Development of High-Pressure and High-Temperature In Situ X-ray Diffraction Experiments and the Study of the Earth's Deep Materials

• YAGI Takehiko

  Institute for Solid State Physics, University of Tokyo

Bibliographic Information

Other Title

• 高温高圧Ｘ線実験の発展と地球深部物質の研究
• ブリッジマン賞受賞記念 高温高圧X線実験の発展と地球深部物質の研究
• ブリッジマンショウ ジュショウ キネン コウオン コウアツ Xセン ジッケン ノ ハッテン ト チキュウ シンブ ブッシツ ノ ケンキュウ

Abstract

This is a review talk presented as a “Bridgman Award Lecture” at the AIRAPT21 held in Catania, Italy, in September 2007. History of the developments of high-pressure and high-temperature experiments to clarify the nature of seismic discontinuities of the Earth’s deep interior is briefly reviewed, together with the scientific contributions of the author. Extension of the pressure range and developments of new techniques, particularly high pressure in situ X-ray diffraction, played important role for better understanding the Earth’s deep interior.

Journal

• The Review of High Pressure Science and Technology

  The Review of High Pressure Science and Technology 18 (2), 160-169, 2008

  The Japan Society of High Pressure Science and Technology

Keywords

• Earth’s deep interior
• seismic discontinuity
• high pressure experiments
• in situ X-ray
• olivine spinel transition
• post spinel transition

Details

• CRID: 1390001204380949888
• NII Article ID: 10021153645
• NII Book ID: AN10452913
• DOI: 10.4131/jshpreview.18.160
• ISSN: 13481940
• ISSN: 0917639X
• NDL BIB ID: 9536613
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I9536613
• Text Lang: ja
• Data Source:
  • JaLC
  • NDL
  • Crossref
  • CiNii Articles
  • KAKEN
• Abstract License Flag: Disallowed