The Influence of Post‐accretion Sedimentation on Marine Magnetic Anomalies

• Published in: Geophysical Research Letters
• Main Authors: Granot, R., Dyment, J.
• Other Authors: Institut de Physique du Globe de Paris (IPGP), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-Université de La Réunion (UR)-Institut de Physique du Globe de Paris (IPG Paris)-Centre National de la Recherche Scientifique (CNRS)
• Format: Article in Journal/Newspaper
• Language: English
• Published: HAL CCSD 2019
• Subjects: [SDU.STU.GP]Sciences of the Universe [physics]/Earth Sciences/Geophysics [physics.geo-ph]; [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography; South Atlantic Ocean
• Online Access: https://hal.science/hal-02390143; https://hal.science/hal-02390143/document; https://hal.science/hal-02390143/file/2019GL082265.pdf; https://doi.org/10.1029/2019GL082265

International audience Marine magnetic anomalies are a critical observation used to investigate seafloor spreading and the transition between oceanic and continental crust at passive margins. However, pronounced post-accretion sedimentation disturbs the thermal state of the crust and therefore alters its remanent magnetization. To study the link between sedimentation and magnetization of the oceanic crust, we built a series of thermomagnetic forward models coupled with different sedimentation histories. We test our approach against observations from the early Cretaceous southern South Atlantic Ocean. Our simulations suggest that, depending on the thickness of post-accretion sediments, the remanent magnetization of the extrusive basalts is partly or completely removed. Therefore, the typical long-wavelength sea surface marine magnetic anomalies observed above oceanic crust covered by a thick sedimentary pile is almost entirely generated by the magnetization of the deeper crustal layers. Plain Language Summary Marine magnetic anomalies are a critical observation used to investigate seafloor spreading and the transition between oceanic and continental crust at passive margins. Here we show that the accumulation of sediments over the oceanic crust has a thermal effect, which can lead, under certain conditions, to the complete removal of magnetization in the upper oceanic crust. This, in turn, may have important consequences for how we understand passive margins and the accuracy of plate kinematic models.