Laboratory VIS–NIR reflectance measurements of heated Vesta regolith analogs: Unraveling the spectral properties of the pitted impact deposits on Vesta

IF 2.2 4区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
T. Michalik, A. Maturilli, E. A. Cloutis, K. Stephan, R. Milke, K.-D. Matz, R. Jaumann, L. Hecht, H. Hiesinger, K. A. Otto
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Abstract

Pitted impact deposits on Vesta show higher reflectance and pyroxene absorption band strengths compared to their immediate surroundings and other typical Vestan materials. We investigated whether heating to different temperatures for different durations of Vestan regolith analog materials can reproduce these spectral characteristics using mixtures of HEDs, the carbonaceous chondrite Murchison, and terrestrial analogs. We find no consistent spectral trend due merely to temperature increases, but observed that the interiors of many heated samples show both higher reflectance and pyroxene band I strength than their heated surfaces. With electron probe microanalysis, we additionally observe the formation of hematite, which could account for the higher reflectance. The presence of hematite indicates oxidation occurring in the sample interiors. In combination with heat, this might cause the increase of pyroxene band strengths through migration of iron cations. The effect grows larger with increasing temperature and duration, although temperature appears to play the more dominant role. A higher proportion of Murchison or the terrestrial carbonaceous chondrite analog within our mixtures also appears to facilitate the onset of oxidation. Our observations suggest that both the introduction of exogenic material on Vesta as well as the heating from impacts were necessary to enable the process (possibly oxidation) causing the observed spectral changes.

Abstract Image

对加热的灶神星碎屑岩类似物进行实验室 VIS-NIR 反射测量:揭示灶神星上凹坑状撞击沉积物的光谱特性
灶神星上的凹坑状撞击沉积物与其周围环境和其他典型的灶神星材料相比,显示出更高的反射率和辉石吸收带强度。我们使用 HEDs、碳质软玉 Murchison 和陆地类似物的混合物,研究了将灶神星碎屑岩类似物加热到不同温度并持续不同时间是否能再现这些光谱特征。我们没有发现仅仅由于温度升高而导致的一致的光谱趋势,但观察到许多加热样品的内部显示出比加热表面更高的反射率和辉石带 I 强度。通过电子探针显微分析,我们还观察到赤铁矿的形成,这可能是反射率较高的原因。赤铁矿的存在表明样品内部发生了氧化。结合热量,这可能会通过铁阳离子的迁移导致辉石带强度的增加。随着温度的升高和时间的延长,这种影响会越来越大,不过温度似乎起着更加主要的作用。在我们的混合物中,较高比例的默奇森或陆地碳质软玉类似物似乎也会促进氧化的开始。我们的观测结果表明,灶神星上外生物质的引入以及撞击产生的热量对于实现导致观测到的光谱变化的过程(可能是氧化)都是必要的。
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来源期刊
Meteoritics & Planetary Science
Meteoritics & Planetary Science 地学天文-地球化学与地球物理
CiteScore
3.90
自引率
31.80%
发文量
121
审稿时长
3 months
期刊介绍: First issued in 1953, the journal publishes research articles describing the latest results of new studies, invited reviews of major topics in planetary science, editorials on issues of current interest in the field, and book reviews. The publications are original, not considered for publication elsewhere, and undergo peer-review. The topics include the origin and history of the solar system, planets and natural satellites, interplanetary dust and interstellar medium, lunar samples, meteors, and meteorites, asteroids, comets, craters, and tektites. Our authors and editors are professional scientists representing numerous disciplines, including astronomy, astrophysics, physics, geophysics, chemistry, isotope geochemistry, mineralogy, earth science, geology, and biology. MAPS has subscribers in over 40 countries. Fifty percent of MAPS'' readers are based outside the USA. The journal is available in hard copy and online.
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