Open AccessSeismic Imaging of Thickened Lithosphere Resulting From Plume Pulsing Beneath Iceland
Author(s) -
Rychert Catherine A.,
Harmon Nicholas,
Armitage John J.
Publication year - 2018
Publication title -
geochemistry, geophysics, geosystems
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.928
H-Index - 136
ISSN - 1525-2027
DOI - 10.1029/2018gc007501
Subject(s) - lithosphere , geology , plume , seafloor spreading , mantle plume , ridge , plate tectonics , mid ocean ridge , seismology , geophysics , delamination (geology) , convergent boundary , panache , ridge push , thermal , oceanic crust , mantle (geology) , tectonics , paleontology , subduction , meteorology , physics
Ocean plates conductively cool and subside with seafloor age. Plate thickening with age is also predicted, and hot spots may cause thinning. However, both are debated and depend on the way the plate is defined. Determining the thickness of the plates along with the process that governs it has proven challenging. We use S‐to‐P (Sp) receiver functions to image a strong, persistent LAB beneath Iceland where the mid‐Atlantic Ridge interacts with a plume with hypothesized pulsating thermal anomaly. The plate is thickest, up to 84 ± 6 km, beneath lithosphere formed during times of hypothesized hotter plume temperatures and as thin as 61 ± 6 km beneath regions formed during colder intervals. We performed geodynamic modeling to show that these plate thicknesses are inconsistent with a thermal lithosphere. Instead, periods of increased plume temperatures likely increased the melting depth, causing deeper depletion and dehydration, and creating a thicker plate. This suggests plate thickness is dictated by the conditions of plate formation.