Permian dyke swarm with bimodal affinity from the Hegenshan ophiolite-arc-accretionary belt, central Inner Mongolia: implications on lithospheric extension in a Carboniferous continental arc
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Supplementary Table 1. Trace elements of zircons from the dyke swarm.
Supplementary Table 2. U-Pb isotopic ages of zircons from the dyke swarm.
Supplementary Table 3. Major-trace elements of the dyke swarm.
Supplementary Table 4. Sr-Nd-Pb isotopic compositions of the granite porphyry-rhyolite dykes.
创建时间：
2020-03-31
