Fig. 3From: Sr isotopic ratios of hydrothermal fluids from the Okinawa Trough and the implications of variation in fluid–sediment interactionsRelationship between Mg/Sr and 87Sr/86Sr in hydrothermal fluids from the Iheya North Knoll, HAKUREI, JADE, Hatoma Knoll, and Yonaguni Knoll IV sites in the Okinawa Trough. For an explanation of insets, refer to Fig. 2Back to article page