Study on C14 Age of Dawengquan Volcano in Longgang Volcano Area
Longgang volcano area is one of the typical monogenetic volcanic fields of Quaternary in China (Wei et al., 1999). Volcanic activities started in Neogene, and got its peak in Pleistocene (Fan et al., 2002; Bai et al., 2006). In AD 460, there was a basaltic explosive eruption (Liu et al., 2009). There are many Maar volcanoes and base-surge deposits, such as Dalongwan (DALW), Erlongwan (ELW), Sanjiaolongwan (SJLW), Sihailongwan (SHLW), Nanlongwan (NLW), Donglongwan (DLW), Longquanlongwan (LQLW), and Dawengquan (DWQ). This paper mainly presents our study of strata and chronology in DWQ volcano.
Dawengquan Maar volcano C14 age Longgang volcano area
Bo Zhao Zhida Bai Debin Xu Hongmei Yu Jiandong Xu Bo Pan
Institute of Geology, China Earthquake Administration, Beijing, China China University of Geoscience, Beijing, China
国际会议
The 6th International Maar Conference(IMC)(第六届国际玛珥会议)
长春
英文
119-119
2016-07-30(万方平台首次上网日期,不代表论文的发表时间)