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Bibliographic Details
Title:The continental drift controversy
Subdivision:Paleomagnetism and confirmation of drift
Volume 2
From: Henry R. Frankel, University of Missouri - Kansas City
Person: Frankel, Henry R.
1944-2019
Verfasser
aut
Main Author: Frankel, Henry R. 1944-2019 (Author)
Format: Book
Language:English
Published: Cambridge Cambridge University Press 2016
Subjects:
Geschichte
Theorie
Expansionstheorie
Gesteinsmagnetismus
Erdmagnetismus
Paläomagnetismus
Kontinentalverschiebung
Plattentektonik
Erdmagnetisches Feld
Online Access:http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=029844133&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA
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Physical Description:xviii, 525 Seiten Diagramme, Karten
ISBN:9781316616062
9780521875059
Staff View

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adam_text Contents A Foreword by Denis Kent page xi Acknowledgments xiv List of abbreviations xvi Introduction xvii 1 Geomagnetism and paleomagnetism: 1946-1952 1 1.1 Breaking the impasse: the three main paleomagnetic groups 1 1.2 Blackett and Runcorn begin their years together at the University of Manchester (1946-1949) 2 1.3 Blackett s fundamental or distributed theory of the origin of the geomagnetic field and Runcorn’s introduction to it 3 1.4 Elsässer develops a self-exciting dynamo in Earth’s core as the source of the geomagnetic field 5 1.5 Runcorn and colleagues carry out the mine experiment and discriminate between fundamental and core theories 7 1.6 Blackett and Runcorn become interested in paleomagnetism; Runcorn accepts a position at the University of Cambridge 10 1.7 Work at the Carnegie Institution in Washington and the case for a geomagnetic field without gross changes 12 1.8 Graham develops field tests of stability 14 1.9 Graham and others at the Carnegie Institution abandon the fold test 17 1.10 Graham opts for self-reversals rather than field reversals 20 1.11 Igneous baked contact test of stability 23 1.12 Hospers arrives in Cambridge, 1949: his early education and commencement of Iceland surveys 25 1.13 Hospers’ first results from Iceland, 1950-1951, and genesis of Fisher’s statistics 29 1.14 Consistency or dispersion as a test of paleomagnetic stability 31 v 32 34 37 41 43 44 45 46 48 56 56 57 59 60 62 67 68 69 75 80 82 84 88 89 94 94 95 Contents 1.15 Runcorn arrives in Cambridge, 1950, decides to work on paleomagnetism, and hires Ted (E.) Irving, 1951 1.16 Irving’s early education and undergraduate years 1.17 Irving and Runcorn’s first work, July through December 1951: only red beds give coherent results 1.18 Irving devises a paleomagnetism test of continental drift, autumn 1951 1.19 Realization in 1943 by Sahni that paleomagnetism could be used to test continental drift 1.20 Irving initiates his test of motion of India 1.21 Why Runcorn and Irving did not immediately redirect all their work to test continental drift 1.22 Reaction of Blackett and Runcorn to Irving’s work 1.23 Summary British paleomagnetists begin shifting their research toward testing mobilism: summer 1951 to fall 1953 2.1 Outline 2.2 Blackett initiates and Clegg leads the paleomagnetic group at Manchester 2.3 Clegg builds a new magnetometer at Manchester 2.4 The Manchester group expands and focuses on the Triassic redbeds 2.5 Irving investigates the origin of magnetization of the Torridonian and begins magnetostratigraphic survey 2.6 Irving completes magnetostratigraphic survey of the Torridonian 2.7 Fisher defends mobilism 2.8 Hospers returns to Iceland, builds an “igneous” magnetometer, and develops his case for reversals of the geomagnetic field 2.9 Hospers develops the geocentric axial dipole hypothesis and tests polar wandering and continental drift 2.10 Creer, his education and initiation in research 2.11 Creer constructs the Cambridge magnetometer 2.12 Creer begins fieldwork 2.13 Runcorn and his research 2.14 Rationality in deciding to launch a paleomagnetic test for continental drift Launching the global paleomagnetic test of continental drift: 1954-1956 3.1 Paleomagnetists on the move 3.2 Four stages in the paleomagnetic test for continental drift Contents vii 3.3 The January 1954 Birmingham meeting 96 3.4 Irving’s thesis, support of continental drift, and plans for Australia 98 3.5 Clegg and colleagues publish the first paleomagnetic support for continental drift: Stage I 104 3.6 Creer’s 1954 APW path for Britain evolves through three versions: move to Stage II 106 3.7 Creer compares his British APW path with a Silurian pole from North America: move to Stage III 117 3.8 Colorado Plateau, a favored sampling area in 1954 122 3.9 Runcorn’s attitude to mobilism before his first North American survey 125 3.10 Runcorn continues to favor polar wandering after his first North American survey 129 3.11 Paleomagnetism at Australian National University: Jaeger’s key role 131 3.12 Irving’s initial work at Australian National University: his move to Stage IV 134 3.13 Imperial College moves to Stage III 138 3.14 Blackett expresses strong preference for mobilism 141 3.15 Differing reactions of the British and Carnegie groups to the paleomagnetic results 145 4 Runcorn shifts to mobilism: 1955-1956 154 4.1 Runcorn returns to North America then moves to Newcastle 154 4.2 Runcorn hires Opdyke to help collect rocks and they formulate a new paleoclimatologic test of the paleomagnetic method 156 4.3 Runcorn changes his mind and supports continental drift 162 4.4 The Canadian paper 165 4.5 Opinions of others as to why Runcorn changed his mind 168 4.6 False accounts of why Runcorn changed his mind 169 4.7 Westoll’s influence 172 4.8 Creer shows Bradley’s manuscript to Runcorn 175 4.9 Bradley and his paper 178 4.10 Further implications of Runcorn seeing Bradley’s paper 182 4.11 The Dutch paper 187 4.12 Bradley, Runcorn, and Euler’s point theorem 191 4.13 Creer and Irving, Runcorn, and Graham: a study in contrasts 192 5 Enlargement and refinement of the paleomagnetic support for mobilism: 1956-1960 197 5.1 Outline 197 5.2 Imperial College and the Tata Institute continue surveys in India 198 Contents viii 5.3 Australian National University obtains apparent polar wander path for Australia 200 5.4 Surveys of Karroo System through 1959 208 5.5 Magnetic cleaning boosts the record 213 5.6 Survey of South America 218 5.7 Surveys of Antarctica 222 5.8 Surveys in Japan and China 226 5.9 Surveys in the USSR 228 5.10 Paleowind studies, previous work 233 5.11 Paleowind studies, work in Britain in the 1950s 238 5.12 Newcastle begins paleowind studies in North America 239 5.13 Paleowinds, the 1957 Royal Astronomical Society meeting 240 5.14 The Newcastle contribution to paleowind work 243 5.15 A spin-off paleowind study 246 5.16 Attempts at paleogeographies by Newcastle and Canberra groups 247 5.17 The increasing necessity for continental drift 258 5.18 Clarification and further support for the GAD model 259 5.19 Alternative approach of Imperial College group 263 6 Earth expansion enters the mobilist controversy 278 6.1 Outline 278 6.2 Laszlo Egyed and his version of Earth expansion 279 6.3 Holmes assesses Egyed’s expansion theory 282 6.4 Egyed develops his expansion theory and proposes a paleomagnetic test 285 6.5 Carey, the man and his views 290 6.6 Carey’s defense of mobilism 297 6.7 Carey’s oroclines 297 6.8 Carey’s solid but flowing mantle 309 6.9 Examples of rheid flow 312 6.10 Mantle convection as rheid flow 314 6.11 Carey’s fit of Africa and South America 317 6.12 Carey’s views in the 1950s prior to embracing expansionism: his appeal to mantle convection 320 6.13 Carey switches to expansionism 323 6.14 Carey’s account of seafloor generation after he embraced Earth expansion 327 6.15 Carey’s appeal to paleomagnetism 330 6.16 Other contributions to the 1956 Hobart symposium 335 6.17 Jaeger favors mobilism because of its paleomagnetic support 346 Contents ix 7 Development and criticism of the paleomagnetic case for mobilism: late 1950s and early 1960s 355 7.1 Removing difficulties during the development and enlargement of the paleomagnetic case for mobilism 355 7.2 Maintaining standards: quarrels among paleomagnetists supportive of mobilism 359 7.3 Preview of the attacks against paleomagnetic support for mobilism and their defeat 364 7.4 Graham’s magnetostriction difficulty 364 7.5 Removing the magnetostriction difficulty 367 7.6 Cox’s troublesome Siletz River Volcanics 371 7.7 Irving explains the aberrant Siletz paleopole 375 7.8 Other rotations 378 7.9 Hibberd’s rapidly spiraling polar wander paths 380 7.10 Stehli raises a Permian paleobiogeographic difficulty and Runcorn and Irving counter 384 7.11 Munk and MacDonald attack paleomagnetism 389 7.12 Billings attacks paleomagnetic support for mobilism 400 7.13 Jeffreys attacks paleomagnetism and its support for mobilism 402 7.14 Concluding remarks: the prevalence of the three research strategies 404 8 Major reaction against the paleomagnetic case for mobilism and early work on the radiometric reversal timescale: 1958-1962 410 8.1 Introduction 410 8.2 Doell and Cox and their milieu and their attitude toward mobilism before 1958 412 8.3 Genesis of the GSA and AG reviews 422 8.4 The GSA review 424 8.5 Doell and Cox’s earlier attitude to the paleomagnetic case for continental drift 431 8.6 The AG review 434 8.7 Was the GSA review an unreasonable assessment of the paleomagnetic case for mobilism? 438 8.8 Some later reflections on the GSA review 444 8.9 Runcorn’s response to the GSA review 447 8.10 Irving’s response to the GSA review 449 8.11 Cox- Irving correspondence 450 8.12 Irving becomes critical of the GSA review: further Cox-Irving correspondence 453 8.13 Cox reviews Irving’s Paleomagnetism 465 Contents 8.14 Cox and Doell on expansion 466 8.15 Initiation of the radiometric reversal timescale at the United States Geological Survey and the Australian National University 469 8.16 Postscript 484 References 491 Index 511 Resolution of the sixty year debate over continental drift, culminating in the triumph of plate tectonics, changed the very fabric of Earth science. This four-volume treatise on The Continental Drift Controversy is the first complete history of the origin, debate and gradual acceptance of this revolutionary explanation of the structure and motion of the Earth s outer surface. Based on extensive interviews, archival papers, and original works, Frankel weaves together the lives and work of the scientists involved, producing an accessible narrative for scientists and non-scientists alike. Volume 2 - Paleomagnetism and Confirmation of Drift Every historian of 20th Century Earth science will need these volumes close at hand; there is no substitute. EOS The Continental Drift Controversy is undoubtedly the definitive account. It is inconceivable that it can be bettered or even matched at any time in the future. Isis Beginning in the early 1950s, continental drift found new life from an unexpected source, paleomagnetism, which records the Earth s magnetic field in rocks and how its direction and intensity has changed over time. This second volume provides the first extensive account of the growing paleomagnetic case for continental drift and the development of Apparent Polar Wander Paths that showed how the continents had changed their positions relative to one another - more or less as Wegener had proposed. Paleomagnetism offered the first physical measure that continental drift had occurred, and helped determine the changing latitudes of the continents through geologic time. Other volumes in The Continental Drift Controversy: Volume 1 - Wegener and the Early Debate Volume 3 - introduction of Seafloor Spreading Volume 4 - Evolution into Plate Tectonics This is one of the most remarkable histories of science to appear in my lifetime. Earth Sciences History These volumes should be read by all geoscientists serious about understanding how we have come to learn the inner workings of our planet.” Preview Here we have an unparalleled study of remarkable depth, detail and quality of a key development in our ideas about how the Earth functions. Progress in Physical Geography Winner of the Sue Tyler Friedman Medal of The Geological Society of London and the Mary C. Rabbitt History And Philosophy of Geology Award of the Geological Society of America Cover illustration: volcanoes of Bromo National Park, Java, Indonesia. © Manamana / Shutterstock.com Cambridge UNIVERSITY PRESS www.cambridge.org ISBN 978-1-316-61606-2 Cover design by Hart McLeod Ltd I 9 781316 616062
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(DE-588)4191566-5
title The continental drift controversy
title_auth The continental drift controversy
title_exact_search The continental drift controversy
title_full The continental drift controversy Volume 2 Paleomagnetism and confirmation of drift Henry R. Frankel, University of Missouri - Kansas City
title_fullStr The continental drift controversy Volume 2 Paleomagnetism and confirmation of drift Henry R. Frankel, University of Missouri - Kansas City
title_full_unstemmed The continental drift controversy Volume 2 Paleomagnetism and confirmation of drift Henry R. Frankel, University of Missouri - Kansas City
title_short The continental drift controversy
title_sort the continental drift controversy paleomagnetism and confirmation of drift
topic Theorie (DE-588)4059787-8 gnd
Expansionstheorie (DE-588)4204335-9 gnd
Gesteinsmagnetismus (DE-588)4157158-7 gnd
Erdmagnetismus (DE-588)4015173-6 gnd
Paläomagnetismus (DE-588)4173115-3 gnd
Kontinentalverschiebung (DE-588)4032288-9 gnd
Plattentektonik (DE-588)4046317-5 gnd
Erdmagnetisches Feld (DE-588)4191566-5 gnd
topic_facet Theorie
Expansionstheorie
Gesteinsmagnetismus
Erdmagnetismus
Paläomagnetismus
Kontinentalverschiebung
Plattentektonik
Erdmagnetisches Feld
url http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=029844133&sequence=000001&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA
http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&local_base=BVB01&doc_number=029844133&sequence=000002&line_number=0002&func_code=DB_RECORDS&service_type=MEDIA
volume_link (DE-604)BV044443005
work_keys_str_mv AT frankelhenryr thecontinentaldriftcontroversyvolume2
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