Literature DB >> 10481004

An infrared spectral match between GEMS and interstellar grains.

J P Bradley1, L P Keller, T P Snow, M S Hanner, G J Flynn, J C Gezo, S J Clemett, D E Brownlee, J E Bowey.   

Abstract

Infrared spectral properties of silicate grains in interplanetary dust particles (IDPs) were compared with those of astronomical silicates. The approximately 10-micrometer silicon-oxygen stretch bands of IDPs containing enstatite (MgSiO3), forsterite (Mg2SiO4), and glass with embedded metal and sulfides (GEMS) exhibit fine structure and bandwidths similar to those of solar system comets and some pre-main sequence Herbig Ae/Be stars. Some GEMS exhibit a broad, featureless silicon-oxygen stretch band similar to those observed in interstellar molecular clouds and young stellar objects. These GEMS provide a spectral match to astronomical "amorphous" silicates, one of the fundamental building blocks from which the solar system is presumed to have formed.

Entities:  

Keywords:  NASA Discipline Exobiology; Non-NASA Center

Mesh:

Substances:

Year:  1999        PMID: 10481004     DOI: 10.1126/science.285.5434.1716

Source DB:  PubMed          Journal:  Science        ISSN: 0036-8075            Impact factor:   47.728


  2 in total

Review 1.  Cometary dust: the diversity of primitive refractory grains.

Authors:  D H Wooden; H A Ishii; M E Zolensky
Journal:  Philos Trans A Math Phys Eng Sci       Date:  2017-07-13       Impact factor: 4.226

2.  Multiple generations of grain aggregation in different environments preceded solar system body formation.

Authors:  Hope A Ishii; John P Bradley; Hans A Bechtel; Donald E Brownlee; Karen C Bustillo; James Ciston; Jeffrey N Cuzzi; Christine Floss; David J Joswiak
Journal:  Proc Natl Acad Sci U S A       Date:  2018-06-11       Impact factor: 11.205

  2 in total

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