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40K-40Ca法的初步研究

A preliminary study on dating and tracing of the 40K-40Ca system

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【作者】 王俊新彭子成刘桂建房明惠桂和荣

【Author】 WANG Junxin1,2 PENG Zicheng1,2 LIU Guijian1 Fang Minghui 1 Gui Herong1 1 (Department of Earth and Space Science, University of Science and Technology of China, Hefei 230026) 2 (State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS, Xian, 710054)

【机构】 中国科学技术大学地球和空间科学系,中国科学技术大学地球和空间科学系,中国科学技术大学地球和空间科学系,中国科学技术大学地球和空间科学系,中国科学技术大学地球和空间科学系 合肥230026中国科学院地球环境研究所黄土与第四纪国家重点实验室,西安710054,合肥230026中国科学院地球环境研究所黄土与第四纪国家重点实验室,西安710054,合肥230026,合肥230026,合肥230026

【摘要】 报道了样品中钾、钙化学分离和纯化,以及质谱测定流程的建立。测试了国家球团矿标样W7220和W7107、国家40K-40Ar法标准矿物黑云母(ZBH-25)和角闪石(ZBJ)的钾钙含量,以及国际二级钙标样Tachiti和国家钾含量标样的钙和钾同位素比值。实测结果与相应的标称值在误差范围内一致。在此基础上,用实验所得的两组黑云母和角闪石的(40Ca/42Ca) 和 (40K/42Ca)数据,构筑了40K-40Ca法等时线年龄为(133.532.1)Ma, 此与标称值年龄132.7Ma在误差范围内一致。而所得的初始值(40Ca/42Ca)i为151.4160.003, 相应的xCa 值为+26.5,示踪了该矿物组合的原岩具有陆源性质,为固体地球化学的研究提出了新的判据。

【Abstract】 The K and Ca contents in the national standards of pellets (W7220, W7107), biotite (ZBH-25) and hornblende (ZBJ), as well as, the K and Ca isotopic ratios of the national K standard and an international standard (Tachiti) have been determined by using mass spectrometry and atomic absorption spectrometry . The measured results are in agreement with the standard values within a reasonable error range. On the basis of the standard measurement, the slope of the regressive line between (40K/42Ca) and (40Ca/42Ca) data is equal to 0.068730.01732, corresponding to the age of (133.532.1)Ma, which is consistent with the 132.7Ma in the error range reported by using the 40K-40Ar method. The primitive ratio (40Ca/42Ca)i deduced from the isochrone is 151.4160.003, corresponding to +26.5 of the xCa value. It means that the original rock of the biotite and hornblende minerals appears in the terrestrial behavior.

【基金】 国家自然科学基金项目(49973011);科技部973项目(G1999043401);中国科学院创新工程项目(KZCX2-SW-118);中国科学技术大学资源与环境基地项目资助
  • 【分类号】P597
  • 【下载频次】103
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