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《Geochimica》 1982-04
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A DISCUSSION ON THE AGE DIVISION OF THE MESOZOIC GRANITES IN WESTERN QINLING RANGE

Tao Bingkun  
Based on geological observation and isotopic age data, a continuous cycle of granite intrusion from Early-Middle Triassic to Cretaceous has been demonstrated for the Mesozoic granitic bodies in western Qinling Range. Six periods can be further recognized within this cycle, i.e., (I) Early-Middle Triassic (240-205my); (II) Late Triassic (205-185 my) ; (III) Early Jurassic (185-170 my); (IV) Middle-Late Jurassic (170-140 my); (V) Early Cretaceous (140-100 my); and (VI) Late Cretaceous (100-70 my).
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