极地研究 ›› 1997, Vol. 8 ›› Issue (2-English): 89-95.
Zheng Xiangshen1, Hu Shiling1, Liu Jiaqi1 and Francesc Sàbat2
Zheng Xiangshen1, Hu Shiling1, Liu Jiaqi1 and Francesc Sàbat2
摘要:
The age of the volcanic rocks of the Mount Bowles Formation (MBF) on the eastern part of Livingston Island, South Shetland Islands, Antarctica is redetermined by using 40Ar/39Ar and laser microarea isochron age dating method with a continuous laser system and mass spectrometer. The isochron ages of an andesite sample and a basaltic andesite sample are (105.62±2.11) Ma and (111.48±2.23) Ma with the 40Ar/39Ar initial ratios of 295.3 and 294.6 respectively, being almost the same as the atmospheric value, which proves that there exists no excess argon in these rocks. The 40Ar/39Ar plateau age of an aplite sample is (96.7±1.6) Ma and the calculated isochron age is 96.6 Ma, which indicates that the aplite occurred after lava eruption. These data suggest that the MBF volcanic rocks were formed during Cretaceous.