Phase relations of a serpentine composition between 5 and 14 GPa: significance of clinohumite and phase E as water carriers into the transition zone

Roland Stalder; Peter Ulmer

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Phase relations of a serpentine composition between 5 and 14 GPa: significance of clinohumite and phase E as water carriers into the transition zone

机译：蛇纹石成分在5至14 GPa之间的相位关系：斜长石和E相作为水进入过渡区的水载体的意义

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《Contributions to Mineralogy and Petrology》 |2001年第6期|1-1|共1页
作者
Roland Stalder; Peter Ulmer;
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Institut für Mineralogie Petrographie Sonneggstrasse 5 ETH Zentrum 8092 Zürich Switzerland;

Institut für Mineralogie Petrographie Sonneggstrasse 5 ETH Zentrum 8092 Zürich Switzerland;

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1. Phase relations of a serpentine composition between 5 and 14 GPa: significance of clinohumite and phase E as water carriers into the transition zone [J] . Roland Stalder, Peter Ulmer Contributions to Mineralogy and Petrology . 2001,第6期

机译：蛇纹石成分在5和14 GPa之间的相位关系：斜长石和E相作为水进入过渡区的水载体的意义
2. Phase relations of a serpentine composition between 5 and 14 GPa: significance of clinohumite and phase E as water carriers into the transition zone [J] . Roland Stalder, Peter Ulmer Contributions to Mineralogy and Petrology . 2001,第6期

机译：蛇纹石成分在5至14 GPa之间的相位关系：斜长石和E相作为水进入过渡区的水载体的意义
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Phase relations of a serpentine composition between 5 and 14 GPa: significance of clinohumite and phase E as water carriers into the transition zone

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