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The distribution, geochronology and geochemistry of early Paleozoic granitoid plutons in the North Altun orogenic belt, NW China: Implications for the petrogenesis and tectonic evolution
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文摘
Early Paleozoic intrusive rocks in the North Altun orogenic belt. Different melting P-T condition and source among these rocks in this area. Subduction angle change causes repeated transition from lithospheric extension to contraction.

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