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
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.