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Crystallographic studies on interplanetary dust particles

Research Project

Project/Area Number 10440156
Research Category

Grant-in-Aid for Scientific Research (B)

Allocation TypeSingle-year Grants
Section一般
Research Field Petrology/Mineralogy/Science of ore deposit
Research InstitutionHigh Energy Accelerator Research Organization

Principal Investigator

OHSUMI Kazumasa  Institute of Materials Structure Science, High Energy Accelerator Research Organization, Professor, 物質構造科学研究所, 教授 (70011715)

Project Period (FY) 1998 – 1999
Project Status Completed (Fiscal Year 1999)
Budget Amount *help
¥11,200,000 (Direct Cost: ¥11,200,000)
Fiscal Year 1999: ¥1,200,000 (Direct Cost: ¥1,200,000)
Fiscal Year 1998: ¥10,000,000 (Direct Cost: ¥10,000,000)
Keywordsinterplanetary dust particles / synchrotron radiation / minute crystal / modulated structure / new mineral
Research Abstract

The aim of this investigation is to contribute materials science of the solar system based on analyses of the interplanetary dust particles (IDPs) collected with space shuttle by NASA. In order to carry out this study, we identify minerals included in IDPs, analyze their textures of minerals and also crystallographic distortion of crystals.
The results, instrumentation and analyses, performed in this two years are described below.
1. Tapered glass capillary optics on the moving stage is installed in the existing diffraction equipment to make micro-beam with high intensities.
2. High spatial resolution of imaging plate)detector instead of X-ray film) readout system is achieved in the existing diffraction equipment.
3. Diffraction data of two (Fe, Ni) sulfides of IDPs (named L2005AE6 and L2005AG17) are obtained by Laue and oscillation method using polychromatic and monochromated synchrotron radiation respectively at the Photon Factory, KEK. They are identified to be NA-type and 3C-type of pyrrhotite. The former has modulation along a-axis and the latter along c-axis. They are first examples from nature, I.e. they are new minerals. Beside 3C-type in the latter sample by four week but distinct Debye-Scherrer lines in the diffraction pattern. The chemical composition of the present 3C-type is different from that of synthetic 3C-type of which structure is already determined. The structure model of the present 3C-type is analyzed, and determined by making use of two extraordinary conditions of missing reflections exhibited in the diffraction pattern.
The results obtained by this investigation are presented at IMA meeting, Canada, 1998, at AsCA98, Malaysia, 1998, and Denver meeting, USA, 1999 as invited papers.

Report

(3 results)
  • 1999 Annual Research Report   Final Research Report Summary
  • 1998 Annual Research Report
  • Research Products

    (4 results)

All Other

All Publications (4 results)

  • [Publications] Takeshi Mikouchi: "X-ray diffraction study of shocked plagioclase in martian and lunar meteorites with the micro-area Laue method using synchrotron radiation"23rd NIPR Symposium. 23. 80-82 (1998)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1999 Final Research Report Summary
  • [Publications] A. V. Ivanov: "Florenskyite, FeTiP, a new phosphide from the Kaidun meterorite"American Mineralogist,. (Submitted).

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      1999 Final Research Report Summary
  • [Publications] Takeshi Mikouchi: "X-ray diffraction study of shocked plagioclase in martian and lunar meteorites with the micro-area Laue method using synchrotoron radiation"23rd NIPR Symposium. 23. 80-82 (1998)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1999 Final Research Report Summary
  • [Publications] A. V. Ivanov: "Florenskyite, FeTiP, a new phosphide from the Kaidum meterorite"American Minralogist. (Submitted).

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      1999 Final Research Report Summary

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Published: 1998-04-01   Modified: 2016-04-21  

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