Exploration of high mass subsurface structures in the northern hemisphere with joint flexure and mantle convection modelling of the Martian gravity field

B.C. Root; R. Alkahal; W. Qin; Cedric  Thieulot

doi:10.5194/epsc2024-730

Exploration of high mass subsurface structures in the northern hemisphere with joint flexure and mantle convection modelling of the Martian gravity field

B.C. Root, R. Alkahal, W. Qin, Cedric Thieulot

Research output: Chapter in Book/Conference proceedings/Edited volume › Conference contribution › Scientific › peer-review

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Abstract

NASA’s InSight mission has brought new information about the Martian lithosphere (Banerdt et al. 2020), which warrants a re-analysis of the support of the crustal and sub-crustal masses. Furthermore, the discovery of a possible mantle plume underneath the region south of Elysium Mons (Broquet et al. 2023), gives evidence for recent magmatic activity underneath the crust of Mars causing dynamic support to volcanic structures.

Original language	English
Title of host publication	EPSC Abstracts
Subtitle of host publication	Europlanet Science Congress 2024
Number of pages	3
Volume	17
DOIs	https://doi.org/10.5194/epsc2024-730
Publication status	Published - 2024
Event	Europlanet Science Congress 2024 - Berlin, Germany Duration: 8 Sept 2024 → 13 Sept 2024

Conference

Conference	Europlanet Science Congress 2024
Abbreviated title	EPSC 2024
Country/Territory	Germany
City	Berlin
Period	8/09/24 → 13/09/24

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10.5194/epsc2024-730

EPSC2024-730-printFinal published version, 1.4 MBLicence: CC BY

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title = "Exploration of high mass subsurface structures in the northern hemisphere with joint flexure and mantle convection modelling of the Martian gravity field",

abstract = "NASA{\textquoteright}s InSight mission has brought new information about the Martian lithosphere (Banerdt et al. 2020), which warrants a re-analysis of the support of the crustal and sub-crustal masses. Furthermore, the discovery of a possible mantle plume underneath the region south of Elysium Mons (Broquet et al. 2023), gives evidence for recent magmatic activity underneath the crust of Mars causing dynamic support to volcanic structures.",

author = "B.C. Root and R. Alkahal and W. Qin and Cedric Thieulot",

year = "2024",

doi = "10.5194/epsc2024-730",

language = "English",

volume = "17",

booktitle = "EPSC Abstracts",

note = "Europlanet Science Congress 2024, EPSC 2024 ; Conference date: 08-09-2024 Through 13-09-2024",

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Root, BC , Alkahal, R , Qin, W & Thieulot, C 2024, Exploration of high mass subsurface structures in the northern hemisphere with joint flexure and mantle convection modelling of the Martian gravity field. in EPSC Abstracts: Europlanet Science Congress 2024. vol. 17, EPSC 2024-730, Europlanet Science Congress 2024, Berlin, Germany, 8/09/24. https://doi.org/10.5194/epsc2024-730

Exploration of high mass subsurface structures in the northern hemisphere with joint flexure and mantle convection modelling of the Martian gravity field. / Root, B.C.; Alkahal, R.; Qin, W. et al.
EPSC Abstracts: Europlanet Science Congress 2024. Vol. 17 2024. EPSC 2024-730.

Research output: Chapter in Book/Conference proceedings/Edited volume › Conference contribution › Scientific › peer-review

TY - GEN

T1 - Exploration of high mass subsurface structures in the northern hemisphere with joint flexure and mantle convection modelling of the Martian gravity field

AU - Root, B.C.

AU - Alkahal, R.

AU - Qin, W.

AU - Thieulot, Cedric

PY - 2024

Y1 - 2024

N2 - NASA’s InSight mission has brought new information about the Martian lithosphere (Banerdt et al. 2020), which warrants a re-analysis of the support of the crustal and sub-crustal masses. Furthermore, the discovery of a possible mantle plume underneath the region south of Elysium Mons (Broquet et al. 2023), gives evidence for recent magmatic activity underneath the crust of Mars causing dynamic support to volcanic structures.

AB - NASA’s InSight mission has brought new information about the Martian lithosphere (Banerdt et al. 2020), which warrants a re-analysis of the support of the crustal and sub-crustal masses. Furthermore, the discovery of a possible mantle plume underneath the region south of Elysium Mons (Broquet et al. 2023), gives evidence for recent magmatic activity underneath the crust of Mars causing dynamic support to volcanic structures.

U2 - 10.5194/epsc2024-730

DO - 10.5194/epsc2024-730

M3 - Conference contribution

VL - 17

BT - EPSC Abstracts

T2 - Europlanet Science Congress 2024

Y2 - 8 September 2024 through 13 September 2024

ER -

Exploration of high mass subsurface structures in the northern hemisphere with joint flexure and mantle convection modelling of the Martian gravity field

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