Iowaite in serpentinite muds at Sites 778, 779, 780, and 784: a possible cause for the low chlorinity of pore waters
The <63-µm fractions of serpentinite muds from two seamounts on the Mariana and Izu-Bonin forearcs were analyzed for mineral composition byX-ray diffraction and forchemical composition byX-ray fluorescence. The silt fraction of the muds consists predominantly of chrysotile, brucite, and ample amo...
Gespeichert in:
| Hauptverfasser: | , |
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| Dokumenttyp: | Article (Journal) |
| Sprache: | Englisch |
| Veröffentlicht: |
1992
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| In: |
ODP proceedings. Scientific results
Year: 1992, Jahrgang: 125, Pages: 313-323 |
| ISSN: | 1096-7451 |
| DOI: | 10.2973/odp.proc.sr.125.176.1992 |
| Online-Zugang: | Verlag, lizenzpflichtig, Volltext: http://www-odp.tamu.edu/publications/125_SR/125TOC.HTM Verlag: https://dx.doi.org/10.2973/odp.proc.sr.125.176.1992 
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| Verfasserangaben: | Dietrich Heling and Alexander Schwarz |
MARC
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| 520 | |a The <63-µm fractions of serpentinite muds from two seamounts on the Mariana and Izu-Bonin forearcs were analyzed for mineral composition byX-ray diffraction and forchemical composition byX-ray fluorescence. The silt fraction of the muds consists predominantly of chrysotile, brucite, and ample amorphous constituents. Chlorite and smectite are less abundant components. | ||
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