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- W2393638557 abstract "Xunwu broken crater located in the transition zone of Wuyi rise belt and Nanling tectonic belt,controlled by the NE direction Huichang-Xunwu fault belt and the EW direction Sannan-Xunwu fault belt,and developed a volcanic-intrusive rocks that made up of porphyroclastic lava and granite-porphyry.The zircon U-Pb dating with a higher accuracy yields the following results:the age of pyroclastic rocks in the volcanic-intrusive rocks in broken crater is(96.7±1.1)Ma and the age of granite-porphyry is(97.3±0.9)Ma.According to the geological chronology,the boundary between the Early Cretaceous and the Late Cretaceous is(99.6±0.9)Ma,the geological age of the volcanic-intrusive rocks of Xunwu broken crater is early Late Cretaceous.Age determinations of the volcanic-intrusive rocks provide the age evidence for Xunwu broken crater which belong to Yousheng formation." @default.
- W2393638557 created "2016-06-24" @default.
- W2393638557 creator A5038170876 @default.
- W2393638557 date "2011-01-01" @default.
- W2393638557 modified "2023-09-23" @default.
- W2393638557 title "The SHRIMP Zircon U-Pb Dating and Its Geologicai Significance on the Volcanic-intrusive Rocks in Broken Crater of Xunwu,Jiangxi Province" @default.
- W2393638557 hasPublicationYear "2011" @default.
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