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The Miba granite is located in the juncture of Kang County in eastern Gansu Provinceand Lueyang County in Shanxi Province. It is considered to be the post-orogenic granite(POG-type) by major element discrimination method of Maniar. ~40Ar/~39Ar dating indicates that itsemplacement time is about 240-230 Ma and it is the result of the Indo-Sinian magmatism. In theearly Yanshan period (about 193.8 Ma), a thermal event resulted in the partial opening of the ar-gon isotope system of the biotite.
The Miba granite is located in the juncture of Kang County in eastern Gansu Province and Lueyang County in Shanxi Province. It is considered to be the post-orogenic granite (POG-type) by major element discrimination method of Maniar. ~ 40Ar / ~ 39Arly dating indicates that itsemplacement time is about 240-230 Ma and it is the result of the Indo-Sinian magmatism. In the early Yanshan period (about 193.8 Ma), a thermal event resulted in the partial opening of the ar-gon isotope system of the biotite .