汉中大佛洞宇宙成因核素~(26)Al/~(10)Be埋藏年龄
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  • 英文篇名:Cosmogenic nuclides ~(26)Al/~(10)Be burial ages of Dafo Cave in Hanzhong, Shaanxi, China
  • 作者:陈清敏 ; 张丽 ; 王喆 ; 罗乾周 ; 蔺新望 ; 张俊良 ; 任娟刚
  • 英文作者:CHEN Qingmin;ZHANG Li;WANG Zhe;LUO Qianzhou;LIN Xinwang;ZHANG Junliang;REN Juangang;Shaanxi Center of Geological Survey, Shaanxi Institute of Geological Survey;State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences;Shaanxi Key Laboratory of Accelerator Mass Spectrometry Technology and Application,Xi'an Accelerator Mass Spectrometry;
  • 关键词:大佛洞 ; 26Al/10Be ; 埋藏年龄 ; 侵蚀速率
  • 英文关键词:Dafo Cave;;26Al/10Be;;burial age;;erosion rate
  • 中文刊名:DQHJ
  • 英文刊名:Journal of Earth Environment
  • 机构:陕西省地质调查院陕西省地质调查中心;中国科学院地球环境研究所黄土与第四纪地质国家重点实验室;西安加速器质谱中心陕西省加速器质谱技术及应用重点实验室;
  • 出版日期:2018-02-15
  • 出版单位:地球环境学报
  • 年:2018
  • 期:v.9;No.46
  • 基金:陕西省公益性地勘专项项目(20170105);; 陕西省地勘基金(61201708317)~~
  • 语种:中文;
  • 页:DQHJ201801004
  • 页数:7
  • CN:01
  • ISSN:61-1482/X
  • 分类号:42-48
摘要
汉中天坑群是在我国湿润热带-亚热带岩溶地貌区北界首次发现的岩溶地质景观,已查明区内发育岩溶洞穴160余处,对研究中国南北方乃至全球古地理环境及气候变化具有重要科学价值。目前该区域地貌演化、岩溶洞穴发育研究刚刚起步,尚没有该岩溶区年代学研究成果报道。本文尝试运用加速器质谱仪(AMS)宇宙成因核素~(26)Al/~(10)Be埋藏年龄测试技术,对汉中南郑岩溶洞穴大佛洞内次生沉积石英砾石进行年龄测定,获得~(26)Al/~(10)Be埋藏年龄为(1.07±0.71)Ma,初步限定了汉中岩溶洞穴大佛洞的发育时期;同时获得大佛洞石英砾石样品在埋藏前该流域侵蚀速率为(156.5±73.4)m?Ma-1。
        Background, aim, and scope Hanzhongtiankeng is the karst geological landscape first discovered on the north margin of the moist tropical-subtropical karst landform area around north latitude 32° in China. There are more than 160 karst caves were surveyed and had important scientific value for Chinese and global paleoenvironment and paleoclimate research. But there have not any report on the chronology of the Hanzhong karst region until now. We purposed to determine the formation ages of karst caves in Hanzhong, China. Materials and methods The quartz gravel samples were collected from Dafo Cave in Hanzhong. Quartz purification and target preparation were carried out at Xi'an Accelerator Mass Spectrometry Center of the Institute of Earth Environment, Chinese Academy of Sciences. And then, the cosmogenic nuclides ~(26)Al/ and ~(10)Be concentrations were measured on 3 MV accelerator mass spectrometry. Results Totally 14.2257 g pure quartz was extracted from the quartz gravel samples from Dafo Cave. Finally, the cosmogenic nuclides 26Al and ~(10)Be concentrations were measured on accelerator mass spectrometry(AMS). And then, the cosmogenic nuclides 26Al/~(10)Be burial age of Dafo Cave and the erosion rate before the quartz gravel samples buried in Dafo Cave was calculated. Discussion The cosmogenic nuclides 26Al/~(10)Be burial age of Dafo Cave reflected that the karst cave in Hanzhong developed in Early Pleistocene probably. The warm and humid paleoclimate in the middle of Early Pleistocene provided necessary condition for the development of karst caves in Hanzhong. Conclusions We first report that the cosmogenic nuclides 26Al/~(10)Be burial age of quartz gravel in Dafo Cave in Hanzhong is(1.07 ± 0.71) Ma. The erosion rate before the quartz gravel samples buried in Dafo Cave is (156.5 ± 73.4) m ? Ma~(-1). Recommendations and perspectives This is a new exploration of dating on Hanzhong karst cave and very important to the research of local landscape evolution, karst evolution, paleoenvironment and paleoclimate. It also shows a well foreground in the geomorphic evolution and karst development research by AMS cosmogenic nuclides dating technology and method.
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