Timescales of the Geomagnetic Field (March 9-11, Sunday- Tuesday)
|
|
- Stephanie Warren
- 6 years ago
- Views:
Transcription
1 AGU Chapman Conference Timescales of the Geomagnetic Field (March 9-11, Sunday- Tuesday) Bless Auditorium, Williamson Hall, University of Florida (First author is the presenter unless another author is underlined) DAY 1, March 9 (Chair: Clement/Tauxe) INTRODUCTION KEYNOTE 1 (25+5) Irving and Hebda Contributions to the study of the Origin and Distribution of Magnolias from Paleomagnetism SPEAKER 1 (15+5) Van der Voo and Torsvik, Long-term Phanerozoic Octupole Fields SPEAKER 2 (15+5) Besse and Oufi Paleomagnetic survey of Late Permian series in Morocco: implications for Pangea reconstruction and GAD Hypothesis COFFEE BREAK (30 MIN) SPEAKER 3 (15+5) Muttoni et al., Early Permian Pangea B to Late Permian Pangea A SPEAKER 4 (15+5) Besse and Courtillot, Apparent and True Polar Wander and the Geometry of the Geomagnetic Field in the Last 200 Million Years SPEAKER 5 (15+5) D. Evans and Raub. Can a Persistently Nonuniformitarian Neoproterozoic-Cambrian Geomagnetic Field Explain Rapid and Oscillatory APW Motions? SPEAKER 6 (15+5) Kirschvink et al. On the paleoposition of North America in mid-vendian through Cambrian time: A Restudy of the Sept Îles and Pointe du Criarde Intrusive Suites, Quebec, Canada SPEAKER 7 (15+5) Meert et al., Non-Dipole Fields and Inclination Analysis: What is the low Inclination Bias Really Telling us? POSTERS KEYNOTE 2 (25+5) McElhinny The Geocentric Axial Dipole Hypothesis - Current Status SPEAKER 8 (15+5) Constable and Johnson The Spectrum of Geomagnetic Temporal Variations SPEAKER 9 (15+5) Johnson and Constable Testing the GAD Hypothesis: Lava Flow Records from 0-5Ma.
2 SPEAKER 10 (15+5) Torsvik and Van der Voo, A Comparison of Hotspot and Palaeomagnetic frames (0-95 Ma) and Estimates of non-dipole Fields SPEAKER 11 (15+5) Yamazaki and Oda, Persistent Non-dipole Components and Intensity-Inclination Correlation SPEAKER 12 (15+5) Opdyke and Mejia, Earth's Magnetic Field 1830 Bar-B-Que at Keene Faculty Center (Campus) Day 2, March 10 (Chair: McElhinny/Irving) KEYNOTE 1 (25+5) Coe and Glen, Short-Term Changes in the Geomagnetic Field: High-Resolution Records and the Relation to Geodynamo Simulations SPEAKER 2 (15+5) Langereis, Reversal Excursions and the Future of High(er) Resolution Correlation SPEAKER 3 (15+5) Krijgsman, Occurrence of Short-Lived Geomagnetic Features Through Time: the Late Miocene -Pliocene gap? COFFEE BREAK (40 MIN) SPEAKER 4 (15+5) Thouveny et al., Geomagnetic Moment Variation and Excursions Since 400 ka BP: Paleomagnetic and Authigenic 10Be/9Be Sedimentary Records from the Portuguese Margin SPEAKER 5 (15+5) Acton et al., Brunhes Geomagnetic and Rock Magnetic Variations Recorded in Eight Holes Cored at ODP Site 1062 on the Bahama Outer Ridge SPEAKER 6 (15+5) Laj et al., High Resolution Global Paleointensity Stack Since 75 kyrs (GLOPIS-75) Calibrated to Absolute Values SPEAKER 7 (15+5) Stoner et al., Timescales of Variability of the Geomagnetic Field: New Constraints From High Resolution Continental Margin Sediments SPEAKER 8 (15+5) Herrero-Brevera and Valet, Paleomagnetism, Paleosecular Variation, Successive Reversals and Absolute Paleointensities Recorded in the Ko'olau and Wai'anae Volcanoes, O'ahu, Hawai'I POSTERS KEYNOTE 2 (25+5) Gubbins, Low Secular Variation in the Pacific SPEAKER 9 (15+5) Roberts and Donald, Report on Some Preliminary Attempts to Improve the on the Realism of Geodynamo Simulations SPEAKER 10 (15+5) Hoffman Regionally Recurring Transitional Field Structures: Further Evidence of Mantle Control Over the Geodynamo SPEAKER 11 (15+5) Harrison A Source Model for the Geomagnetic Field SPEAKER 12 (15+5) Baker and Aldridge Paleomagnetic Intensity Data as a Time Series: Opening a Window Into Dynamics of Earth's Fluid Core?
3 SPEAKER 13 (15+5) Heirtzler, Geomagnetic Field During a Reversal 1900 Banquet at Soveriegn Restaurant (12 SE 2 nd Ave) Speaker: Walter Pitman Day 3, March 11 (Chair: Kent/Torsvik) KEYNOTE 1 (25+5) Larson, Characteristics of the Geomagnetic Field From the Present to the Middle Jurassic: The Perspective From Marine Magnetic Anomalies SPEAKER 1 (15+5) Tauxe and Staudigel, Strength of the Geomagnetic Field in the Cretaceous Normal Superchron: New Data from Submarine Basaltic Glass of the Troodos Ophiolite SPEAKER 2 (15+5) Tarduno et al., The Long-term Nature of the Geodynamo Based on Coupled Analyses of Paleointensity and Paleosecular Variation COFFEE BREAK (40 MIN) SPEAKER 3 (15+5) Dunlop and Yu, Intensity of the Geomagnetic Field During Precambrian Time SPEAKER 4 (15+5) Valet et al. Integration of Paleointensity Data SPEAKER 5 (15+5) Gallet and Pavlov, Third Superchron During the Early Paleozoic? SPEAKER 6 (15+5) Musgrave and Fussell, A Snapshot of Secular Variation Near the Start of the Kiaman Superchron SPEAKER 7 (15+5) Lanci et al., Cryptochrons and Brief Subchrons Recorded at ODP Site 1218 (Equatorial Pacific) POSTERS + LAB VISITS KEYNOTE 2 (25+5) Lowrie, Magnetic Stratigraphy and Geomagnetic Reversal History SPEAKER 8 (15+5) MacFadden, Magnetic Reversals and Old Bones: Opdyke's Contributions to Cenozoic Mammal Evolution SPEAKER 9 (15+5) Clement, How long does it take for Earth's magnetic field to reverse polarity? SPEAKER 10 (15+5) Sager and Tivey, Deep-Tow Investigations of 'Tiny Wiggles' in the Western Pacific Jurassic "Quiet Zone" SPEAKER 11 (15+5) Steiner, Ultra-fast geomagnetic field reversals in the mid-jurassic: ~10,000 yr polarity intervals recorded by Jurassic quiet zone crust SPEAKER 12 (15+5) Pares and Van der Voo, Tiny wiggles in the Cenozoic Magnetic Record: Short Polarity Events Obscured by Intensity Fluctuations? PUBLICATION PLANNING
4 1830 Reception at Florida Museum of Natural History (Powell Hall, Hull Road & SW 34 St.) POSTERS (25 POSTERS) displayed throughout the meeting on 6 x 4 ft poster boards 1) Raub and Kirschvink, A pdrm Model Including Bioturbation by Macrofauna and Meiofauna, and Microbial Diagenesis: Time-Averaged Magnetizations Require One- Tier Sampling and Statistics. 2) Rutter and M. Evans, The Use of Quaternary Magnetostratigraphy in Long Distance Correlation and Depositional Processes 3) Sternberg et al., A Pilot Paleointensity Study of 19th and 20th Century Bricks from the New York City Area 4) Yamamoto, Possible Overestimation of Absolute Paleointensity Data for the Last 5 Ma 5) Boehnel and Molina-Garza, Paleosecular variation in Mexico during Tertiary and Quaternary 6) Stone and Layer, Paleosecular Variation of the Geomagnetic Field in Alaska: The Aleutians Islands and Wrangell Mountains Revisited 7) Geissman and Keating, Multiphase Modeling of Contact Metamorphic Systems and Application to a Miocene Transitional Geomagnetic Field Record, Paiute Ridge, Nevada 8) Herrero-Bervera et al., Geomagnetic Field Inclinations and Absolute Paleointensities for a 350 kyr Time gap From the 350 m Core of the Kalihi Scientific Drilling Project Recovered From the Ko'olau Volcano, O'ahu, Hawai'i. 9) Herrero-Bervera and Valet, Geomagnetic Directional and Absolute Paleointensity Variations Over 350 kyr From Lava Sequences Recorded in O'ahu, Hawai'i. 10) Wehland et al., Towards a Continuous Record of Earth Magnetic Field Reversals by Secondary Pyrrhotite ptrms 11) Tamrat et al., Strata Bound Reversal Stratigraphy in the Middle and Upper Semri Group of the Lower Vindhyanchal Basin (India): Preliminary Paleomagnetic Results 12) Schill and Lowrie, Polarity Record in the Klippen of Bhutans 13) Pares & Lanci, Paleogene and Neogene Magnetostratigraphy from ODP Leg 199 Sediments 14) H. Evans et al., Preliminary Magnetostratigraphic Results From ODP Leg 198- Shatsky Rise
5 15) Liddicoat, Negrini and Zic, Laschamp and Mono Lake Excursions in the same Lacustrine Record from Western North America 16) Liddicoat, Benson et al. Ages of the Mono Lake Excursion and Related Volcanic Tephra in the Great Basin of the Western United States 17) Liddicoat and Coe, Mono Lake Excursion in the Western and Southwestern United States 18) Kent and Schneider, Motions of Mantle Hotspots With Respect to the Spin Axis 19) Muttoni et al., Tethyan magnetostratigrapy from Pizzo Mondello and correlation to the Late Triassic Newark APTS 20) Channell et al., Carnian - Norian biomagnetostratigraphy at Silická Brezová (Slovakia): correlation to other Tethyan sections and to the Newark Basin 21) Channell, Comparison of U-channel and Discrete Sample Data Recording Polarity Reversals and Excursions: Examples From the North Atlantic 22) Singer and Hoffman, An 40Ar/39Ar Based Geomagnetic Instability Timescale (GITS) for the Brunhes and Matuyama Chrons 23) Biggin and Thomas Long term variations in geomagnetic intensity: Links to mantle and crustal processes 24) Selkin et al., How Variable Was the Late Archaean Field?: Paleointensity and Paleomagnetism of the Stillwater Complex, MT 25) Mozzoni and Cain, What is the core trying to tell us?
Brunhes Geomagnetic and Rock Magnetic Variations Recorded in Eight Holes Cored at ODP Site 1062 on the Bahama Outer Ridge
Brunhes Geomagnetic and Rock Magnetic Variations Recorded in Eight Holes Cored at ODP Site 1062 on the Bahama Outer Ridge Gary D. Acton Ocean Drilling Program, Texas A&M University, 1000 Discovery Drive,
More informationThe Lithosphere and the Tectonic System. The Structure of the Earth. Temperature 3000º ºC. Mantle
The Lithosphere and the Tectonic System Objectives: Understand the structure of the planet Earth Review the geologic timescale as a point of reference for the history of the Earth Examine the major relief
More informationGeomagnetic Reversals: Rates, Timescales, Preferred Paths, Statistical Models and Simulations
Geomagnetic Reversals: Rates, Timescales, Preferred Paths, Statistical Models and Simulations Catherine Constable Institute of Geophysics and Planetary Physics Scripps Institution of Oceanography University
More informationReview participation point: The evidence for a fluid outer core is:
DDA1 Continental Drift to Plate Tectonics PS 100 Chapter 28 Review participation point: The evidence for a fluid outer core is: A. Average density of the earth is greater than the density of the crust.
More informationGEOMAGNETIC TEMPORAL SPECTRUM
Geomagnetic Temporal Spectrum Catherine Constable 1 GEOMAGNETIC TEMPORAL SPECTRUM Catherine Constable Institute of Geophysics and Planetary Physics Scripps Institution of Oceanography University of California
More informationThere are numerous seams on the surface of the Earth
Plate Tectonics and Continental Drift There are numerous seams on the surface of the Earth Questions and Topics 1. What are the theories of Plate Tectonics and Continental Drift? 2. What is the evidence
More informationThe Magnetic Field of the Earth
The Magnetic Field of the Earth Paleomagnetism, the Core, and the Deep Mantle RONALD T. MERRILL Department of Geophysics University of Washington Seattle, Washington MICHAEL W. McELHINNY Gondwana Consultants
More informationG 3. AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society
Geosystems G 3 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Article Volume 4, Number 6 14 June 2003 1049, doi:10.1029/2002gc000489 ISSN: 1525-2027 Source of
More informationOcean Crustal Magnetization and Magnetic Anomalies
Ocean Crustal Magnetization and Magnetic Anomalies Anomaly and magnetization basics Lavas as largest magnetic source what controls their magnetization? Do lower crustal layers contribute? Magnetic anomalies
More informationG 3. Paleosecular variation and the average geomagnetic field at ±20 latitude
Geosystems G 3 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Article Volume 7, Number 7 20 July 2006 Q07007, doi:10.1029/2005gc001181 ISSN: 1525-2027 Click Here
More informationGeomagnetic excursions: Knowns and unknowns
Click Here for Full Article GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L17307, doi:10.1029/2008gl034719, 2008 Geomagnetic excursions: Knowns and unknowns Andrew P. Roberts 1 Received 17 May 2008; revised 11
More informationOn the Spatial Averaging of Paleomagnetic Data
Geophysica (2014), 50(1), 49 58 On the Spatial Averaging of Paleomagnetic Data Toni Veikkolainen 1*, Kimmo Korhonen 2 and Lauri J. Pesonen 1 1 Division of Materials Physics, Dept. of Physics, University
More information3. The diagram below shows how scientists think some of Earth's continents were joined together in the geologic past.
1. The map below shows the present-day locations of South America and Africa. Remains of Mesosaurus, an extinct freshwater reptile, have been found in similarly aged bedrock formed from lake sediments
More informationEvidence for a Geodynamo Driven by Thermal Energy in the Outermost Core and by Precession Deeper in the Outer Core
Research Article: Open Access Fuller. Int J Earth Sci Geophys 2017, 3:012 Evidence for a Geodynamo Driven by Thermal Energy in the Outermost Core and by Precession Deeper in the Outer Core Michael D Fuller*
More information5.11 Time-Averaged Field and Paleosecular Variation
5.11 Time-Averaged Field and Paleosecular Variation C. L. Johnson, University of British Columbia, Vancouver, BC, Canada P. McFadden, Geoscience Australia, Canberra, ACT, Australia ª 27 Elsevier B.V. All
More informationLecture #13 notes, Geology 3950 Spring 2006: CR Stern Magnetic reversals (text pages th edition and in the 5 th edition)
Lecture #13 notes, Geology 3950 Spring 2006: CR Stern Magnetic reversals (text pages 35-37 4 th edition and 53-55 in the 5 th edition) The earth has a magnetic field generated by circulation of charged
More informationQuestions and Topics
Plate Tectonics and Continental Drift Questions and Topics 1. What are the theories of Plate Tectonics and Continental Drift? 2. What is the evidence that Continents move? 3. What are the forces that
More informationDrifting Continents and Spreading Seas. The Road To Plate Tectonics
Drifting Continents and Spreading Seas The Road To Plate Tectonics Alfred Wegener and the Continental Drift hypothesis: Up until the early 1900s, long-held tradition in the earth sciences stated that continents
More informationA Brunhes-Matuyama polarity transition record from anoxic sediments in the South Atlantic (Ocean Drilling Program Hole 1082C)
Earth Planets pace, 53, 817 827, 2001 A Brunhes-Matuyama polarity transition record from anoxic sediments in the outh Atlantic (Ocean Drilling Program Hole 1082C) Toshitsugu Yamazaki and Hirokuni Oda Geological
More informationThe Geodynamo and Paleomagnetism Brown and Mussett (1993) ch. 6; Fowler p
In this lecture: The Core The Geodynamo and Paleomagnetism Brown and Mussett (1993) ch. 6; Fowler p. 32-50 Problems Outer core Physical state Composition Inner core Physical state Composition Paleomagnetism
More informationThe Magnetic Field of the Earth. Paleomagnetism, the Core, and the Deep Mantle
The Magnetic Field of the Earth Paleomagnetism, the Core, and the Deep Mantle This is Volume 63 in the INTERNATIONAL GEOPHYSICS SERIES A series of monographs and textbooks Edited by RENATA DMOWSKA and
More informationShallow bias in Neogene palaeomagnetic directions from the Guide Basin, NE Tibet, caused by inclination error
Geophys. J. Int. (2005) 163, 944 948 doi: 10.1111/j.1365-246X.2005.02802.x GJI Geomagnetism, rock magnetism and palaeomagnetism Shallow bias in Neogene palaeomagnetic directions from the Guide Basin, NE
More informationGeomagnetic paleosecular variation for the past 5 Ma in the Society Islands, French Polynesia
LETTER Earth Planets Space, 54, 797 802, 2002 Geomagnetic paleosecular variation for the past 5 Ma in the Society Islands, French Polynesia Y. Yamamoto 1, K. Shimura 1, H. Tsunakawa 1, T. Kogiso 2,K.Uto
More informationGlobal Tectonics. Kearey, Philip. Table of Contents ISBN-13: Historical perspective. 2. The interior of the Earth.
Global Tectonics Kearey, Philip ISBN-13: 9781405107778 Table of Contents Preface. Acknowledgments. 1. Historical perspective. 1.1 Continental drift. 1.2 Sea floor spreading and the birth of plate tectonics.
More information10. Paleomagnetism and Polar Wandering Curves.
Map of ocean floor Evidence in Support of the Theory of Plate Tectonics 10. Paleomagnetism and Polar Wandering Curves. The Earth's magnetic field behaves as if there were a bar magnet in the center of
More information10. BRUNHES CHRON MAGNETIC FIELD EXCURSIONS RECOVERED FROM LEG 172 SEDIMENTS 1
Keigwin, L.D., Rio, D., Acton, G.D., and Arnold, E. (Eds.) Proceedings of the Ocean Drilling Program, Scientific Results Volume 172 1. BRUNHES CHRON MAGNETIC FIELD EXCURSIONS RECOVERED FROM LEG 172 SEDIMENTS
More informationA paleomagnetic power spectrum
Physics of the Earth and Planetary Interiors 153 (2005) 61 73 A paleomagnetic power spectrum Catherine Constable, Catherine Johnson 1 Green Institute of Geophysics and Planetary Physics, Scripps Institution
More informationRegionally Recurrent Paleomagnetic Transitional Fields and Mantle Processes
Regionally Recurrent Paleomagnetic Transitional Fields and Mantle Processes Kenneth A. Hoffman Physics Department, Cal Poly State University, San Luis Obispo, California Brad S. Singer Department of Geology
More informationGeomagnetic field variations during the last 400 kyr in the western equatorial Pacific: Paleointensity-inclination correlation revisited
GEOPHYSICAL RESEARCH LETTERS, VOL. 35, L20307, doi:10.1029/2008gl035373, 2008 Geomagnetic field variations during the last 400 kyr in the western equatorial Pacific: Paleointensity-inclination correlation
More informationMorphology of the Iceland Basin Excursion from a. from a spherical harmonics analysis and an iterative Bayesian inversion procedure of sedimentary
Morphology of the Iceland Basin Excursion from a spherical harmonics analysis and an iterative Bayesian inversion procedure of sedimentary records Luca Lanci, Catherine Kissel, Roman Leonhardt, Carlo Laj
More informationDEEP-TOW STUDY OF MAGNETIC ANOMALIES IN THE PACIFIC JURASSIC QUIET ZONE. A Thesis MASAKO TOMINAGA
DEEP-TOW STUDY OF MAGNETIC ANOMALIES IN THE PACIFIC JURASSIC QUIET ZONE A Thesis by MASAKO TOMINAGA Submitted to the Office of Graduate Studies of Texas A&M University in partial fulfillment of the requirements
More informationChapter 2 Plate Tectonics and the Ocean Floor
Chapter 2 Plate Tectonics and the Ocean Floor Matching. Match the term or person with the appropriate phrase. You may use each answer once, more than once or not at all. 1. hydrothermal vents A. convergent
More informationGO ON. Directions: Use the diagram below to answer question 1.
d i a g n o s t i c t e s t : e a r t h a n d s p a c e s c i e n c e question 1. 1. What is the correct order (starting from the surface) of Earth s layers? A crust, outer core, inner core, mantle B mantle,
More information02- Die Plattentektonik
02- Die Plattentektonik Geological evidences for continental drift G r e enlan d Baltic shield Russian platform The fit of the continents around the North Atlantic, after Bullard et al. (1965), and the
More informationIntroduction to Oceanography. Chapter 2: Plate Tectonics Overview
Introduction to Oceanography Chapter 2: Plate Tectonics Overview Much evidence supports plate tectonics theory. The plate tectonics model describes features and processes on Earth. Plate tectonic science
More informationGeology of the Hawaiian Islands
Geology of the Hawaiian Islands Class 3 20 January 2004 Any Questions? IMPORTANT Big Island Field Trip We need a firm commitment PLUS $164 payment for airfare BEFORE January 29th Plate Tectonics Fundamental
More informationOCN 201 Seafloor Spreading and Plate Tectonics. Question
OCN 201 Seafloor Spreading and Plate Tectonics Question What was wrong from Wegener s theory of continental drift? A. The continents were once all connected in a single supercontinent B. The continents
More informationPhysics of the Earth and Planetary Interiors
Physics of the Earth and Planetary Interiors 170 (2008) 34 45 Contents lists available at ScienceDirect Physics of the Earth and Planetary Interiors journal homepage: www.elsevier.com/locate/pepi Testing
More informationSuperchrons provide an opportunity to view the geomagnetic
The Cretaceous superchron geodynamo: Observations near the tangent cylinder John A. Tarduno*, Rory D. Cottrell, and Alexei V. Smirnov Department of Earth and Environmental Sciences, University of Rochester,
More informationBiology. Slide 1 of 40. End Show. Copyright Pearson Prentice Hall
Biology 1 of 40 2 of 40 Fossils and Ancient Life What is the fossil record? 3 of 40 Fossils and Ancient Life The fossil record provides evidence about the history of life on Earth. It also shows how different
More informationBefore Plate Tectonics: Theory of Continental Drift
Before Plate Tectonics: Theory of Continental Drift Predecessor to modern plate tectonics Shape and fit of the continents was the initial evidence Snider-Pelligrini (1858) Taylor (1908) Wegner (1915) Fig.
More informationPaleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil)
GEOFÍSICA INTERNACIONAL (2015) 54-2: 167-178 ORIGINAL PAPER Paleomagnetic Pole Positions and Geomagnetic Secular Variation from the Cretaceous Ponta Grossa Dike Swarm (Brazil) * Urrutia-Fucugauchi Resumen
More informationDOWNLOAD PDF MAGNETIC STRATIGRAPHY
Chapter 1 : Stratigraphy - Wikipedia The magnetic property most useful in stratigraphic work is the change in the direction of the remanent magnetization of the rocks, caused by reversals in the polarity
More informationContinental drift
Plate Tectonics Continental drift Continental drift Continental drift Continental drift Continental drift Plate Tectonics Plate Tectonics Continental Drift and Paleomagnetism Paleomagnetism Renewed interest
More informationA 2.14-Myr astronomically tuned record of relative geomagnetic paleointensity from the western Philippine Sea
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 108, NO. B1, 2059, doi:10.1029/2001jb001698, 2003 A 2.14-Myr astronomically tuned record of relative geomagnetic paleointensity from the western Philippine Sea Chorng-Shern
More informationLecture 15: The ancient geomagnetic field. Why study the ancient field. Paleosecular variation: the Holocene. past 5 Myr. Excursions and reversals
Lecture 15: The ancient geomagnetic field Why study the ancient field Paleosecular variation: the Holocene past 5 Myr Excursions and reversals 1 Why study the ancient geomagnetic field The geomagnetic
More informationFull file at CHAPTER 2 The Way the Earth Works: Plate Tectonics
CHAPTER 2 The Way the Earth Works: Plate Tectonics MULTIPLE CHOICE 1. Wegener proposed continental drift after he observed evidence from fossils, glacial deposits, and the fit of the continents that suggested
More information11. PALEOMAGNETIC RECORDS OF STAGE 3 EXCURSIONS, LEG 172 1
Keigwin, L.D., Rio, D., Acton, G.D., and Arnold, E. (Eds.) Proceedings of the Ocean Drilling Program, Scientific Results Volume 172 11. PALEOMAGNETIC RECORDS OF STAGE 3 EXCURSIONS, LEG 172 1 Steve P. Lund,
More informationGeomagnetism. The Earth s Magnetic field. Magnetization of rocks. The Earth s magnetic record. Proof of continental drift.
Geomagnetism The Earth s Magnetic field. The Earth s magnetic record Magnetization of rocks C Gary A. Glatzmaier University of California, Santa Cruz Proof of continental drift Magnetism Magnetic Force
More informationThe High Lava Plains Project: Understanding the Causes of Continental Intraplate Tectonomagmatism
The High Lava Plains Project: Understanding the Causes of Continental Intraplate Tectonomagmatism The High Lava Plains (HLP) of the northwestern USA is one of the most accessible yet least understood examples
More informationPacific Secular Variation A result of hot lower mantle. David Gubbins School of Earth Sciences University of Leeds
Pacific Secular Variation A result of hot lower mantle David Gubbins School of Earth Sciences University of Leeds Thermal Core-Mantle Interaction (hot) (cold) Lateral variations in heat flux boundary condition
More informationPaleointensity variations of Earth s magnetic field and their relationship with polarity reversals
Ž. Physics of the Earth and Planetary Interiors 110 1999 115 128 Paleointensity variations of Earth s magnetic field and their relationship with polarity reversals Jon D. Pelletier DiÕision of Geological
More informationChapter 2 The Way The Earth Works: Plate Tectonics
Chapter 2 The Way The Earth Works: Plate Tectonics In this Chapter! What were Wegener s observations?! Paleomagnetism: the key proof of continental drift! Observations that led Harry Hess to sea-floor
More informationWhat Forces Drive Plate Tectonics?
What Forces Drive Plate Tectonics? The tectonic plates are moving, but with varying rates and directions. What hypotheses have been proposed to explain the plate motion? Convection Cells in the Mantle
More informationThe principle of fossil succession allows strata in different parts of the world to be correlated, and worldwide relative ages to be worked out
Correlating beds using index fossils Stratigraphic Classification: Piles of stratified rocks need to be classified. A formation is an easily identifiable rock unit that differs from layers above and below
More informationGeology of the Batemans Bay region. Geological evolution. The Lachlan Orogen
Australian Journal of Earth Sciences 1 The word orogen is derived from the ancient Greek language word for mountain building. The Lachlan Orogen The rocks exposed in the Batemans Bay are part of the geological
More informationAnnouncements & Questions? Textbook Options
Announcements & Questions? Course syllabus and lecture notes have been posted http://www.soest.hawaii.edu/gg/faculty/popp/ GG101.html Questions about the textbook and access to mygeoscienceplace.com should
More informationCOMPOSITION and PHYSICAL PROPERTIES GENERAL SUBJECTS. GEODESY and GRAVITY
COMPOSITION and PHYSICAL PROPERTIES Composition and structure of the continental crust Composition and structure of the core Composition and structure of the mantle Composition and structure of the oceanic
More informationCivilization exists by geologic consent, subject to change without notice William Durant
89.325 Geology for Engineers Plate Tectonics Civilization exists by geologic consent, subject to change without notice William Durant Properties of the Planets Size Density Distance from sun Chemistry
More informationAnnouncements. Manganese nodule distribution
Announcements Lithospheric plates not as brittle as previously thought ESCI 322 Meet in Env. Studies Bldg Rm 60 at 1 PM on Tuesday One week (Thursday): Quiz on Booth 1994 and discussion. (Lots of odd terms
More informationFull file at
Essentials of Oceanography, 10e (Trujillo/Keller) Chapter 2 Plate Tectonics and the Ocean Floor Match the term with the appropriate phrase. You may use each answer once, more than once or not at all. A)
More informationWith a group, get a bar magnet, some plastic wrap, iron filings and a compass.
Name: EPS 50 Lab 8: The Earth's Magnetic Field Chapter 2, p. 39-41: The Seafloor as a Magnetic Tape Recorder Chapter 7, p. 213: Paleomagnetic Stratigraphy Chapter 14, p. 396-406: Earth s Magnetic Field
More informationGY 112: Earth History
UNIVERSITY OF SOUTH ALABAMA GY 112: Earth History Lectures 31: Mesozoic Tectonics Instructor: Dr. Douglas W. Haywick Last Time Mesozoic Overview A) The end of the Paleozoic B) Mesozoic time frame and evolutionary
More informationA reversal of the Earth s magnetic field recorded in mid-miocene lava flows of Gran Canaria: Paleointensities
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 107, NO. B11, 2299, doi:10.1029/2001jb000949, 2002 A reversal of the Earth s magnetic field recorded in mid-miocene lava flows of Gran Canaria: Paleointensities R.
More informationTIME VARIATIONS IN GEOMAGNETIC INTENSITY
TIME VARIATIONS IN GEOMAGNETIC INTENSITY Jean-Pierre Valet Institut de Physique du Globe de Paris, Paris, France Received 15 May 2001; revised 8 October 2001; accepted 8 October 2002; published 19 April
More informationPlate Tectonics. 1)The plate tectonic system 2)A theory is born 3) Early evidence for continental drift 4) Continental drift and paleomagnetism
Plate Tectonics Plate boundaries 1)The plate tectonic system 2)A theory is born 3) Early evidence for continental drift 4) Continental drift and paleomagnetism 6)History and future of plate motions system
More informationEarth s Structure and Surface
Earth s Structure and Surface Structure of the Earth The earth is thought have originated about 4.5 billion years ago from a cloud or clouds of dust. The dust was the remains of a huge cosmic explosion
More informationPhanerozoic (last 0.54 by) Tectonics Climate Life
Phanerozoic (last 0.54 by) Tectonics Climate Life Tools for Locating Past Continent Positions Fossils depending on climate Alignment of geological features Geometrical fit of continental margins Similarity
More informationMesozoic rock formations in the NY region. The Geologic History of New York State. The Mesozoic. Mesozoic Rock Formations in the NY Region
The eologic History of New York State The Mesozoic eologic Provinces NY Region Timescale and geologic provinces of NY-NJ Mesozoic Rock Formations in the NY Region Mesozoic rock formations in the NY region
More informationLimitations in correlation of regional relative geomagnetic paleointensity
Limitations in correlation of regional relative geomagnetic paleointensity D.G. McMillan and C.G. Constable 2. School of Mathematics and Statistics, University of Newcastle upon Tyne, Newcastle upon Tyne
More informationEarth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building
Earth Science, (Tarbuck/Lutgens) Chapter 10: Mountain Building 1) A(n) fault has little or no vertical movements of the two blocks. A) stick slip B) oblique slip C) strike slip D) dip slip 2) In a(n) fault,
More informationG 3. AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society
Geosystems G 3 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Article Volume 7, Number 3 8 March 2006 Q03004, doi:10.1029/2005gc001122 ISSN: 1525-2027 Geomagnetic
More informationAvailable online at
Available online at www.sciencedirect.com Earth and Planetary Science Letters 268 (2008) 245 254 www.elsevier.com/locate/epsl Testing the relationship between timing of geomagnetic reversals/excursions
More informationPlate Tectonics A Geologic Revolution
Plate Tectonics A Geologic Revolution Earth s Structure Iron-nickel core Silicate Mantle Mohorovicic Discontinuity Asthenosphere Lithosphere Continental Drift the Great Debate Date Topic or Event Scientist
More informationANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017
ANOTHER MEXICAN EARTHQUAKE! Magnitude 7.1, Tuesday Sept. 19, 2017 Why is there no oceanic crust older than 200 million years? SUBDUCTION If new oceanic crust is being continuously created along the earth
More information12/3/2014. Plate Tectonics: A Scientific Revolution Unfolds Earth Science, 13e Chapter 7. Continental drift: an idea before its time
Plate Tectonics: A Scientific Revolution Unfolds Earth Science, 13e Chapter 7 Stanley C. Hatfield Southwestern Illinois College Continental drift: an idea before its time Alfred Wegener First proposed
More information17. THE MAGNETOSTRATIGRAPHY OF NORTHWEST PACIFIC SEDIMENTS, DEEP SEA DRILLING PROJECT LEG 86 1
17. THE MAGNETOSTRATIGRAPHY OF NORTHWEST PACIFIC SEDIMENTS, DEEP SEA DRILLING PROJECT LEG 86 1 Ulrich Bleil, Institut für Geophysik, Ruhr-Universitàt Bochum 2 ABSTRACT Results of paleomagnetic analyses
More informationThe role of the Earth s mantle in controlling the frequency of geomagnetic reversals
The role of the Earth s mantle in controlling the frequency of geomagnetic reversals Gary A. Glatzmaier*, Robert. Coe*, Lionel Hongre* & Paul H. Roberts * Earth ciences Department, University of California,
More informationPHYSICAL GEOLOGY AND THE ENVIRONMENT (2 ND CANADIAN EDITION)
Chapter 2: Plate Tectonics Chapter Summary: Plate tectonics is a theory that suggests Earth's surface is divided into several large plates that change position and size. Intense geologic activity occurs
More informationPlate Tectonics: A Scientific Revolution Unfolds
Chapter 2 Lecture Earth: An Introduction to Physical Geology Eleventh Edition Plate Tectonics: A Scientific Revolution Unfolds Tarbuck and Lutgens From Continental Drift to Plate Tectonics Prior to the
More information38. RELATIVE GEOMAGNETIC INTENSITY DURING THE LAST 4 M.Y. FROM THE EQUATORIAL PACIFIC 1
Pisias, N.G., Mayer, L.A., Janecek, T.R., Palmer-Julson, A., and van Andel, T.H. (Eds.), 1995 Proceedings of the Ocean Drilling Program, Scientific Results, Vol. 138 38. RELATIVE GEOMAGNETIC INTENSITY
More informationGY 111: Physical Geology
UNIVERSITY OF SOUTH ALABAMA GY 111: Physical Geology Lecture 21: Rock Deformation Instructor: Dr. Douglas W. Haywick Last Time A) How long is long? B) Geological time divisions Web notes 20 Geological
More informationAstronomical ages for Miocene polarity chrons C4Ar C5r ( Ma), and for three excursion chrons within C5n.2n
Earth and Planetary Science Letters 256 (2007) 455 465 www.elsevier.com/locate/epsl Astronomical ages for Miocene polarity chrons C4Ar C5r (9.3 11.2 Ma), and for three excursion chrons within C5n.2n Helen
More informationESSENTIALS OF PALEOMAGNETISM
ESSENTIALS OF PALEOMAGNETISM LISA TAUXE With Contributions from Robert F. Butler, R. Van der Voo, and Subir K. Banerjee CONTENTS PREFACE xiii 1 THE PHYSICS OF MAGNETISM 1 1.1 What is a magnetic field?
More informationPSc 201 Chapter 3 Homework. Critical Thinking Questions
PSc 201 Chapter 3 Homework Critical Thinking Questions 1. (adapted from text) Seawater is denser than fresh water. A ship moving from the Atlantic Ocean into the Great Lakes goes from seawater to fresh
More informationMesozoic Earth History
Mesozoic Earth History The Mesozoic Era 251-66 MYA Breakup of Pangea Changes in air and oceanic currents Evolution of new terrestrial and marine life Opening of the Atlantic Ocean Basin Rocky Mountains
More informationTrue polar wander since 32 Ma B.P.: A paleomagnetic investigation of the skewness of magnetic anomaly 12r on the Pacific plate
JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 115,, doi:10.1029/2009jb006862, 2010 True polar wander since 32 Ma B.P.: A paleomagnetic investigation of the skewness of magnetic anomaly 12r on the Pacific plate
More informationMono Basin climate changes correlative with North Atlantic Dansgaard-Oeschger oscillations
Mono Basin climate changes correlative with North Atlantic Dansgaard-Oeschger oscillations Susan Zimmerman Lawrence Livermore Nat l. Lab. Corinne Hartin RSMAS- U Miami Crystal Pearl Queens College,CUNY
More informationWhy does the Earth have volcanoes? Why is there Earthquakes?
Why does the Earth have volcanoes? Why is there Earthquakes? Turn to your neighbor and review: How and when did the Earth form? How old are the first traces of life on Earth? Logical? * 1.5Ga (1 st multicellular
More informationG 3. AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society
Geosystems G 3 AN ELECTRONIC JOURNAL OF THE EARTH SCIENCES Published by AGU and the Geochemical Society Article Volume 9, Number 4 23 April 2008 Q04032, doi:10.1029/2007gc001696 ISSN: 1525-2027 Click Here
More informationPLATE TECTONICS. Continental Drift. Continental Drift. Continental Drift. Continental Drift- Wegener s Evidence
Continental Drift PLATE TECTONICS E.B. Taylor (1910) and Alfred Wegener (1915) published on Continental Drift. Continental Drift Wegener s evidence 1. Fit of the Continents 2. Fossil Evidence 3. Rock Type
More informationRedefinition of the Blake Event
Redefinition of the Blake Event Steve P. Lund 1, Martha Schwartz 1, and Lloyd Keigwin 2 1) University of Southern California, Los Angeles, CA 2) Wood Hole Oceanographic Institution, Woods Hole, MA Abstract
More informationChapter 3 Time and Geology
Chapter 3 Time and Geology Methods of Dating Rocks 1. Relative dating - Using fundamental principles of geology (Steno's Laws, Fossil Succession, etc.) to determine the relative ages of rocks (which rocks
More informationOcean Basins, Bathymetry and Sea Levels
Ocean Basins, Bathymetry and Sea Levels Chapter 4 Please read chapter 5: sediments for next class and start chapter 6 on seawater for Thursday Basic concepts in Chapter 4 Bathymetry the measurement of
More informationLecture 10: Plate Tectonics I. 1. Midterm 1 scores returned 2. Homework #9 due Thursday 12pm
Lecture 10: Plate Tectonics I 1. Midterm 1 scores returned 2. Homework #9 due Thursday 12pm Learning Objectives (LO)! Lecture 10: Plate Tectonics I! ** Chapter 3 **! What we ll learn today:" 1. Describe
More informationChapter 20. Plate Tectonics
Chapter 20 Plate Tectonics Early Evidence (Wegener) The geometric fit of the continents. The similarity in rock age groups between adjoining regions. The similarity in Paleozoic fossils between adjoining
More informationQuestions for Discussion. Plate Tectonics II: The Ocean Floor and the Seafloor Spreading Hypothesis
Plate Tectonics II: The Ocean Floor and the Seafloor Spreading Hypothesis Arthur Holmes British Geologist (1890-1965) Used radiometric dating to determine an accurate age for the Earth and to create a
More informationShipboard Laboratories INTEGRATED OCEAN DRILLING PROGRAM
Riserless Vessel Shipboard Laboratories INTEGRATED OCEAN DRILLING PROGRAM JOIDES Resolution Paleomagnetism Laboratory February, 2005 What is the Paleomagnetism Laboratory? The oceanic crust below marine
More informationPALAEOMAGNETISM. Results from palaeomagnetism Polar wander curves: continental drift and rotation.
PALAEOMAGNETISM OUTLINE Magnetism in rocks Induced and remanent magnetism: - dia, para, ferro, antiferro, and ferrimagnetics; domain theory, Curie temperature, blocking temperature. Natural remanent magnetism
More informationPrentice Hall EARTH SCIENCE
Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 9 Plate Tectonics 9.1 Continental Drift An Idea Before Its Time Wegener s continental drift hypothesis stated that the continents had once been joined
More information