【摘 要】
：
A group of Rb-Sr ages, i.e. plagioclase-whole rock (WR) isochron age of (205±7) Ma,hornblende-WR isochron age of (164±10) Ma and biotite-WR isochron age of (
【出 处】
：
Chinese Science Bulletin
论文部分内容阅读
A group of Rb-Sr ages, i.e. plagioclase-whole rock (WR) isochron age of (205±7) Ma,hornblende-WR isochron age of (164±10) Ma and biotite-WR isochron age of (123.4±1.2)Ma, for one pyroxenite sample from Renjiawan in North Dabie Terrane (NDT) are reported. According to the closure temperature of 600℃ for plageoclase and 300℃ for biotite, the Renjiawan pyroxenite should intrude into the NDT before 205 Ma, and the younger Rb-Sr ages may reflect the cooling history of the intrusion or reset by the very strong Cretaceous thermal event in NDT.
A group of Rb-Sr ages, ie plagioclase-whole rock (WR) isochron age of (205 ± 7) Ma, hornblende-WR isochron age of (164 ± 10) Ma and biotite-WR isochron age of (123.4 ± 1.2) Ma, for one pyroxenite sample from Renjiawan in North Dabie Terrane (NDT) are reported. According to the closure temperature of 600 ° C for plageoclase and 300 ° C for biotite, the Renjiawan pyroxenite should intrude into the NDT before 205 Ma, and the younger Rb -Sr ages may reflect the cooling history of the intrusion or reset by the very strong Cretaceous thermal event in NDT.
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