Constraints on the Origin of the Martian Dichotomy From Southern Highlands Marsquakes

Abstract The Martian hemispheric dichotomy is delineated by significant differences in elevation and crustal thickness between the Northern Lowlands and Southern Highlands. Yet, its origin remains controversial. Here, we improve the signal‐to‐noise ratios and determine the locations of the low‐frequ...

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Main Authors: Weijia Sun, Hrvoje Tkalčić
Format: Article
Language:English
Published: Wiley 2025-01-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2024GL110921
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author Weijia Sun
Hrvoje Tkalčić
author_facet Weijia Sun
Hrvoje Tkalčić
author_sort Weijia Sun
collection DOAJ
description Abstract The Martian hemispheric dichotomy is delineated by significant differences in elevation and crustal thickness between the Northern Lowlands and Southern Highlands. Yet, its origin remains controversial. Here, we improve the signal‐to‐noise ratios and determine the locations of the low‐frequency marsquakes recorded during the InSight mission. We find a new cluster of marsquakes in Terra Cimmeria, Southern Highlands, in addition to those previously located in Cerberus Fossae, Northern Lowlands. Using the spectral ratio method, we estimate the quality factor Q in the range 481–543 for Terra Cimmeria versus 800–2,000 determined for Cerberus Fossae. The attenuation difference might be linked to the temperature differences between the two hemispheres, along with more vigorous convection beneath the Southern Highlands. These seismological observations, together with geochronological constraints of giant impacts, reinforce the “endogenic” hypothesis that mantle convection causes the crustal dichotomy.
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spelling doaj-art-fb0b5bcc3ac8432ab8557f0e34b9143a2025-01-20T13:05:57ZengWileyGeophysical Research Letters0094-82761944-80072025-01-01521n/an/a10.1029/2024GL110921Constraints on the Origin of the Martian Dichotomy From Southern Highlands MarsquakesWeijia Sun0Hrvoje Tkalčić1Key Laboratory of Earth and Planetary Physics Institute of Geology and Geophysics Chinese Academy of Sciences Beijing ChinaResearch School of Earth Sciences The Australian National University Canberra ACT AustraliaAbstract The Martian hemispheric dichotomy is delineated by significant differences in elevation and crustal thickness between the Northern Lowlands and Southern Highlands. Yet, its origin remains controversial. Here, we improve the signal‐to‐noise ratios and determine the locations of the low‐frequency marsquakes recorded during the InSight mission. We find a new cluster of marsquakes in Terra Cimmeria, Southern Highlands, in addition to those previously located in Cerberus Fossae, Northern Lowlands. Using the spectral ratio method, we estimate the quality factor Q in the range 481–543 for Terra Cimmeria versus 800–2,000 determined for Cerberus Fossae. The attenuation difference might be linked to the temperature differences between the two hemispheres, along with more vigorous convection beneath the Southern Highlands. These seismological observations, together with geochronological constraints of giant impacts, reinforce the “endogenic” hypothesis that mantle convection causes the crustal dichotomy.https://doi.org/10.1029/2024GL110921marsdichotomymarsquakeattenuationmantle convectiontectonics
spellingShingle Weijia Sun
Hrvoje Tkalčić
Constraints on the Origin of the Martian Dichotomy From Southern Highlands Marsquakes
Geophysical Research Letters
mars
dichotomy
marsquake
attenuation
mantle convection
tectonics
title Constraints on the Origin of the Martian Dichotomy From Southern Highlands Marsquakes
title_full Constraints on the Origin of the Martian Dichotomy From Southern Highlands Marsquakes
title_fullStr Constraints on the Origin of the Martian Dichotomy From Southern Highlands Marsquakes
title_full_unstemmed Constraints on the Origin of the Martian Dichotomy From Southern Highlands Marsquakes
title_short Constraints on the Origin of the Martian Dichotomy From Southern Highlands Marsquakes
title_sort constraints on the origin of the martian dichotomy from southern highlands marsquakes
topic mars
dichotomy
marsquake
attenuation
mantle convection
tectonics
url https://doi.org/10.1029/2024GL110921
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AT hrvojetkalcic constraintsontheoriginofthemartiandichotomyfromsouthernhighlandsmarsquakes