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Tao Chunhui

Evolution of enhanced magmatism at the ultraslow spreading Southwest Indian Ridge between 46°E and 53.5°E
780 thousand years of upper-crustal construction at a melt-rich segment of the ultraslow spreading Southwest Indian Ridge 50°28'E
Enhanced hydrothermal activity on an ultraslow-spreading supersegment with a seismically detected melting anomaly
Newly discovered hydrothermal fields along the ultraslow-spreading Southwest Indian Ridge around 63°E

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