New Numerically Derived Scaling Relationships for Impact Basins on Mars
Most impact basins are believed to have formed during the early epochs of planetary evolution. The planet's gravity, internal structure, and thermal regime have the strongest control over their formation. Because of this, we can use the geophysical constraints on Mars' interior composition...
| Main Authors: | , , |
|---|---|
| Format: | Journal Article |
| Published: |
2024
|
| Online Access: | http://purl.org/au-research/grants/arc/FT210100063 http://hdl.handle.net/20.500.11937/96132 |
| _version_ | 1848766097867669504 |
|---|---|
| author | Branco, H.C. Miljkovic, Katarina Plesa, A.C. |
| author_facet | Branco, H.C. Miljkovic, Katarina Plesa, A.C. |
| author_sort | Branco, H.C. |
| building | Curtin Institutional Repository |
| collection | Online Access |
| description | Most impact basins are believed to have formed during the early epochs of planetary evolution. The planet's gravity, internal structure, and thermal regime have the strongest control over their formation. Because of this, we can use the geophysical constraints on Mars' interior composition, structure, and geophysical evolution derived from the InSight mission to better understand the formation of impact basins on the planet. To achieve this, we performed numerical simulations of large impacts using the iSALE shock physics code. We investigated the effects of temperature and crustal thickness variations on impact basin size and morphology. Our scaling relationships indicate that: (a) basins formed in a warmer crust have larger final diameters in comparison to basins formed in a colder crust, a difference that is further accentuated as basin size gets bigger; and (b) the largest impact basins on Mars were created by impactors ranging from 35 to 680 km in diameter, up to ∼32% larger than estimates based on classical scaling. Our results expand the current understanding of the extent of early and large impact bombardment on Mars and provide a more comprehensive knowledge of impact basin formation on planetary surfaces. |
| first_indexed | 2025-11-14T11:45:44Z |
| format | Journal Article |
| id | curtin-20.500.11937-96132 |
| institution | Curtin University Malaysia |
| institution_category | Local University |
| last_indexed | 2025-11-14T11:45:44Z |
| publishDate | 2024 |
| recordtype | eprints |
| repository_type | Digital Repository |
| spelling | curtin-20.500.11937-961322024-11-07T01:23:45Z New Numerically Derived Scaling Relationships for Impact Basins on Mars Branco, H.C. Miljkovic, Katarina Plesa, A.C. Most impact basins are believed to have formed during the early epochs of planetary evolution. The planet's gravity, internal structure, and thermal regime have the strongest control over their formation. Because of this, we can use the geophysical constraints on Mars' interior composition, structure, and geophysical evolution derived from the InSight mission to better understand the formation of impact basins on the planet. To achieve this, we performed numerical simulations of large impacts using the iSALE shock physics code. We investigated the effects of temperature and crustal thickness variations on impact basin size and morphology. Our scaling relationships indicate that: (a) basins formed in a warmer crust have larger final diameters in comparison to basins formed in a colder crust, a difference that is further accentuated as basin size gets bigger; and (b) the largest impact basins on Mars were created by impactors ranging from 35 to 680 km in diameter, up to ∼32% larger than estimates based on classical scaling. Our results expand the current understanding of the extent of early and large impact bombardment on Mars and provide a more comprehensive knowledge of impact basin formation on planetary surfaces. 2024 Journal Article http://hdl.handle.net/20.500.11937/96132 10.1029/2023JE008217 http://purl.org/au-research/grants/arc/FT210100063 https://creativecommons.org/licenses/by-nc/4.0/ fulltext |
| spellingShingle | Branco, H.C. Miljkovic, Katarina Plesa, A.C. New Numerically Derived Scaling Relationships for Impact Basins on Mars |
| title | New Numerically Derived Scaling Relationships for Impact Basins on Mars |
| title_full | New Numerically Derived Scaling Relationships for Impact Basins on Mars |
| title_fullStr | New Numerically Derived Scaling Relationships for Impact Basins on Mars |
| title_full_unstemmed | New Numerically Derived Scaling Relationships for Impact Basins on Mars |
| title_short | New Numerically Derived Scaling Relationships for Impact Basins on Mars |
| title_sort | new numerically derived scaling relationships for impact basins on mars |
| url | http://purl.org/au-research/grants/arc/FT210100063 http://hdl.handle.net/20.500.11937/96132 |