It intruded in Upper Ordovician Shifeng Formation and is dated as 333 86Ma of U Pb concordant age of zircon, which belongs to middle stage of Variscan.

 
  • 巖體侵入上奧陶統石縫組(O3s) , 巖體的鋯石U?Pb 一致線(xiàn)年齡333-86 Ma, 屬華力西中期。
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