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The Luobusa Ophiolite, Southern Tibet, lies in the eastern portion of Indus–Yarlung Zangbo suture zone that separates Eurasia from the Indian continent. An aeromagnetic reconnaissance survey has revealed an EW-trending Yarlung Zangbo River aeromagnetic anomaly zone, and it is considered to be caused mainly by the Indus–Yarlung Zangbo Ophiolite. The Luobusa Ophiolite reflects the eastern portion of...
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