Trace element partitioning between orthopyroxene and anhydrous silicate melt on the lherzolite solidus from 1.1 to 3.2 GPa and 1,230 to 1,535°C in the model system Na2O–CaO–MgO–Al2O3–SiO2

詳細情報 詳細情報について

• CRID

  1362825896049352192

• DOI

  10.1007/s00410-008-0346-5

• ISSN

  14320967

  00107999

• Web Site

  http://link.springer.com/content/pdf/10.1007/s00410-008-0346-5.pdf

  http://link.springer.com/article/10.1007/s00410-008-0346-5/fulltext.html

  http://link.springer.com/content/pdf/10.1007/s00410-008-0346-5

• データソース種別

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