The water-undersaturated and dry Qz-Ab-Or system revisited. Experimental results at very low water activities and geological implications
Liquidus phase relations have been determined in the system Qz-Ab-Or-H2) at H2)-undersaturated conditions (melt water content of 1 wt% H2)) in the pressure range 200-800 MPA. Starting materials were homogeneous synthetic glasses containing 1 wt% H2).
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| Veröffentlicht in: | Contributions to mineralogy and petrology 2001-06, Vol.141 (3), p.347-357 |
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| container_end_page | 357 |
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| container_issue | 3 |
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| container_title | Contributions to mineralogy and petrology |
| container_volume | 141 |
| creator | Holtz, Francois |
| description | Liquidus phase relations have been determined in the system Qz-Ab-Or-H2) at H2)-undersaturated conditions (melt water content of 1 wt% H2)) in the pressure range 200-800 MPA. Starting materials were homogeneous synthetic glasses containing 1 wt% H2). |
| doi_str_mv | 10.1007/s004100100245 |
| format | Article |
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| identifier | ISSN: 0010-7999 |
| ispartof | Contributions to mineralogy and petrology, 2001-06, Vol.141 (3), p.347-357 |
| issn | 0010-7999 1432-0967 |
| language | eng |
| recordid | cdi_proquest_journals_208164339 |
| source | SpringerLink Journals (MCLS) |
| subjects | Fluid dynamics Geology Meltwater Mineralogy Petrology Temperature Water Water content |
| title | The water-undersaturated and dry Qz-Ab-Or system revisited. Experimental results at very low water activities and geological implications |
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