The evolution of crystal‐poor rhyolite in the middle Okinawa Trough and its implications for the state of magma chamber
Xinyu Luo,
Zhigang Zeng,
Zuxing Chen
et al.
Abstract:The crystal‐poor rhyolitic pumice is the product of extreme magma differentiation and is characterized by highly vesicular, honeycomb‐like structure. However, little is known about the evolutionary history and the time of volatile saturation of the pumice‐forming melt. A crystal‐poor rhyolitic pumice (TVG7‐1) has been collected from the Yoron Hole hydrothermal field in the middle Okinawa Trough, a young continental margin back‐arc basin in the western Pacific. This study conducted a detailed analysis on the te… Show more
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