High Pressure Earth Science. Physical Properties of Silicate Melt at High Pressure.

• SUZUKI Akio

  Institute of Mineraloby Petrology and Economic Geology, Tohoku University

Bibliographic Information

Other Title

• 高圧地球科学　　超高圧下における珪酸塩融体の物性
• チョウコウアツカ ニ オケル ケイサンエンユウタイ ノ ブッセイ

Abstract

In order to understand the magmatic process, a knowledge of the physical properties of silicate melt is required. Density and viscosity are especially fundamental properties, which control the migration of magmas and the separation of residual crystals. In this article, recent advances in the investigation of silicate melt at high pressure are reviewed.

Journal

• The Review of High Pressure Science and Technology

  The Review of High Pressure Science and Technology 9 (1), 11-18, 1999

  The Japan Society of High Pressure Science and Technology

Keywords

• high pressure
• multi anvil
• silicate melt
• magma
• density
• diamond
• equation of state

Details

• CRID: 1390282679358428032
• NII Article ID: 10002849695
• NII Book ID: AN10452913
• DOI: 10.4131/jshpreview.9.11
• COI: 1:CAS:528:DyaK1MXhvFOlt7g%3D
• ISSN: 13481940
• ISSN: 0917639X
• ISSN: http://id.crossref.org/issn/0917639X
• NDL BIB ID: 4674344
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I4674344
• Text Lang: ja
• Data Source:
  • JaLC
  • NDL
  • Crossref
  • CiNii Articles
• Abstract License Flag: Disallowed