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Post-collisional adakitic rocks (26–9Ma) have been recognized in southern Tibet for almost 20years; however, their origins and geodynamics remain highly controversial. This paper reports geochronological and geochemical data for the Lasa intrusion exposed in the Zhongba terrane and proposes implications for the origins of the Miocene adakitic rocks in southern Tibet. The Lasa intrusion consists of...
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