首页> 外文期刊>Icarus: International Journal of Solar System Studies >Three-dimensional spectral analysis of compositional heterogeneity at Arruntia crater on (4) Vesta using Dawn FC
【24h】

Three-dimensional spectral analysis of compositional heterogeneity at Arruntia crater on (4) Vesta using Dawn FC

机译:使用黎明FC对(4)Vesta上Arruntia火山口成分异质性进行三维光谱分析

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

We introduce an innovative three-dimensional spectral approach (three band parameter space with polyhedrons) that can be used for both qualitative and quantitative analyzes improving the characterization of surface compositional heterogeneity of (4) Vesta. It is an advanced and more robust methodology compared to the standard two-dimensional spectral approach (two band parameter space). The Dawn Framing Camera (FC) color data obtained during High Altitude Mapping Orbit (resolution similar to 60 m/pixel) is used. The main focus is on the howardite-eucrite-diogenite (HED) lithologies containing carbonaceous chondritic material, olivine, and impact-melt. The archived spectra of HEDs and their mixtures, from RELAB, HOSERLab and USGS databases as well as our laboratory-measured spectra are used for this study. Three-dimensional convex polyhedrons are defined using computed band parameter values of laboratory spectra. Polyhedrons based on the parameters of Band Tilt (R-0.92 mu m/R-0.96 mu m), Mid Ratio ((R-0.75 mu m/R-0.83 mu m)/(R-0.83 mu m/R-0.92 mu m)) and reflectance at 0.55 mu m (R-0.55 mu m) are chosen for the present analysis. An algorithm in IDL programming language is employed to assign FC data points to the respective polyhedrons. The Arruntia region in the northern hemisphere of Vesta is selected for a case study because of its geological and mineralogical importance. We observe that this region is eucrite-dominated howarditic in composition. The extent of olivine-rich exposures within an area of 2.5 crater radii is similar to 12% larger than the previous finding (Thangjam, G. et al. [2014]. Meteorit. Planet. Sci. 49, 1831-1850). Lithologies of nearly pure CM2-chondrite, olivine, glass, and diogenite are not found in this region. Although there are no unambiguous spectral features of impact melt, the investigation of morphological features using FC clear filter data from Low Altitude Mapping Orbit (resolution similar to 18 m/pixel) suggests potential impact-melt features inside and outside of the crater. Our spectral approach can be extended to the entire Vestan surface to study the heterogeneous surface composition and its geology. (C) 2015 Elsevier Inc. All rights reserved.
机译:我们介绍了一种创新的三维光谱方法(带多面体的三带参数空间),该方法可用于定性和定量分析,从而改善(4)Vesta表面组成异质性的特征。与标准的二维频谱方法(两个波段参数空间)相比,它是一种先进且更强大的方法。使用在高海拔测绘轨道(分辨率类似于60 m /像素)中获得的黎明取景相机(FC)颜色数据。主要重点是含有碳质软骨状材料,橄榄石和冲击熔体的芒硝-真石-二元岩(HED)岩性。来自RELAB,HOSERLab和USGS数据库的HED及其混合物的存档光谱以及我们实验室测量的光谱用于本研究。使用计算得到的实验室光谱带参数值定义三维凸多面体。基于Band Tilt(R-0.92μm/ R-0.96μm),Mid Ratio((R-0.75μm/ R-0.83μm)/(R-0.83μm/ R-0.92μm)的参数的多面体m))和0.55微米(R-0.55微米)的反射率用于本分析。采用IDL编程语言的算法将FC数据点分配给相应的多面体。选择维斯塔北半球的Arruntia地区作为案例研究,因为其地质和矿物学重要性。我们观察到,该区域在成分上是尤氏体占主导地位。在2.5个火山口半径范围内,富橄榄石的暴露程度比以前的发现大12%(Thangjam,G.等人[2014]。Meteorit。Planet。Sci。49,1831-1850)。在该区域没有发现近乎纯净的CM2球粒陨石,橄榄石,玻璃和重辉岩的岩性。尽管没有明确的冲击熔体光谱特征,但是使用低空测绘轨道(分辨率类似于18 m /像素)的FC透明滤镜数据对形态特征进行的研究表明,火山口内部和外部都有潜在的冲击熔体特征。我们的光谱方法可以扩展到整个Vestan表面,以研究非均质表面成分及其地质情况。 (C)2015 Elsevier Inc.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号