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The LA-ICPMS zircon U-Pb geochronology of three typically Indosinian granitic plutons yielded weighted mean 206Pb/238U ages of 214.1±5.9 Ma and 210.3±4.7 Ma for the biotite monzonitic granites from the Xiema and Xiangzikou plutons in Hunan Province,and 205.3±1.6 Ma for biotite granite from the Napeng pluton,western Guandong Province,respectively,showing a similar late Indosinian age of crystallization.In combination with other geochronological data from Indosinian granites within the South China Block(SCB),it is proposed that those late Indosinian granites with an age of ~210 Ma and the early Indosinian granites(230-245 Ma)have the similar petrogenesis in identical tectonic setting.The Indosinian granites within the SCB might be the products of anatexis of the thickening crust in a compressive regime.These data provide a further understanding for the temporal and spatial distribution of the Indosinian granites and the dynamic evolution of the SCB.
The LA-ICPMS zircon U-Pb geochronology of three typically Indosinian granitic plutons yielded a weighted mean 206 Pb / 238 ages of 214.1 ± 5.9 Ma and 210.3 ± 4.7 Ma for the biotite monzonitic granites from the Xiema and Xiangzikou plutons in Hunan Province, and 205.3 ± 1.6 Ma for biotite granite from the Napeng pluton, western Guandong Province, respectively, showing a similar late Indosinian age of crystallization. In combination with other geochronological data from Indosinian granites within the South China Block (SCB), it is proposed that those late Indosinian The granites with an age of ~ 210 Ma and the early Indosinian granites (230-245 Ma) have the similar petrogenesis in identical tectonic setting. The Indosinian granites within the SCB might be the products of anatexis of the thickening crust in a compressive regime. data provide a further understanding for the temporal and spatial distribution of the Indosinian granites and the dynamic evolution of the SCB.