Japan Geoscience Union Meeting 2014

Presentation information

Oral

Symbol P (Space and Planetary Sciences) » P-PS Planetary Sciences

[P-PS25_2AM2] Meteorite anatomy: synthetic analyses of solar system matter

Fri. May 2, 2014 11:00 AM - 12:45 PM 213 (2F)

Convener:*Yusuke Seto(Graduate School of Science, Kobe University), Tomohiro Usui(Department of Earth and Planetary Sciences,Tokyo Institute of Technology), Shoichi Itoh(Graduate school of Science, Kyoto University), Hikaru Yabuta(Osaka University, Department of Earth and Space Science), Hitoshi Miura(Graduate School of Natural Sciences, Department of Information and Biological Sciences, Nagoya City University), Chair:Hitoshi Miura(Graduate School of Natural Sciences, Department of Information and Biological Sciences, Nagoya City University), Hikaru Yabuta(Osaka University, Department of Earth and Space Science)

11:15 AM - 11:30 AM

[PPS25-09] Artificial cosmic spherules produced by heating and quenching experiments

*Takaaki GONDO1, Hiroshi ISOBE1 (1.Grad. Sch. Sci. Tech., Kumamoto Univ.)

Keywords:micrometeorite, carbonaceous chondrite, H chondrite, atmospheric heating, cosmic spherule

Micrometeorites (MMs) are extraterrestrial fine particles derived from asteroids and comets and continuously falling to the Earth. Depending on their velocity, mass and entry angle, micrometeorites have undergone various degrees of heating during the atmospheric entry within a few seconds. This heating lead to significant textural, mineralogical and chemical modifications to MMs. The MMs larger them 70 micron meters in diameter show variously melted textures. In particular, completely melted micrometeorites are known as cosmic spherules. Cosmic spherules have experienced large degrees of melting of primary phases during atmospheric entry, and form molten droplets. In this study, we carried out rapid heating and quenching experiments on fine particles of three kinds of meteorites (CV, CM and H chondrite) to reproduce cosmic spherules by atmospheric entry. The run products of meteorites as starting materials show quite analogous textures to cosmic spherules including porphyritic olivine and barred olivine. The most of molten particles show spherical shape due to surface tension of the silicate melt. The outside shape of the particles is various depending on melt fraction of the particle. We successfully reproduced artificial cosmic spherules with remarkably analogous textures to natural ones. We can compare textural variations of cosmic spherules to run products and possible precursors of cosmic spherules. Analogy of the run products to cosmic spherules can be applied from textural, mineralogical and chemical modifications during atmospheric entry to estimate abundance of the interplanetary fine particles in the vicinity of the Earth's orbit.