Abstract
PrefaceThe English petrographer, mineralogist and structural petrologist Frank Coles Phillips is best known to mineralogists and geologists today for his now-classic textbooksAn Introduction to Crystallography(1946) andThe Use of Stereographic Projection in Structural Geology(1954); and to gemmologists for his major revision of Herbert Smith'sGemstones(1958). The adoption in Britain of the stereogram as a fundamental interpretational tool in structural geology owes much to the second of Phillips' books, and the development of structural geology in Australia was influenced by a lecture-tour which he undertook in 1953. A superb teacher, Phillips' main legacy lies in the students he trained and in the influence of his textbooks.As a result of his fluency in German, by 1932 Phillips, by then a young lecturer in the Department of Mineralogy at Cambridge University, had taken up the new techniques, first advocated by the Austrian geologist Bruno Sander (1884-1979) in 1930, for the analysis ofGefügekunde(petrofabrics) of geological bodies; i.e. the interpretation of the three-dimensional fabric of rocks, based on the determination of the statistical distribution of the orientation of particular crystallographic axes of minerals such as quartz, muscovite and biotite, accomplished by means of the 'universal' microscope stage (the petrofabric method). In 1937, at a time when the interpretation of structural geology in Britain was largely a field-based, qualitative practice, Phillips published a pioneering study in which he applied Sander's quantitative methods in an attempt to unravel the complex structural history of the Moine rocks of NW Scotland. Much of Phillips' subsequent research focused on the application of the petrofabric method to the Moine, and later to the metamorphic rocks of SW England, doggedly following the rules for kinematic interpretation as laid down by Sander in the 1930s and later embodied in his cryptic and partly incomprehensible magnum opusEinführung in die Gefügekunde der geologischen Körper(An Introduction to the Study of Fabrics of Geological Bodies; 1948-50), eventually made available to a wider audience in a heroic English translation by Phillips, published in 1970.Unfortunately, as time went on, suspicion began to grow amongst structural geologists that Sander's rules were both ambiguous and meaningless as regards the deformation of real rocks. Their application to the Moine, in which the 'girdles' defined by the orientation of the opticc-axes of the quartz crystals in the rock fabric, were found to lie in NNE-SSW planes, perpendicular to the common lineation, led Phillips to the conclusion that 'theoriginof the linear structures is connected with folding due to movements along south-west to north-east lines, earlier than the post-Cambrian displacements . . . . it is the lineation parallel to theb-axis of the fabric which has provided the direction of yield during the later thrust-movements,' a deduction rejected by his contemporaries as inconsistent with the NNE-SSW strike of the Moine rocks. This resulted in Moine petrofabrics becoming embroiled in a long-running controversy. Another principal conclusion of Phillips' work, which subsequently became rather overlooked in the disagreements which arose over movement direction in relation to petrofabric girdles, was his apparent demonstration that the Moine metasediments have a regional metamorphic fabric that pre-dated the Moine Thrust movements and was broken down in the Moine Thrust Zone - a view erroneously taken by H. H. Read as confirming his 1934 hypothesis that the Moines were Lewisian in age.The present depth of understanding of multiple folding (a phenomenon which was unrecognized in 1937) and the complex relationships which can develop between folding, pre-existing lineations, and petrofabrics simply did not exist at the time that Phillips was undertaking his pioneering studies. The on-going controversy regarding the interpretation of Phillips' petrofabric results was initially resolved by D. Flinn's demonstration in 1962 that neither fold axes nor axial planes necessarily indicate movement directions or the directions of flow in rocks, but the situation has only been completely resolved since the mid-1980s, as a result of four crucial findings.(1)Pre-thrusting structures (?Precambrian) have been discovered throughout the Moine rocks of the northern Highlands; these include an early bedding-parallel foliation and a weakly preserved north-south to NNE-SSW trending mineral lineation.(2)The examinations of deformed conglomerates and related fabric studies have convinced many geologists that both the regional WNW-ESE 'stretching' (extension) lineation and its associated quartz c-axis girdles, found by Phillips, result from the WNW-directed Caledonian movements which formed the Moine Thrust.(3)The widespread recognition of sheath folds in the Moine rocks has revealed that fold axes originally formed oblique to the WNW-ESE lineation have often been rotated into parallelism with this lineation during ductile deformation; the geometry and facing directions of the sheath folds and related flow perturbation folds are consistent with top-to-the-WNW-directed thrusting.(4)A continuity of structures has been recognized between (i) the cover rocks and the Lewisian basement, and (ii) the Moine Thrust Zone and the overlying Moine Nappe, which Phillips first recognized but did not interpret correctly.In effect, therefore, Phillips was not entirely wrong but, as Flinn put it, 'right (to some extent) for the wrong reasons', largely because of Sander's confusion between the movement directions of externally applied forces and those of internal movements in response to the applied forces.One of us (R. J. H.) was taught by Phillips (1960–1963), while the other was a colleague of his on the staff at the University of Bristol for ten years (1957–1967). Our critical review of Phillips' research is set in the context of contemporaneous developments in structural and Moine geology. It was promoted by the lack of any obituary notice, or account of his scientific work, by either the Mineralogical Society or The Geological Society of London. It is unfortunate that he died at a time when obituary notices no longer appeared in theProceedings of The Geological Societyand before their present system of including them in theAnnual Reportbegan.Mr W. F. C. Phillips is sincerely thanked for giving us much personal information about his late father, for the loan of his father's Australian diary and photograph album, and for permission to reproduce various photographs; Mrs S. J. C. Toogood is also thanked for permission to reproduce Figure 1.1 and for providing us with useful comments on aspects of her father's life. We are also particularly grateful to Professor Derek Flinn, University of Liverpool, for his most useful comments on aspects of the structural interpretations made by Sander, Phillips, Anderson, and others, and for providing the photograph of the Funzie conglomerate; to Dr Robert E. Holdsworth, University of Durham, for his useful criticism in his role as Geological Society editor and for providing the photograph of the 'eye structure'; to Professor Richard Law, Virginia Polytechnic Institute and State University, USA, for copious information regarding work by himself and his colleagues on the Moine Thrust and for providing the photographs of the Stack of Glencoul and the Moine Thrust; and to Professor Lionel Weiss for providing us with photographs of various Moine structures and the Bygdin conglomerate. Dr G. A. Chinner, Dr G. Evans and Professor I. N. McCave all kindly provided us with additional photographic material. Dr Chinner is also thanked for his personal reminiscences, and for providing us with Dr Henry's notes (1935) of Phillips' lectures on oremicroscopy. Professor Mervyn Paterson, Australian National University,also kindly sent us a copy of his excellent lecture notes made at the time of Phillips' (1952) Australian tour.Dr A. C. Bishop, Dr C. Bowler, Dr R. Bradshaw, Dr G. A. Chinner, Professor W. A. Deer, Professor E. den Tex, Professor D. L. Dineley, Professor D. T. Donovan, Professor G. Evans, Dr R. C. Evans, Professor D. Flinn, Dr D. Goldring, the late Dr P. L. Hancock, Mr W. B. Harland, Dr B. E. Hobbs, Dr M. R. W. Johnson, Dr P. J. Leggo, Professor B. Marshall, Professor J. L. M. Morrison and Mrs O. Morrison, Professor M. S. Paterson, Dr P. A. Sabine, the late Professor R. J. G. Savage, the late Professor R. M. Shackleton, Professor D. J. Shearman, Dr D. Shelley, Professor R. L. Stanton, Professor L. E. Weiss, Professor A. J. R. White and Professor E. H. T. Whitten are all thanked for their personal reminiscences.We would also like to thank A. Allan, Archivist, University of Liverpool; Ms R. Banger, Librarian, Department of Earth Sciences, University of Cambridge; Ms M. Farrar, Cambridge University Archives; D. Freeman, Curator, Royal Geological Society of Cornwall; R. Gillanders, Land Survey Records Officer, British Geological Survey National Geological Records Centre; R. Horrocks, Archivist, Liverpool Record Office; F. J. Jeffery, Archivist, Plymouth College; Dr E. Loeffler, Department of Earth Sciences, University of Bristol; D. P. F. McCallum, Board of Graduate Studies, University of Cambridge; Ms P. M. Mellor, Department of Earth Sciences, University of Sheffield; K. Murphy, Executive Secretary, The Mineralogical Society; Professor J. G. Ramsay; Ms N. Steven, Development and Alumni Relations Office, University of Bristol; the late Dr J. C. Thackray, Archivist, The Geological Society of London; Sir Tony Wrigley, Master, Corpus Christi College, Cambridge; Ms W. Cawthorne and other library staff of The Geological Society of London; and G. Waller, Superintendent of the Manuscripts Reading Room, Cambridge University Library; and in Australia: Associate Professor D. F. Branagan, School of Geosciences, University of Sydney; L. T. Dillon, University Archivist, The University of New South Wales, Sydney; Ms O. Doubrovskaya, Senior Records Officer, University of Technology, Sydney; R. Gurney, University of Sydney Archives; Dr B. Hobbs, Chief, CSIRO Division of Exploration and Mining, Wembley; Professor D. R. Oldroyd, School of Science and Technology Studies, University of New South Wales; and Ms K. Percival, University Archivist, University of Adelaide, for providing us with much useful information. Professors Oldroyd and Branagan, and Dr Peter L. Lowenstein (Zimbabwe) assisted us with determining the location of some of the places visited by Phillips in 1939 and 1953. Stuart Baldwin, Bill George, Wendy Cawthorne, Ms G. Douglas, Librarian and Archivist, Linnean Society, London, and Bob Ellis, Norfolk and Norwich Naturalists' Society, all assisted us to trace the bibliographic reference to Phillips' 1934 Scolt Island study.Graham Chinner, John Cope, John Cosgrove, Derek Flinn, Robert Holdsworth, Michael Johnson, David Oldroyd, John Platt, David Shelley and Jack Soper all provided us with helpful, encouraging (and, in some cases, challenging) comments on various versions of our manuscript.We also thank the following persons and organizations for their permission to use quotations from various letters and sources, and/or permission to reproduce photographs and other illustrative material: The American Geophysical Union,American Journal of Science, Bergen Museum, British Association for the Advancement of Science, Cambridge University Press, Dr G. A. Chinner, Dr J. W. Cosgrove, Professor G. Evans, Dr R. C. Evans, Dr N. Fairbairn, Professor D. Flinn, Gemmological Association, Geological Society of America, Geological Society of London, Professor A. L. Harris, Dr B. Hobbs, Dr M. R. W. Johnson, Professor R. D. Law, Professor G. S. Lister, Professor I. N. McCave, Mineralogical Society,Norsk Geologiske Tidsskrift, Professor M. S. Paterson, Pearson Education Ltd, Mr W. F. C. Phillips, the late Professor N. Rast, Royal Society of Edinburgh, Société Géologique de Belgique, Dr N. J. Soper, Springer-Verlag Ltd, Mrs S. J. C. Toogood, University of Liverpool, Professor L. E. Weiss, John Wiley & Sons Inc., and Mrs J. H. Winchell. We have tried to contact copyright holders (or their literary executors) for permission in all cases and apologize for any omissions where tracing them has not been successful.