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The boundary between the Central Asian Orogenic belt and Tethyan tectonic domain deduced from Pb isotopic data
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文摘

An isotopic boundary exists between the CAOB and TTD.

Distinctive 208Pb/206Pb isotopic compositions of the PAO and Tethys mantle domains.

Different long-time integrated Th/U evolution caused distinct PAO and Tethys mantle.

Different magma–tectonic processes formed the CAOB and TTD.

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