Petrology of NWA 7533: Formation by Impacts on Ancient Martian Crust
NWA 7533 contains FeNi grains (~1μm), up to 4.5% Ni in pyrite, and 500 nm Os-Ir-rich particles. Lithic clasts are pyroxenite, norite and zircon-bearing monzonite. The impact melt can be modeled as a mixture of crystal clasts and is poor in monzonite.
| Main Authors: | , , , , , , , , , , , |
|---|---|
| Format: | Conference Paper |
| Published: |
WILEY-BLACKWELL
2013
|
| Online Access: | http://hdl.handle.net/20.500.11937/11731 |
| _version_ | 1848747884097306624 |
|---|---|
| author | Hewins, R. Zanda, B. Humayun, M. Lorand, J. Deldicque, D. Pont, S. Fieni, C. Nemchin, Alexander Grange, M. Kennedy, A. Goepel, C. Lewin, E. |
| author_facet | Hewins, R. Zanda, B. Humayun, M. Lorand, J. Deldicque, D. Pont, S. Fieni, C. Nemchin, Alexander Grange, M. Kennedy, A. Goepel, C. Lewin, E. |
| author_sort | Hewins, R. |
| building | Curtin Institutional Repository |
| collection | Online Access |
| description | NWA 7533 contains FeNi grains (~1μm), up to 4.5% Ni in pyrite, and 500 nm Os-Ir-rich particles. Lithic clasts are pyroxenite, norite and zircon-bearing monzonite. The impact melt can be modeled as a mixture of crystal clasts and is poor in monzonite. |
| first_indexed | 2025-11-14T06:56:14Z |
| format | Conference Paper |
| id | curtin-20.500.11937-11731 |
| institution | Curtin University Malaysia |
| institution_category | Local University |
| last_indexed | 2025-11-14T06:56:14Z |
| publishDate | 2013 |
| publisher | WILEY-BLACKWELL |
| recordtype | eprints |
| repository_type | Digital Repository |
| spelling | curtin-20.500.11937-117312019-10-25T07:40:00Z Petrology of NWA 7533: Formation by Impacts on Ancient Martian Crust Hewins, R. Zanda, B. Humayun, M. Lorand, J. Deldicque, D. Pont, S. Fieni, C. Nemchin, Alexander Grange, M. Kennedy, A. Goepel, C. Lewin, E. NWA 7533 contains FeNi grains (~1μm), up to 4.5% Ni in pyrite, and 500 nm Os-Ir-rich particles. Lithic clasts are pyroxenite, norite and zircon-bearing monzonite. The impact melt can be modeled as a mixture of crystal clasts and is poor in monzonite. 2013 Conference Paper http://hdl.handle.net/20.500.11937/11731 WILEY-BLACKWELL restricted |
| spellingShingle | Hewins, R. Zanda, B. Humayun, M. Lorand, J. Deldicque, D. Pont, S. Fieni, C. Nemchin, Alexander Grange, M. Kennedy, A. Goepel, C. Lewin, E. Petrology of NWA 7533: Formation by Impacts on Ancient Martian Crust |
| title | Petrology of NWA 7533: Formation by Impacts on Ancient Martian Crust |
| title_full | Petrology of NWA 7533: Formation by Impacts on Ancient Martian Crust |
| title_fullStr | Petrology of NWA 7533: Formation by Impacts on Ancient Martian Crust |
| title_full_unstemmed | Petrology of NWA 7533: Formation by Impacts on Ancient Martian Crust |
| title_short | Petrology of NWA 7533: Formation by Impacts on Ancient Martian Crust |
| title_sort | petrology of nwa 7533: formation by impacts on ancient martian crust |
| url | http://hdl.handle.net/20.500.11937/11731 |