mineral.Univ.Padova 25,1-49. Anand, SN. 1971. Geological and geophysical investigations of diamondiferous volcanic pipe rocks from Lattavaram area, Anantapur district, Andhra Pradesh. Misc. Publ. Geol. Surv. India 19, 128-133. Ancochea, E. & Nixon, P.H. 1987. Xenoliths in the Iberian Peninsula In: Nixon (1987), qv, 119-124. Andersen,T.B. & Jansen,OJ. 1987. The Sunnhordland Batholith, W.Norway: regional setting and internal structure, with emphasis on the granitoid plutons. Norsk Geol.Tiddskr. 67, 159-181. * Anderson,J.G.C. 1935aThe Arrochar intrusive complex.GeoIMag.72,263-282. Anderson,J.G.C. 1935b.The marginal intrusions of Ben Nevis: the Coille Lianachain complex and the Ben Nevis dyke-swarm. Tr.Geol.Soc.Glasgow 19,225-269. Anderson,J.G.C. 1937a. Intrusions of the Glen Falloch area.GeolMag.74,458-468. Anderson,J.G.C. 1937b.The Etive granite complex.Q.l.Geol.SocLond.93,487-533. Anderson,J.G.C. & Tyrrell,G.W. 1936.Xenolithic minor intrusions in the Loch Lomond district. Tr.Geol.Soc. Glasgow 19,373-384. * Andrade,M.M.de. 1950.Um lampr6firo com homeblenda e biotite, da P6voa de Varzim. Est.Not.Trab.Serv. Fom. Mineral. (Porto), 14,49-56. • Andrade,M.M.de. 1954.Contribution a l'etude des roches alcalines d' Angola. 19th Int.Geol.Congr. (1952) fasc. xx,241-252. Andrade,M.M.de. 1979.Sobre a ocorrencia dum sistema de diques de lampr6firos na Praia de Labruje. Publ.MusLab. Mineral.GeoI.Fac.Ciencias Porto 91,151-153. * Andreasson,P.G.,Solyom,z. & Roberts,D. 1979.Petrochemistry and tectonic significance of basic and alkaline-ultrabasic dykes in the Leksdal Nappe,north Trondheim region,Norway.Norges Geol.Unders. 348,47-72. Andre,F. 1981. Un exemple de vaugneite, cumulat d'une association gabbro-dioritique dans Ie massif des Ballon (Vosges meridionales). CR.Acod.Sci.Paris Ser.II, 293, 445-448 Andrews,E.C., Mingaye J.C.H., & Card,G.W. 1907. The geology of the New England Plateau. Rec.Geol.Surv.N.S. W. 8(3),196-251. Andrews, J.R, Phillips W.E.A. & Molloy M.A. 1978. The metamorphic rocks of part of the north central Ox Mountains inlier of Counties Sligo and Mayo. J.Earth SciR.Dublin Soc. 1, 173-194 Anon. 1971. Diamond. Geol.Surv.IndiaMisc.Publ. 19, 269pp. BIBLIOGRAPHY 159 * Anon. 1988. The mafic dyke swarms of southernmost Sweden; guide.IGCP-257 Tech.Rep. 1,51-91. * Anton,L. & Constantinescu,R. 1977.0bservatii asupra lamproftrelor din Muntii Fagaras. In Romanian, Eng1.abstr. Rom. Inst.Geol.Geophys. Dari SeamIJ Sedintelor 64(1),53-76. * Aoki,K. 1981.Chemical composition of potassic basaltic rocks from the Colorado plateau.Sci.Rep.Tohoku Univ.xv,135-139. Appavadhanulu,K. 1966.Minette and riebeckite-ka\isyenite dykes in some upper Cuddapah rocks,Kumool district,Andhra Pradesh. Rec.Geol.Surv.lndia 94(2),303-304. Arima, M. & Edgar, A.D. 1981. Substitution mechanisms and solubility of titanium in phlogopites from rocks of probable mantle origin. Contrib. Mineral. Petrol. 77, 288-295. *Arima,M. & Edgar,A.D. 1983.A high pressure experimental study on a magnesian-rich leucite-lamproite from the West Kimberley area,Australia: petrogenetic implications.Contrib.Mineral.Petrol.84,228-234. * Arima, M. & Kerrich, R. 1988. Jurassic kimberlites from Picton and Varty Lake, Ontario: geochemical and stable isotope characteristics. Contrib. Mineral. Petrol. 99, 385-391. * Arribas,A.San Miguel. 1952.0bservations petrologiques sur les roches lamprophyriques de la Costa Brava Catalane (Bagur).19th Int.Geol.Congr.Sect.vi,77-99. Arthaud,F. & Matte,P. 1977. Late Pa1aeozoic strike-slip faulting in Southern Europe and North Mrica: results of right-lateral shear zone between Appalachians and Urals.
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    The Edinburgh Geologist Magazina of tho Edinburgh Gaological Soclaly Issue No. 31 Autumn 1998 Incorporating the Proceedings of the Edinburgh Geological Society for the 163rd Session 1996·1997 THE EDINBURGH GEOLOGIST Issue No. 31 Autumn 1998 Cover Illustration The cover illustration shows a drawing of Hemiarges iflghami, a trilobite from the Ordovician Stinchar Limestone ncar Girvan. This species lived along the coast of Laurentia, but found Avalonia a bit on the cool side. (see article by Phil SlOne, 'The Geology of Devolution' on page 8) The drawing is taken from a paper by R P Tripp (Pa laeolltology, 1979, Vol. 22, 339-361) and is reproduced by kind permission of the Palaeontological Association. Acknowledgements Publication of THE EDINBURGH GEOWGIST is supported by grants from the Peach and Horne Memorial Fund and the Sime Bequest Published October 1998 by The Edinburgh Geological Society Editor Alan Fyfe British Geological Survey Murchison Hou se Edinburgh EH93LA ISSN 0265-7244 Price £ 1.50 net Editorial by Alan Fyfc It is my pleasure to have been appointed as the editor of THE EDINBURGH GEOLOGIST and to welcome you to the thirty-first edition. I follow a long line of illustrious editors and hope that I am able to maintain the standard of the publication. My thanks are due to the outgoing editor, Andrew Highton for filling me in on the pitfalls and helping to get me started. This issue sees a slightly altered format, though the changes are largely cosmetic and I have attempted to maintain the general look and feel that has evolved over the years.
  • Downloaded for Personal Non-Commercial Research Or Study, Without Prior Permission Or Charge

    Downloaded for Personal Non-Commercial Research Or Study, Without Prior Permission Or Charge

    MacArtney, Adrienne (2018) Atmosphere crust coupling and carbon sequestration on early Mars. PhD thesis. http://theses.gla.ac.uk/9006/ Copyright and moral rights for this work are retained by the author A copy can be downloaded for personal non-commercial research or study, without prior permission or charge This work cannot be reproduced or quoted extensively from without first obtaining permission in writing from the author The content must not be changed in any way or sold commercially in any format or medium without the formal permission of the author When referring to this work, full bibliographic details including the author, title, awarding institution and date of the thesis must be given Enlighten:Theses http://theses.gla.ac.uk/ [email protected] ATMOSPHERE - CRUST COUPLING AND CARBON SEQUESTRATION ON EARLY MARS By Adrienne MacArtney B.Sc. (Honours) Geosciences, Open University, 2013. Submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy at the UNIVERSITY OF GLASGOW 2018 © Adrienne MacArtney All rights reserved. The author herby grants to the University of Glasgow permission to reproduce and redistribute publicly paper and electronic copies of this thesis document in whole or in any part in any medium now known or hereafter created. Signature of Author: 16th January 2018 Abstract Evidence exists for great volumes of water on early Mars. Liquid surface water requires a much denser atmosphere than modern Mars possesses, probably predominantly composed of CO2. Such significant volumes of CO2 and water in the presence of basalt should have produced vast concentrations of carbonate minerals, yet little carbonate has been discovered thus far.