火星探査機が予期せぬ鉱物を発見(Unburied treasure: Rover researchers find unexpected minerals on Mars)

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2025-03-04 パデュー大学

パデュー大学のロジャー・ウィーンス教授率いる研究チームは、NASAの探査車パーサヴィアランスを用いて、火星表面でカオリナイトやスピネルを含む岩石を発見しました。これらの鉱物は通常、温暖で湿潤な環境で形成されるため、火星がかつて地球のような環境を持っていた可能性を示唆しています。しかし、これらの岩石の起源は未解明であり、今後の研究が必要とされています。

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ジェゼロ・クレーターの高アルミニウム岩石が明らかにする初期火星の激しい変質 Intense alteration on early Mars revealed by high-aluminum rocks at Jezero crater

C. Royer,C. C. Bedford,J. R. Johnson,B. H. N. Horgan,A. Broz,O. Forni,S. Connell,R. C. Wiens,L. Mandon,B. S. Kathir,E. M. Hausrath,A. Udry,J. M. Madariaga,E. Dehouck,R. B. Anderson,P. Beck,O. Beyssac,É. Clavé,S. M. Clegg,E. Cloutis,T. Fouchet,T. S. J. Gabriel,B. J. Garczynski,A. Klidaras,… S. Maurice
Communications Earth & Environment  Published:07 November 2024
DOI:https://doi.org/10.1038/s43247-024-01837-2

火星探査機が予期せぬ鉱物を発見(Unburied treasure: Rover researchers find unexpected minerals on Mars)

Abstract

The NASA Perseverance rover discovered light-toned float rocks scattered across the surface of Jezero crater that are particularly rich in alumina ( ~ 35 wt% Al2O3) and depleted in other major elements (except silica). These unique float rocks have heterogeneous mineralogy ranging from kaolinite/halloysite-bearing in hydrated samples, to spinel-bearing in dehydrated samples also containing a dehydrated Al-rich phase. Here we describe SuperCam and Mastcam-Z observations of the float rocks, including the first in situ identification of kaolinite or halloysite on another planet, and dehydrated phases including spinel and apparent partially dehydroxylated kaolinite. The presence of spinel in these samples is likely detrital in origin, surviving kaolinitization, pointing to an ultramafic origin. However, the association of low hydration with increased Al2O3 abundances suggests heating-induced dehydration which could have occurred during the lithification or impact excavation of these rocks. Given the orbital context of kaolinite-bearing megabreccia in the Jezero crater rim, we propose an origin for these rocks involving intense aqueous alteration of the parent material, followed by dehydration/lithification potentially through impact processes, and dispersion into Jezero crater through flood or impact-related processes.

1701物理及び化学
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