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![](./images/clear.gif) 1.- Stability of titanian clinohumite-olivine intergrowths in HFSE-enriched chlorite-harzburgite produced by high-pressure dehydration of antigorite-serpentinite and its potential implications for the origin of subduction signatures
American Geophysical Union; Washington, DC; USA; United States, 2005
AGU 2005 fall meeting
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