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Member Since 1968
Rob S. Coe
AGU Research
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Accurate RESET Corrected Paleointensities from Non-Single-Domain Mt. Lassen 1915 Dacite
PALEOINTENSITY: INSTRUMENTS, EXPERIMENTS, RESULTS, SIMULATIONS, AND THE HISTORY OF THE GEOMAGNETIC FIELD II POSTER
geomagnetism, paleomagnetism and electromagnetism | 16 december 2021
Xiaowei Chen, Huapei Wang, Robert S. Coe, Dennis V...
Accurate records of paleointensities are the key to understanding Earth and planetary dynamo processes. The Thellier-series paleointensity experiments...
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Switching field angular dependence and the measurement of anhysteretic remanence magnetization (ARM)
FUNDAMENTAL MINERAL AND ROCK MAGNETISM I
geomagnetism, paleomagnetism and electromagnetism | 14 december 2020
David R. Finn, Robert S. Coe
We describe a procedure for measuring ARM coercivity spectrum with a three-axis static alternating field demagnetization (AFD). The approach is unique...
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Defining the Limits of Greater India
GEOPHYSICAL RESEARCH LETTERS
17 april 2019
Jun Meng, Stuart A. Gilder, Chengshan Wang, Robert...

Greater India comprises a part of the Indian plate that subducted under Asia to help form the Tibetan Plateau. Defining the size of the Greater Ind...

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Synchronizing volcanic, sedimentary, and ice core records of Earth’s last magnetic polarity reversal
FALL MEETING 2018
13 december 2018
Brad S. Singer, Robert S. Coe, Brian R. Jicha, Nob...
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What We Know and Don't Know about Reversals
FALL MEETING 2018
12 december 2018
Robert S. Coe
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Millennial-Scale Instability in the Geomagnetic Field Prior to the Matuyama-Brunhes Reversal
GEOCHEMISTRY, GEOPHYSICS, GEOSYSTEMS
30 march 2018
Andrea Balbas, Anthony A. Koppers, Peter Clark, Ro...

Changes in the Earth's magnetic field have global significance that reach from the outer core extending out to the uppermost atmosphere. Paleomagne...

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Reduced convergence within the Tibetan Plateau by 26 Ma?
GEOPHYSICAL RESEARCH LETTERS
03 july 2017
Jun Meng, Robert S. Coe, Chengshan Wang, Stuart A....

Understanding the dynamics of double‐thickening and uplifting of the Tibetan crust requires constraints on the magnitude and timing of crusta...

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Measurement and Discrepancies of Tsunami Flow Directions Using Anisotropy of Magnetic Susceptibility (AMS) and Dip Orientations of Heavy Mineral Layers in Tsunami Deposits
FALL MEETING 2016
15 december 2016
Shusaku Kon, Robert S. Coe, David R. Finn, Guy R. ...
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