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<p>The crust of Mars preserves a record of early planetary evolution in the absence of plate tectonics, offering crucial insights into the development of terrestrial planets. Seismic data from NASA’s InSight mission reveal a stratified crust with an intracrustal seismic discontinuity at ~24 km, overlying the crust–mantle boundary at ~38 km. The nature of this intracrustal discontinuity remains unresolved. Here, however, using phase equilibrium modelling integrated with petrophysics and Bayesian statistics, we show that it marks a transition from mafic to ultramafic lithologies and interpret the lowermost ultramafic layer as a ~14-km-thick melt-depleted cumulate zone overlying the petrologic crust–mantle boundary. Thermal modelling indicates that such a melt-depleted layer could not have formed under ambient temperature conditions; instead, it requires an elevated heat flow probably driven by mantle upwelling and magmatic intrusion, promoting magmatic differentiation and partial melting within the crust. Together with prior evidence for evolved melts and upper-crustal differentiation, our results indicate that Mars once hosted vertically integrated transcrustal magmatic systems akin to those common on Earth. This demonstrates that these systems and their attendant geochemical differentiation can form without plate tectonics, offering a universal mechanism for building secondary and tertiary crust on hot rocky planets.</p>

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Seismic evidence for a melt-depleted lower crust and transcrustal magmatism on Mars

  • 期刊论文

  • 出版模式：

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  • 发表日期：

    2026年6月26日

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  • T. Mackay-Champion,
  • M. Anderson Loake,
  • R. Palin,
  • J. Wade,
  • J.-M. Kendall

摘要

The crust of Mars preserves a record of early planetary evolution in the absence of plate tectonics, offering crucial insights into the development of terrestrial planets. Seismic data from NASA’s InSight mission reveal a stratified crust with an intracrustal seismic discontinuity at ~24 km, overlying the crust–mantle boundary at ~38 km. The nature of this intracrustal discontinuity remains unresolved. Here, however, using phase equilibrium modelling integrated with petrophysics and Bayesian statistics, we show that it marks a transition from mafic to ultramafic lithologies and interpret the lowermost ultramafic layer as a ~14-km-thick melt-depleted cumulate zone overlying the petrologic crust–mantle boundary. Thermal modelling indicates that such a melt-depleted layer could not have formed under ambient temperature conditions; instead, it requires an elevated heat flow probably driven by mantle upwelling and magmatic intrusion, promoting magmatic differentiation and partial melting within the crust. Together with prior evidence for evolved melts and upper-crustal differentiation, our results indicate that Mars once hosted vertically integrated transcrustal magmatic systems akin to those common on Earth. This demonstrates that these systems and their attendant geochemical differentiation can form without plate tectonics, offering a universal mechanism for building secondary and tertiary crust on hot rocky planets.