The continental drift controversy . Volume 1 Wegener and the early debate / / Henry R. Frankel [[electronic resource]] |
Autore | Frankel Henry R. <1944-> |
Pubbl/distr/stampa | Cambridge : , : Cambridge University Press, , 2012 |
Descrizione fisica | 1 online resource (xxii, 604 pages) : digital, PDF file(s) |
Disciplina | 551.1/36 |
Soggetto topico |
Continental drift - Research - History - 20th century
Academic disputations - History - 20th century |
ISBN |
1-107-21879-9
1-280-64733-7 9786613633385 1-139-37815-5 1-139-37529-6 0-511-84236-8 1-139-37672-1 1-139-37130-4 1-139-37958-5 |
Formato | Materiale a stampa |
Livello bibliografico | Monografia |
Lingua di pubblicazione | eng |
Nota di contenuto |
Cover; THE CONTINENTAL DRIFT CONTROVERSY; Dedication; Title; Copyright; Contents; Foreword; Acknowledgements; Abbreviations; Introduction; Notes; 1: How the mobilism debate was structured; 1.1 The three phases of the continental drift controversy; 1.2 Solutions, theories, hypotheses, and ideas or concepts; 1.3 Problems and difficulties; 1.4 First and second stage problems; 1.5 Four examples of first stage problems; 1.6 Four examples of second stage problems; 1.7 Difficulties; 1.8 Unreliability difficulties; 1.9 Anomaly difficulties; 1.10 Missing-data difficulties
1.11 Theoretical difficulties1.12 Difficulty-free solutions; 1.13 The three research strategies and how they gave structure to the debate; 1.14 Specialization and regionalism in the Earth sciences; 1.15 Why regionalism and specialization affected theory preference during the mobilist debate; Notes; 2: Wegener and Taylor develop their theories of continental drift; 2.1 Introduction; 2.2 Geological theorizing at the turn of the twentieth century; 2.3 The contractionism of Suess; 2.4 The reception of Suess' contractionism and the difficulties it encountered; 2.5 Wegener the man 2.6 Wegener's 1912 theory of partition and horizontal displacement of continents, from idea to working hypothesis2.7 Wegener presents and defends his drift theory in 1912: his six major arguments; 2.8 Wegener's further arguments in 1912; 2.9 Taylor and his career; 2.10 The emergence of Taylor's theory of creep and horizontal displacement; 2.11 Taylor's cosmogony and his notion of continental drift, 1898; 2.12 Taylor's 1910 presentation and defense of his creep and drift theory; 2.13 Wegener and Taylor: the independence of their inspiration; 2.14 Wegener and Taylor compared 2.15 Evolution of Wegener's theory, 1912-1922Notes; 3: Sub-controversies in the drift debate: 1920s-1950s; 3.1 Introduction; 3.2 Wegener's theory as presented in 1922; 3.3 Biotic disjuncts and Wegener's 1922 explanation of them; 3.4 Landbridgers revise and rebut; 3.5 Mobilists rally increasing support for continental drift; 3.6 The resurgence of American permanentism: isthmian links; 3.7 Du Toit, Simpson, and Longwell debate; 3.8 Support for permanentism continues through the mid-1950s; 3.9 Questioning reliability and completeness of the biogeographical record 3.10 Permo-Carboniferous glaciation: Wegener's 1922 solutionkey support for Wegener; 3.11 Permo-Carboniferous glaciation: fixists attack Wegener's solution and refurbish their own; 3.12 Permo-Carboniferous glaciation: mobilists counterattack; 3.13 The geodetic sub-controversy over the westward drift of Greenland; 3.14 Use of research strategies in the three sub-controversies; 3.15 Köppen and Wegener determine ancient latitudes; Notes; 4: The mechanism sub-controversy: 1921-1951; 4.1 Introduction; 4.2 Wegener's 1922 mechanism; 4.3 Wegener's mechanism attacked: 1921 through 1926 4.4 Van der Gracht modifies Wegener's mechanism |
Record Nr. | UNINA-9910451982303321 |
Frankel Henry R. <1944-> | ||
Cambridge : , : Cambridge University Press, , 2012 | ||
Materiale a stampa | ||
Lo trovi qui: Univ. Federico II | ||
|
The continental drift controversy . Volume 3 Introduction of seafloor spreading / / Henry R. Frankel [[electronic resource]] |
Autore | Frankel Henry R. <1944-> |
Pubbl/distr/stampa | Cambridge : , : Cambridge University Press, , 2012 |
Descrizione fisica | 1 online resource (xvi, 476 pages) : digital, PDF file(s) |
Disciplina | 551.1/36 |
Soggetto topico |
Continental drift - Research - History - 20th century
Academic disputations - History - 20th century |
ISBN |
1-139-36564-9
1-107-22590-6 1-280-64735-3 9786613633408 1-139-37817-1 1-139-02541-4 1-139-37531-8 1-139-37674-8 1-139-37960-7 1-139-37132-0 |
Formato | Materiale a stampa |
Livello bibliografico | Monografia |
Lingua di pubblicazione | eng |
Nota di contenuto |
Cover; THE CONTINENTAL DRIFT CONTROVERSY: Volume III: Introduction of Seafloor Spreading; Dedication; Title; Copyright; Contents; Foreword; Acknowledgments; Abbreviations; Introduction; 1: Extension and reception of paleomagnetic/paleoclimatic support for mobilism: 1960-1966; 1.1 Introduction; 1.2 Dott reexamines the Squantum Tillite; 1.3 Comparisons of paleomagnetic and paleoclimatic evidence: the 1959 Newcastle symposium and its 1961 publication Descriptive Palaeoclimatology; 1.4 Reviews of Descriptive Palaeoclimatology; 1.5 Speculations on mechanism in the early 1960s
1.6 The 1962 anthology Continental Drift and MacDonald's review of it1.7 Blackett turns to paleoclimatology; 1.8 Deutsch proposes continental drift without polar wandering; 1.9 The 1963 Newcastle NATO conference; 1.10 Bucher continues to criticize mobilism at the NATO conference; 1.11 Harland and Rudwick link mobilism, the Great Infra-Cambrian Ice Age and the burgeoning of Cambrian fauna; 1.12 Responses of some biogeographers to the paleomagnetic case for continental drift; 1.13 Hamilton welcomes paleomagnetism's support of mobilism 1.14 Kay and Colbert reassess mobilism because of its paleomagnetic support1.15 Japanese rock magnetists avoid accepting the paleomagnetic case for mobilism; 1.16 Further poles from Australia, 1958-1964; 1.17 Further poles from Africa: the Salisbury (Harare) Group and further work at the Bernard Price Institute, Johannesburg, 1959-1964; 1.18 Convergence of paleomagnetism and paleoclimatology at Canberra, 1959-1966; Notes; 2: Reception of the paleomagnetic case for mobilism by several notables: 1957-1965; 2.1 Introduction; 2.2 Gutenberg's career 2.3 Gutenberg supports mobilism during the 1920s and 1930s2.4 In the 1950s Gutenberg reconsiders mobilism and appeals to paleomagnetism; 2.5 Vening Meinesz reconsiders mobilism; 2.6 Vening Meinesz becomes favorably inclined toward mobilism because of its paleomagnetic support; 2.7 MacDonald denies mantle convection and Runcorn responds; 2.8 MacDonald renews his attack on the paleomagnetic case for mobilism; 2.9 Harold Jeffreys, his career; 2.10 Jeffreys renews his attack on mobilism in the first Harold Jeffreys Lecture; 2.11 Bullard's journey to mobilism: his early career 2.12 Bullard considers mantle convection and measures ocean floor heat flow2.13 Bullard begins to consider mobilism seriously; 2.14 Bullard recognizes that all obstacles to the paleomagnetic case had been removed and becomes a mobilist; 2.15 Bullard squabbles with geologists about the contributions of geology and geophysics to the mobilism debate; 2.16 Arthur Holme's attitude to the paleomagnetic case for mobilism; 2.17 Mobilism's solution to divergent APW paths, its difficulty-free status 2.18 On the general failure to recognize the difficulty-free status of the paleomagnetic case for mobilism |
Record Nr. | UNINA-9910452005303321 |
Frankel Henry R. <1944-> | ||
Cambridge : , : Cambridge University Press, , 2012 | ||
Materiale a stampa | ||
Lo trovi qui: Univ. Federico II | ||
|
The continental drift controversy . Volume 4 Evolution into plate tectonics / / Henry R. Frankel [[electronic resource]] |
Autore | Frankel Henry R. <1944-> |
Pubbl/distr/stampa | Cambridge : , : Cambridge University Press, , 2012 |
Descrizione fisica | 1 online resource (xix, 675 pages) : digital, PDF file(s) |
Disciplina | 551.1/36 |
Soggetto topico |
Continental drift - Research - History - 20th century
Academic disputations - History - 20th century |
ISBN |
1-139-36630-0
1-107-23119-1 1-280-77361-8 9786613684387 1-139-37889-9 1-139-09593-5 1-139-37603-9 1-139-37204-1 1-139-37746-9 1-139-38032-X |
Formato | Materiale a stampa |
Livello bibliografico | Monografia |
Lingua di pubblicazione | eng |
Nota di contenuto | Cover; THE CONTINENTAL DRIFT CONTROVERSY; Dedication; Title; Copyright; Index |
Record Nr. | UNINA-9910462424403321 |
Frankel Henry R. <1944-> | ||
Cambridge : , : Cambridge University Press, , 2012 | ||
Materiale a stampa | ||
Lo trovi qui: Univ. Federico II | ||
|
The continental drift controversy . Volume 2 Paleomagnetism and confirmation of drift / / Henry R. Frankel [[electronic resource]] |
Autore | Frankel Henry R. <1944-> |
Pubbl/distr/stampa | Cambridge : , : Cambridge University Press, , 2012 |
Descrizione fisica | 1 online resource (xviii, 525 pages) : digital, PDF file(s) |
Disciplina | 551.1/36 |
Soggetto topico |
Continental drift - Research - History - 20th century
Academic disputations - History - 20th century |
ISBN |
1-139-36563-0
1-107-22589-2 1-280-64734-5 9786613633392 1-139-37816-3 1-139-37530-X 0-511-84316-X 1-139-37673-X 1-139-37959-3 1-139-37131-2 |
Formato | Materiale a stampa |
Livello bibliografico | Monografia |
Lingua di pubblicazione | eng |
Nota di contenuto |
Cover; THE CONTINENTAL DRIFT CONTROVERSY: Volume II: Paleomagnetism and Confirmation of Drift; Dedication; Title; Copyright; Contents; Foreword; Introduction; Acknowledgments; Abbreviations; Note; 1: Geomagnetism and paleomagnetism: 1946-1952; 1.1 Breaking the impasse: the three main paleomagnetic groups; 1.2 Blackett and Runcorn begin their years together at the University of Manchester (1946-1949); 1.3 Blackett's fundamental or distributed theory of the origin of the geomagnetic field and Runcorn's introduction to it
1.4 Elsasser develops a self-exciting dynamo in Earth's core as the source of the geomagnetic field1.5 Runcorn and colleagues carry out the mine experiment and discriminate between fundamental and core theories; 1.6 Blackett and Runcorn become interested in paleomagnetism; Runcorn accepts a position at the University of Cambridge; 1.7 Work at the Carnegie Institution in Washington and the case for a geomagnetic field without gross changes; 1.8 Graham develops field tests of stability; 1.9 Graham and others at the Carnegie Institution abandon the fold test 1.10 Graham opts for self-reversals rather than field reversals1.11 Igneous baked contact test of stability; 1.12 Hospers arrives in Cambridge, 1949: his early education and commencement of Iceland surveys; 1.13 Hospers' first results from Iceland, 1950-1951, and genesis of Fisher's statistics; 1.14 Consistency or dispersion as a test of paleomagnetic stability; 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 results1.18 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; Notes 2: British paleomagnetists begin shifting their research toward testing mobilism: summer 1951 to fall 19532.1 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 |
Record Nr. | UNINA-9910452246303321 |
Frankel Henry R. <1944-> | ||
Cambridge : , : Cambridge University Press, , 2012 | ||
Materiale a stampa | ||
Lo trovi qui: Univ. Federico II | ||
|
The continental drift controversy . Volume 4 Evolution into plate tectonics / / Henry R. Frankel [[electronic resource]] |
Autore | Frankel Henry R. <1944-> |
Pubbl/distr/stampa | Cambridge : , : Cambridge University Press, , 2012 |
Descrizione fisica | 1 online resource (xix, 675 pages) : digital, PDF file(s) |
Disciplina | 551.1/36 |
Soggetto topico |
Continental drift - Research - History - 20th century
Academic disputations - History - 20th century |
ISBN |
1-139-36630-0
1-107-23119-1 1-280-77361-8 9786613684387 1-139-37889-9 1-139-09593-5 1-139-37603-9 1-139-37204-1 1-139-37746-9 1-139-38032-X |
Formato | Materiale a stampa |
Livello bibliografico | Monografia |
Lingua di pubblicazione | eng |
Nota di contenuto | Cover; THE CONTINENTAL DRIFT CONTROVERSY; Dedication; Title; Copyright; Index |
Record Nr. | UNINA-9910790352103321 |
Frankel Henry R. <1944-> | ||
Cambridge : , : Cambridge University Press, , 2012 | ||
Materiale a stampa | ||
Lo trovi qui: Univ. Federico II | ||
|
The continental drift controversy . Volume 3 Introduction of seafloor spreading / / Henry R. Frankel [[electronic resource]] |
Autore | Frankel Henry R. <1944-> |
Pubbl/distr/stampa | Cambridge : , : Cambridge University Press, , 2012 |
Descrizione fisica | 1 online resource (xvi, 476 pages) : digital, PDF file(s) |
Disciplina | 551.1/36 |
Soggetto topico |
Continental drift - Research - History - 20th century
Academic disputations - History - 20th century |
ISBN |
1-139-36564-9
1-107-22590-6 1-280-64735-3 9786613633408 1-139-37817-1 1-139-02541-4 1-139-37531-8 1-139-37674-8 1-139-37960-7 1-139-37132-0 |
Formato | Materiale a stampa |
Livello bibliografico | Monografia |
Lingua di pubblicazione | eng |
Nota di contenuto |
Cover; THE CONTINENTAL DRIFT CONTROVERSY: Volume III: Introduction of Seafloor Spreading; Dedication; Title; Copyright; Contents; Foreword; Acknowledgments; Abbreviations; Introduction; 1: Extension and reception of paleomagnetic/paleoclimatic support for mobilism: 1960-1966; 1.1 Introduction; 1.2 Dott reexamines the Squantum Tillite; 1.3 Comparisons of paleomagnetic and paleoclimatic evidence: the 1959 Newcastle symposium and its 1961 publication Descriptive Palaeoclimatology; 1.4 Reviews of Descriptive Palaeoclimatology; 1.5 Speculations on mechanism in the early 1960s
1.6 The 1962 anthology Continental Drift and MacDonald's review of it1.7 Blackett turns to paleoclimatology; 1.8 Deutsch proposes continental drift without polar wandering; 1.9 The 1963 Newcastle NATO conference; 1.10 Bucher continues to criticize mobilism at the NATO conference; 1.11 Harland and Rudwick link mobilism, the Great Infra-Cambrian Ice Age and the burgeoning of Cambrian fauna; 1.12 Responses of some biogeographers to the paleomagnetic case for continental drift; 1.13 Hamilton welcomes paleomagnetism's support of mobilism 1.14 Kay and Colbert reassess mobilism because of its paleomagnetic support1.15 Japanese rock magnetists avoid accepting the paleomagnetic case for mobilism; 1.16 Further poles from Australia, 1958-1964; 1.17 Further poles from Africa: the Salisbury (Harare) Group and further work at the Bernard Price Institute, Johannesburg, 1959-1964; 1.18 Convergence of paleomagnetism and paleoclimatology at Canberra, 1959-1966; Notes; 2: Reception of the paleomagnetic case for mobilism by several notables: 1957-1965; 2.1 Introduction; 2.2 Gutenberg's career 2.3 Gutenberg supports mobilism during the 1920s and 1930s2.4 In the 1950s Gutenberg reconsiders mobilism and appeals to paleomagnetism; 2.5 Vening Meinesz reconsiders mobilism; 2.6 Vening Meinesz becomes favorably inclined toward mobilism because of its paleomagnetic support; 2.7 MacDonald denies mantle convection and Runcorn responds; 2.8 MacDonald renews his attack on the paleomagnetic case for mobilism; 2.9 Harold Jeffreys, his career; 2.10 Jeffreys renews his attack on mobilism in the first Harold Jeffreys Lecture; 2.11 Bullard's journey to mobilism: his early career 2.12 Bullard considers mantle convection and measures ocean floor heat flow2.13 Bullard begins to consider mobilism seriously; 2.14 Bullard recognizes that all obstacles to the paleomagnetic case had been removed and becomes a mobilist; 2.15 Bullard squabbles with geologists about the contributions of geology and geophysics to the mobilism debate; 2.16 Arthur Holme's attitude to the paleomagnetic case for mobilism; 2.17 Mobilism's solution to divergent APW paths, its difficulty-free status 2.18 On the general failure to recognize the difficulty-free status of the paleomagnetic case for mobilism |
Record Nr. | UNINA-9910779151603321 |
Frankel Henry R. <1944-> | ||
Cambridge : , : Cambridge University Press, , 2012 | ||
Materiale a stampa | ||
Lo trovi qui: Univ. Federico II | ||
|
The continental drift controversy . Volume 2 Paleomagnetism and confirmation of drift / / Henry R. Frankel [[electronic resource]] |
Autore | Frankel Henry R. <1944-> |
Pubbl/distr/stampa | Cambridge : , : Cambridge University Press, , 2012 |
Descrizione fisica | 1 online resource (xviii, 525 pages) : digital, PDF file(s) |
Disciplina | 551.1/36 |
Soggetto topico |
Continental drift - Research - History - 20th century
Academic disputations - History - 20th century |
ISBN |
1-139-36563-0
1-107-22589-2 1-280-64734-5 9786613633392 1-139-37816-3 1-139-37530-X 0-511-84316-X 1-139-37673-X 1-139-37959-3 1-139-37131-2 |
Formato | Materiale a stampa |
Livello bibliografico | Monografia |
Lingua di pubblicazione | eng |
Nota di contenuto |
Cover; THE CONTINENTAL DRIFT CONTROVERSY: Volume II: Paleomagnetism and Confirmation of Drift; Dedication; Title; Copyright; Contents; Foreword; Introduction; Acknowledgments; Abbreviations; Note; 1: Geomagnetism and paleomagnetism: 1946-1952; 1.1 Breaking the impasse: the three main paleomagnetic groups; 1.2 Blackett and Runcorn begin their years together at the University of Manchester (1946-1949); 1.3 Blackett's fundamental or distributed theory of the origin of the geomagnetic field and Runcorn's introduction to it
1.4 Elsasser develops a self-exciting dynamo in Earth's core as the source of the geomagnetic field1.5 Runcorn and colleagues carry out the mine experiment and discriminate between fundamental and core theories; 1.6 Blackett and Runcorn become interested in paleomagnetism; Runcorn accepts a position at the University of Cambridge; 1.7 Work at the Carnegie Institution in Washington and the case for a geomagnetic field without gross changes; 1.8 Graham develops field tests of stability; 1.9 Graham and others at the Carnegie Institution abandon the fold test 1.10 Graham opts for self-reversals rather than field reversals1.11 Igneous baked contact test of stability; 1.12 Hospers arrives in Cambridge, 1949: his early education and commencement of Iceland surveys; 1.13 Hospers' first results from Iceland, 1950-1951, and genesis of Fisher's statistics; 1.14 Consistency or dispersion as a test of paleomagnetic stability; 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 results1.18 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; Notes 2: British paleomagnetists begin shifting their research toward testing mobilism: summer 1951 to fall 19532.1 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 |
Record Nr. | UNINA-9910779289003321 |
Frankel Henry R. <1944-> | ||
Cambridge : , : Cambridge University Press, , 2012 | ||
Materiale a stampa | ||
Lo trovi qui: Univ. Federico II | ||
|
The continental drift controversy . Volume 4 Evolution into plate tectonics / / Henry R. Frankel |
Autore | Frankel Henry R. <1944-> |
Edizione | [1st ed.] |
Pubbl/distr/stampa | Cambridge ; ; New York, : Cambridge University Press, 2012 |
Descrizione fisica | 1 online resource (xix, 675 pages) : digital, PDF file(s) |
Disciplina | 551.1/36 |
Soggetto topico |
Continental drift - Research - History - 20th century
Continental drift - History - 20th century Plate tectonics - History Academic disputations - History - 20th century Geodynamics - Philosophy - History - 20th century Geology, Structural - Philosophy - History - 20th century |
ISBN |
1-139-36630-0
1-107-23119-1 1-280-77361-8 9786613684387 1-139-37889-9 1-139-09593-5 1-139-37603-9 1-139-37204-1 1-139-37746-9 1-139-38032-X |
Formato | Materiale a stampa |
Livello bibliografico | Monografia |
Lingua di pubblicazione | eng |
Nota di contenuto | Cover; THE CONTINENTAL DRIFT CONTROVERSY; Dedication; Title; Copyright; Index |
Altri titoli varianti | Evolution into plate tectonics |
Record Nr. | UNINA-9910807330003321 |
Frankel Henry R. <1944-> | ||
Cambridge ; ; New York, : Cambridge University Press, 2012 | ||
Materiale a stampa | ||
Lo trovi qui: Univ. Federico II | ||
|
The continental drift controversy . Volume 2 Paleomagnetism and confirmation of drift / / Henry R. Frankel |
Autore | Frankel Henry R. <1944-> |
Edizione | [1st ed.] |
Pubbl/distr/stampa | Cambridge ; ; New York, : Cambridge University Press, 2012 |
Descrizione fisica | 1 online resource (xviii, 525 pages) : digital, PDF file(s) |
Disciplina | 551.1/36 |
Soggetto topico |
Paleomagnetism
Continental drift - Research - History - 20th century |
ISBN |
1-139-36563-0
1-107-22589-2 1-280-64734-5 9786613633392 1-139-37816-3 1-139-37530-X 0-511-84316-X 1-139-37673-X 1-139-37959-3 1-139-37131-2 |
Formato | Materiale a stampa |
Livello bibliografico | Monografia |
Lingua di pubblicazione | eng |
Nota di contenuto |
Cover; THE CONTINENTAL DRIFT CONTROVERSY: Volume II: Paleomagnetism and Confirmation of Drift; Dedication; Title; Copyright; Contents; Foreword; Introduction; Acknowledgments; Abbreviations; Note; 1: Geomagnetism and paleomagnetism: 1946-1952; 1.1 Breaking the impasse: the three main paleomagnetic groups; 1.2 Blackett and Runcorn begin their years together at the University of Manchester (1946-1949); 1.3 Blackett's fundamental or distributed theory of the origin of the geomagnetic field and Runcorn's introduction to it
1.4 Elsasser develops a self-exciting dynamo in Earth's core as the source of the geomagnetic field1.5 Runcorn and colleagues carry out the mine experiment and discriminate between fundamental and core theories; 1.6 Blackett and Runcorn become interested in paleomagnetism; Runcorn accepts a position at the University of Cambridge; 1.7 Work at the Carnegie Institution in Washington and the case for a geomagnetic field without gross changes; 1.8 Graham develops field tests of stability; 1.9 Graham and others at the Carnegie Institution abandon the fold test 1.10 Graham opts for self-reversals rather than field reversals1.11 Igneous baked contact test of stability; 1.12 Hospers arrives in Cambridge, 1949: his early education and commencement of Iceland surveys; 1.13 Hospers' first results from Iceland, 1950-1951, and genesis of Fisher's statistics; 1.14 Consistency or dispersion as a test of paleomagnetic stability; 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 results1.18 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; Notes 2: British paleomagnetists begin shifting their research toward testing mobilism: summer 1951 to fall 19532.1 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 |
Record Nr. | UNINA-9910815403903321 |
Frankel Henry R. <1944-> | ||
Cambridge ; ; New York, : Cambridge University Press, 2012 | ||
Materiale a stampa | ||
Lo trovi qui: Univ. Federico II | ||
|
The continental drift controversy . Volume 3 Introduction of seafloor spreading / / Henry R. Frankel |
Autore | Frankel Henry R. <1944-> |
Edizione | [1st ed.] |
Pubbl/distr/stampa | Cambridge ; ; New York, : Cambridge University Press, 2012 |
Descrizione fisica | 1 online resource (xvi, 476 pages) : digital, PDF file(s) |
Disciplina | 551.1/36 |
Soggetto topico |
Academic disputations - History - 20th century
Continental drift - Research - History - 20th century |
ISBN |
1-139-36564-9
1-107-22590-6 1-280-64735-3 9786613633408 1-139-37817-1 1-139-02541-4 1-139-37531-8 1-139-37674-8 1-139-37960-7 1-139-37132-0 |
Formato | Materiale a stampa |
Livello bibliografico | Monografia |
Lingua di pubblicazione | eng |
Nota di contenuto |
Cover; THE CONTINENTAL DRIFT CONTROVERSY: Volume III: Introduction of Seafloor Spreading; Dedication; Title; Copyright; Contents; Foreword; Acknowledgments; Abbreviations; Introduction; 1: Extension and reception of paleomagnetic/paleoclimatic support for mobilism: 1960-1966; 1.1 Introduction; 1.2 Dott reexamines the Squantum Tillite; 1.3 Comparisons of paleomagnetic and paleoclimatic evidence: the 1959 Newcastle symposium and its 1961 publication Descriptive Palaeoclimatology; 1.4 Reviews of Descriptive Palaeoclimatology; 1.5 Speculations on mechanism in the early 1960s
1.6 The 1962 anthology Continental Drift and MacDonald's review of it1.7 Blackett turns to paleoclimatology; 1.8 Deutsch proposes continental drift without polar wandering; 1.9 The 1963 Newcastle NATO conference; 1.10 Bucher continues to criticize mobilism at the NATO conference; 1.11 Harland and Rudwick link mobilism, the Great Infra-Cambrian Ice Age and the burgeoning of Cambrian fauna; 1.12 Responses of some biogeographers to the paleomagnetic case for continental drift; 1.13 Hamilton welcomes paleomagnetism's support of mobilism 1.14 Kay and Colbert reassess mobilism because of its paleomagnetic support1.15 Japanese rock magnetists avoid accepting the paleomagnetic case for mobilism; 1.16 Further poles from Australia, 1958-1964; 1.17 Further poles from Africa: the Salisbury (Harare) Group and further work at the Bernard Price Institute, Johannesburg, 1959-1964; 1.18 Convergence of paleomagnetism and paleoclimatology at Canberra, 1959-1966; Notes; 2: Reception of the paleomagnetic case for mobilism by several notables: 1957-1965; 2.1 Introduction; 2.2 Gutenberg's career 2.3 Gutenberg supports mobilism during the 1920s and 1930s2.4 In the 1950s Gutenberg reconsiders mobilism and appeals to paleomagnetism; 2.5 Vening Meinesz reconsiders mobilism; 2.6 Vening Meinesz becomes favorably inclined toward mobilism because of its paleomagnetic support; 2.7 MacDonald denies mantle convection and Runcorn responds; 2.8 MacDonald renews his attack on the paleomagnetic case for mobilism; 2.9 Harold Jeffreys, his career; 2.10 Jeffreys renews his attack on mobilism in the first Harold Jeffreys Lecture; 2.11 Bullard's journey to mobilism: his early career 2.12 Bullard considers mantle convection and measures ocean floor heat flow2.13 Bullard begins to consider mobilism seriously; 2.14 Bullard recognizes that all obstacles to the paleomagnetic case had been removed and becomes a mobilist; 2.15 Bullard squabbles with geologists about the contributions of geology and geophysics to the mobilism debate; 2.16 Arthur Holme's attitude to the paleomagnetic case for mobilism; 2.17 Mobilism's solution to divergent APW paths, its difficulty-free status 2.18 On the general failure to recognize the difficulty-free status of the paleomagnetic case for mobilism |
Record Nr. | UNINA-9910810365603321 |
Frankel Henry R. <1944-> | ||
Cambridge ; ; New York, : Cambridge University Press, 2012 | ||
Materiale a stampa | ||
Lo trovi qui: Univ. Federico II | ||
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