Seismically constrained gravity inversions reveal magmatic and metamorphic processes at a major lithospheric boundary in northwestern Australia

Moro, Polyanna de Sousa; Aitken, Alan; Giraud, Jérémie; Jessell, Mark; Pour, Fariba Kohan

doi:10.1016/j.tecto.2023.230003

Cited by 3 publications

(1 citation statement)

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“…This study followed the alternating inversion method used by Aitken et al (2013), Alghamdi et al (2018), andMoro et al (2023). Each of our model runs ran three cycles of four single-iteration inversions, respectively one iteration for mantle density, then one iteration each for the density within the crust layers, the geometry of the Moho, and the sedimentary basin thickness.…”

Section: Gravity Inversionmentioning

confidence: 99%

Crustal Heterogeneity of Antarctica Signals Spatially Variable Radiogenic Heat Production

Li,

Aitken

2024

Geophysical Research Letters

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Geothermal heat flow (GHF) is a key basal boundary condition for Antarctic ice‐sheet flow. Large‐scale variations are resolved by several recent models but knowledge of the smaller‐scale variations, crucial for ice sheet dynamics, is limited by unresolved variations in crustal radiogenic heat production. To define this at continent‐scale we use 3D gravity inversion constrained by seismic Moho estimates to identify variations in crustal composition and geometry beneath thick ice. Geochemically‐defined empirical relationships between density and heat production capture the global average trend and its variability, and allow to estimate from upper‐crust density spatial variations in radiogenic heat production. Significant variations are observed typically 1.2–1.6 μW/m3, and as high as 2 μW/m3 in West Antarctica. The contribution to GHF from these heat‐production variations is similarly variable, typically 16–24 mW/m2 and up to 60 mW/m2. The mapped variations are significant for correctly representing GHF in Antarctica.

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Section: Gravity Inversionmentioning

confidence: 99%