Genesis of Cenozoic low-Ca alkaline basalts in the Nanjing basaltic field, eastern China: The case for mantle xenolith-magma interaction
Version of Record online: 31 MAY 2013
©2013. American Geophysical Union. All Rights Reserved.
Geochemistry, Geophysics, Geosystems
Volume 14, Issue 5, pages 1660–1677, May 2013
How to Cite
2013), Genesis of Cenozoic low-Ca alkaline basalts in the Nanjing basaltic field, eastern China: The case for mantle xenolith-magma interaction, Geochem. Geophys. Geosyst., 14, 1660–1677, doi:10.1002/ggge.20127., , , , and (
- Issue online: 27 JUN 2013
- Version of Record online: 31 MAY 2013
- Accepted manuscript online: 29 MAR 2013 12:00AM EST
- Manuscript Revised: 21 MAR 2013
- Manuscript Accepted: 21 MAR 2013
- Manuscript Received: 7 JAN 2013
All supporting information may be found in the online version of this article.
|Table_S1.xlsx||Excel 2007 spreadsheet||22K||Contains major element (wt %) compositions of minerals from one peridotite xenolith (TS-X03) hosted in Tashan basalts.|
|Table_S2.doc||Word document||79K||Contains trace element compositions (10-9) of blank and international standards (10-6).|
|readme.txt||Word 2007 document||1K||Supporting information|
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