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The Evolution of Meteoroid Streams. Modelling the Orbital Evolution of the Perseid Meteoroids. Modelling the Ejection of Meteoroids from Comets. Sources of Interplanetary Dust. Dermott, S. The Contamination of Iapetus by Phoebe Dust. Martian Self-Sustaining Dust Torus.

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Brownlee, D. Igenbergs, E. Hypervelocity Capture of Meteoroids in Aerogel. The Elemental Composition of Interplanetary Dust.

F1 – Commission F1 Meteors, Meteorites and Interplanetary Dust

Collection and Microanalysis of Antarctic Micrometeorites. Isotopic Anomalies in Interplanetary Dust Particles. Flynn, G.

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Optical and Thermal Properties of Zodiacal Dust. Berriman, G. Grogan, K. Clementine Photographs of the Inner Zodiacal Light.

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Time Variation of the Solar Dust Cloud. Modelcalculations of Near Solar Dust Properties. Dust Particles Near the Sun. Composition and Optical Properties of Cometary Dust. Morphology of Cometary Dust Coma and Tail.

Interplanetary dust measurements near the Earth

Tentative Interpretation of the Dichotomy Between Comets. Recent Observational Developments.

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Scattering Properties of Dust Particles in Weightlessness. Optical Properties of Fluffy Particles. Scattering Properties of Cometary Grains.

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  • Remnants Of Our Solar System's Formation Found In Our Interplanetary Dust.
  • How is it distributed?.
  • Modelling the Temperature of Cometary Particles. Sublimation of Interplanetary Dust. Laboratory Experiments on Carbonaceous and Silicate Materials. This limits the possible encounter trajectories for these particles to relatively circular, prograde orbits.

    Earth's Interplanetary Dust Traced to Comets by Rosetta Probe | Space

    As a result, it is unlikely that these IDPs are from Earth-crossing comets or asteroids. Asteroids, and comets having low inclinations and perihelia outside 1. Chemical and mineralogical information suggests that the pyroxene-rich IDPs are from comets and the layer-lattice silicate-rich IDPs are from asteroids.

    The collected IDPs dominated by olivine appear to include a larger fraction of particles heating above degrees C, suggesting that these particles were captured from more eccentric orbits.