Variability of Sea‐Surface Magnetic Anomalies at Ultraslow Spreading Centers: Consequence of Detachment Faulting and Contrasted Magmatism?
Author:
Affiliation:
1. Université de Paris, Institut de physique du globe de Paris, CNRS Paris France
Funder
Chinese Government Scholarship
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021GL097276
Reference39 articles.
1. Magnetic polarity structure of the lower oceanic crust
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3. MAGNETIC ANOMALIES DUE TO PRISM‐SHAPED BODIES WITH ARBITRARY POLARIZATION
4. Magnetic signature of large exhumed mantle domains of the Southwest Indian Ridge – results from a deep-tow geophysical survey over 0 to 11 Ma old seafloor
5. Modes of faulting at mid-ocean ridges
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1. Geophysical investigation of the Mado Megamullion oceanic core complex: implications for the end of back-arc spreading;Progress in Earth and Planetary Science;2023-07-14
2. Temporal and spatial variation of seafloor spreading at ultraslow spreading ridges: Contribution of marine magnetics;Earth and Planetary Science Letters;2023-01
3. Magnetic Anomalies Caused by 3D Polyhedral Structures With Arbitrary Polynomial Magnetization;Geophysical Research Letters;2022-09-21
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