Constraints on the Emplacement of Martian Nakhlite Igneous Rocks and Their Source Volcano From Advanced Micro‐Petrofabric Analysis-Reference-Cited by-同舟云学术

Constraints on the Emplacement of Martian Nakhlite Igneous Rocks and Their Source Volcano From Advanced Micro‐Petrofabric Analysis

Published:2022-06 Issue:6 Volume:127 Page:
ISSN:2169-9097
Container-title:Journal of Geophysical Research: Planets
language:en
Short-container-title:JGR Planets

Author:

Griffin S.¹^ORCID,Daly L.¹²³⁴^ORCID,Keller T.¹^ORCID,Piazolo S.⁵^ORCID,Forman L. V.²⁶^ORCID,Lee M. R.¹^ORCID,Baumgartner R. J.⁷⁸^ORCID,Trimby P. W.⁹^ORCID,Benedix G. K.²⁶¹⁰^ORCID,Irving A. J.¹¹,Hoefnagels B.¹²

Affiliation:

1. School of Geographical and Earth Sciences University of Glasgow Glasgow UK

2. Space Science and Technology Centre School of Earth and Planetary Sciences Curtin University Perth WA Australia

3. Australian Centre for Microscopy and Microanalysis The University of Sydney Sydney NSW Australia

4. Department of Materials University of Oxford Oxford UK

5. School of Earth and Environment University of Leeds Leeds UK

6. Department of Earth and Planetary Sciences Western Australia Museum Perth WA Australia

7. School of Biological, Earth and Environmental Sciences The University of New South Wales Kensington NSW Australia

8. CSIRO Mineral Resources Australian Resources Research Centre Kensington WA Australia

9. Oxford Instruments Nano Analysis High Wycombe UK

10. Planetary Sciences Institute Tucson AZ USA

11. Department of Earth and Space Sciences University of Washington Seattle WA USA

12. Big Bang Meteorites

Funder

Science and Technology Facilities Council

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JE007080

Reference79 articles.

1. Launch of martian meteorites in oblique impacts

2. Grain detection from 2d and 3d EBSD data—Specification of the MTEX algorithm

3. Plastic deformation and development of clinopyroxene lattice preferred orientations in eclogites

4. Numerical modelling of erosion and assimilation of sulfur-rich substrate by martian lava flows: Implications for the genesis of massive sulfide mineralization on Mars

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2. Can the Magmatic Conditions of the Martian Nakhlites be Discerned via Investigation of Clinopyroxene and Olivine Intracrystalline Misorientations?;Journal of Geophysical Research: Planets;2022-06