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瓮安生物群中“内陷式动物原肠胚化石”的同步辐射无损成像及其亲缘关系的重新解释
  • ISSN号：1000-7857
  • 期刊名称：《科技导报》
  • 时间：0
  • 分类：P618.51[天文地球—矿床学;天文地球—地质学]
  • 作者机构：[1]现代古生物学与地层学国家重点实验室,中国科学院南京地质古生物研究所,南京210008, [2]南京大学地球科学与工程学院,内生金属矿床成矿机制研究国家重点实验室,南京210093, [3]江苏省地质矿产调查研究所,南京210016, [4]有色金属华东地质勘查局,南京210007
  • 相关基金：本文受国家自然科学基金（批准号：40703018;J0930006）,中国博士后基金（No.20070411040）,江苏省博士后基金（项目编号0701012C）,南京大学内生金属矿床成矿机制研究国家重点实验室开放基金（项目编号14-08-15）和中国科学院南京地质古生物研究所现代古生物学与地层学国家重点实验室开放基金（No.073108）的共同资助. 致谢在金坛盐矿采样期间,得到中盐金坛盐化有限责任公司金坛盐矿矿长徐孜俊等同志的帮助,在此表示诚挚的感谢.
作者： 殷宗军[1], 朱茂炎[1]
关键词： 包裹体, 低温冷冻扫描电镜-能谱法, MG/CA, 金坛盐矿, 江苏, fluid inclusion, Cryo-SEM-EDS, Mg/Ca, Jintan Salt Mine, Jiangsu Province
中文摘要：

我国白垩纪晚期—古近纪由于燕山运动和喜马拉雅运动,形成了一系列的断陷盆地,金坛盐矿就是该时期始新世中晚期的盐湖沉积。本次研究首次在国内半定量的进行了石盐原生包裹体的分析,发现其中Ca2＋缺失而富含SO42-,原始卤水成分为Na-Mg-K-Ca-Cl-SO4体系。

英文摘要：

During the late Cretaceous-Tertiary,a series of fault basins were formed because of Yanshanian orogeny and Himalayan orogeny.Jintan Salt Mine is a middle-late Eocene salt lake deposits.In this paper,we reconstruct for the first time in China the chemistry composition of ancient brine using the primary fluid inclusions in halite.The brine in fluid inclusions has little Ca2＋ but abundant SO42-,which suggests the ancient salt lake is a Na-Mg-K-Ca-Cl-SO4 system.

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期刊信息
  • 《科技导报》
  • 北大核心期刊（2011版）
  • 主管单位:中国科学技术协会
  • 主办单位:中国科学技术协会
  • 主编：项昌乐
  • 地址：北京市海淀区学院南路86号科技导报社
  • 邮编：100081
  • 邮箱：kjdbbjb@cast.org.cn
  • 电话：010-62138113
  • 国际标准刊号：ISSN：1000-7857
  • 国内统一刊号：ISSN：11-1421/N
  • 邮发代号:2-872
  • 获奖情况:
  • 国内外数据库收录:
  • 俄罗斯文摘杂志,美国化学文摘（网络版）,英国农业与生物科学研究中心文摘,波兰哥白尼索引,美国乌利希期刊指南,美国剑桥科学文摘,英国科学文摘数据库,中国中国科技核心期刊,中国北大核心期刊（2008版）,中国北大核心期刊（2011版）,中国北大核心期刊（2014版）
  • 被引量:24858