An igneous fragment from cluster IDP L2011#21: An analog for the source of pyrrhotite and taenite in comet 81P/Wild 2 captured in Stardust aerogel
Author:
Affiliation:
1. Department of Earth and Planetary Sciences; MSC03-2040, 1-University of New Mexico; Albuquerque; New Mexico; 87131-0001; USA
Publisher
Wiley
Subject
Space and Planetary Science,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/maps.12153/fullpdf
Reference67 articles.
1. Evidence for aqueous activity on comet 81P/Wild 2 from sulfide mineral assemblages in Stardust samples and CI chondrites;Berger;Geochimica et Cosmochimica Acta,2011
2. Chemically anomalous, pre-accretionally irradiated grains in interplanetary dust from comets;Bradley;Science,1994a
3. Nanometer-scale mineralogy and petrography of fine-grained aggregates in anhydrous interplanetary dust particles;Bradley;Geochimica et Cosmochimica Acta,1994b
4. Pyroxene whiskers and platelets in interplanetary dust: Evidence of vapour phase growth;Bradley;Nature,1983
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1. The smallest comet 81P/Wild 2 dust dances around the CI composition;Meteoritics & Planetary Science;2015-09-10
2. Single minerals, carbon- and ice-coated single minerals for calibration of GIADA onboard ROSETTA to comet 67P/Churyumov–Gerasimenko;Planetary and Space Science;2014-10
3. Two refractory Wild 2 terminal particles from a carrot‐shaped track characterized combining MIR / FIR /Raman microspectroscopy and FE ‐ SEM / EDS analyses;Meteoritics & Planetary Science;2014-03-04
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