邵世宁, 熊先孝. 中国硼矿主要矿集区及其资源潜力探讨[J]. 化工矿 产地质, 2010, 32(2): 70-72. Shao Longning, Xiong Xianxiao. The main boron ore concentration area and its resource potential in China[J]. Geology of Chemical Minerals, 2010, 32(2): 70-72.
[3]
徐凤银, 施俊, 张少云, 等. 柴达木盆地柴中断裂带演化及其对成盆作 用的控制[J]. 石油学报, 2009, 30(6): 803-808. Xu Fengyin, Shijun, Zhang Shaoyun, et al. Evolution of Qaizhong Fault and its effects on the basin formation in Qaidam Basin[J]. Acta Petrolei Sinica, 2009, 30(6): 803-808.
[4]
汪祖智. 柴达木盆地北东向构造线的分布及其在石油勘探上的意义[J]. 石油勘探与开发, 1984, 5: 9-15. Wang Zuzhi. The distribution of the north east tectonic line of Qaidam basin and its significance in oil exploration[J]. Petroleum Exploration and Development, 1984, 5: 9-15.
[5]
姜波, 徐凤银, 彭德华, 等. 柴达木盆地北缘断裂构造变形特征[J]. 中 国矿业大学学报, 2004, 33(6): 687-692. Jiang Bo, Xu Fengyin, Peng Dehua, et al. Deformation Characteristics of Fault Structure on the Northern Fringe of Qaidam Basin[J]. Journal of China University of Mining & Technology, 2004, 33(6): 687-692.
[6]
青海省地质矿产局. 青海省区域地质志[M]. 北京: 地质出版社, 1991. Bureau of Geology and Mineral Resources of Qinghai Province. Regional geology of Qinghai province[M]. Beijing: Geological Publishing House, 1991.
[7]
申文环. 柴北缘塔塔楞环斑花岗岩体的特征及成因探讨[D]. 西安:长安大学, 2007. Shen Wenhuan. The characteristics and genesis of granite rock in the northern Qaidam basin[D]. Xi'an: Chang'an University, 2007.
[8]
卢新祥, 孙廷贵, 张雪亭, 等. 柴达木盆地北缘塔塔楞环斑花岗岩的 SHRIMP年龄[J]. 地质学报, 2007, 81(5): 626-632. Lu Xinxiang, Sun Tinggui, Zhang Xueting, et al. The SHRIMP age of granite in Tataleng river of Northern Qaidam basin[J]. Acta Geologica Sinica, 2007, 81(5): 626-632.
[9]
马宇峰. 青海省雅沙图西部地区硼矿地质普查初步报告[R]. 西宁: 中国科学院柴达木盐湖科学调查队,地质部矿物原料研究所, 1960. Ma Yufeng. The preliminary report on boron ore geology survey in the western region of Yashatu area, Qinghai province[R]. Xining: Qaidam Salt Lake Science, Chinese Academy of Sciences Survey Team, Institute of the Geological Mineral Materials Research, 1960.
[10]
Fournier R O. The behavior of silica in hydrothermal solutions[J]. Review of Economic Geology, 1985, 2: 45-59.
[11]
Sun D P. Origin of the Borate Deposits under the Condition of Hypergenesi[J]. Journal of Salt-lake Research, 2002, 10(1): 46-58.
[12]
Craig H. The measurement of oxygen isotope paleotemperatures[M]// Tongiorgi E. Stable Isotopes in Oceanographic Studies and Paleotemperature. Pisa:VLishi E F, 1965: 9-130.
[13]
郑绵平, 向军. 青藏高原盐湖[M]. 北京: 科学出版社, 1989: 61-329. Zheng Mianping, Xiangjun. Salt lakes of Tibet plateau[M]. Beijing: Science Press, 1989: 61-329
[14]
郑绵平, 张雪飞, 侯献华, 等. 青藏高原晚新生代湖泊地质环境与成盐 成藏作用[J]. 地球学报, 2013, 34(2): 129-138. Zheng Mianping, Zhang Xuefei, Hou Xianhua, et al. Geological environments of the late cenozoic lakes and salt-forming and oil-gas pool- forming actions in the Tibetan Plateau[J]. Acta Geoscientica Sinica, 2013, 34(2): 129-138.
郑绵平, 王秋霞, 多吉, 等. 水热成矿新类型—西藏铯硅华矿床[M]. 北 京: 地质出版社. 1995: 14-26. Zheng Mianping, Wang Qiuxia, Duo Ji, et al. A new hydrothermal mineralization type—Tibet cesium sinter ore deposit[M] . Beijing: Geological Publishing House, 1995: 14-26.
[17]
杨谦. 柴达木盆地硼矿[J]. 沉积学报, 1989, 7(2): 117-122. Yang Qian. Boron ore of Qaidam basin[J]. Acta Sedimentologica Sinica, 1989, 7(2): 117-122.
[18]
周澄伟. 雅沙图居红土硼矿矿区地质勘探总结报告[R]. 海西: 青海 柴达木地质队, 1959. Zhou Chengwei. The geological exploration and summary report of Juhongtu boron ore in Yashatu district[R]. Haixi: Qinghai chaidamu geological team, 1959.
[19]
马宇峰. 青海省德令哈县雅沙图614矿物探工作结果报告[R]. 北京: 中国地质科学院矿物原料研究所, 1961. Ma Yufeng. The geophysical work report of the 614 boron ore in Yashatu district of De Lingha, Qinghai province[R]. Beijing: Geological Institute of Mineral Rraw Materials, 1961.
[20]
朱镜清. 青海省德令哈市居红土硼矿点及外围普查报告[R]. 西宁: 青海省地矿局第六地质队, 1991. Zhu Jingqing. The geological report in Juhongtu boron mines and peripheral census of De Lingha, Qinghai province[R]. Xining: The Sixth Geological Team Mine Bureau in Qinghai Province ,1991.
[21]
邱盛南, 李衍霖. 青海某地硼酸盐矿床的探讨[J]. 青海地质, 1979(1): 55-64. Qiu Shengnan, Li Yanlin. The discussion of the borate ore somewhere of Qinghai[J]. Qinghai Geology, 1979(1): 55-64.
[22]
刘铮, 唐丽华, 朱其清, 等. 我国主要土壤中微量元素的含量与分布 初步总结[J]. 土壤学报, 1978, 15(2): 138-141. Liu Zheng, Tang Lihua, Zhu Qiqing, et al. The preliminary summary of the distribution and content of trace elements in soil[J]. Acta Pedologica Sinica, 1978, 15(2): 138-141.
[23]
张天乐, 王宗良, 胡云中. 腾冲现代热泉系统硅华的矿物学特征及其 地质意义[J]. 岩石矿物学杂志, 1997, 16(2): 170-178. Zhang Tianle, Wang Zongliang, Hu Yunzhong. The mineralogical characteristics and geological significance of sinter inTengchong hot springs modern system[J]. Acta Petrologica & Mineralogica, 1997, 16 (2): 170-178.
[24]
Williams L A, Crerar D A. Silica digenesis: II. General mechanisms[J]. Sediment Petrol, 1985, 55: 312-321.
[25]
许靖华, 何起祥, 吴应林, 等. 我国西南早中三叠时间"绿豆岩"等时 面上下的碳、氧稳定同位素地球化学[J]. 中国地质科学院成都地质 矿产研究所所刊, 1983, 4: 4. Xu Jinghua, He Qixiang, Wu Yinglin, et al. Carbon and oxygen stable isotopic geochemistry of the "mung bean rock" in the early Triassic time , southwest China[J]. Institute of Mineral Resources, Chinese Academy of Geological Sciences, 1983, 4: 4.
KeithMH,WeberJN.Isotopiccompositionandenvironment classification of selected limestone and fossils[J]. Geochimica Cosmochimica Acta, 1964, 28: 1787-1816
[28]
邵龙义. 碳酸盐岩氧、碳同位素与古温度等的关系[J]. 中国矿业大学 学报, 1994, 23(1): 39-42. Shao Longyi.The relationship between Carbonate oxygen, carbon isotopes, and paleotemperature[J]. Journal of China University of Mining & Technology, 1994, 23(1): 39-42.
[29]
高春亮, 余俊清, 展大鹏, 等. 柴达木盆地盐湖硼矿资源的形成和分 布特征[J]. 盐湖研究, 2009, 17(4): 6-12. Gao Chunliang, Yu Junqing, Zhan Dapeng, et al. The formation and distribution characteristics of salt lake boron ore resources, Qaidam basin[J]. Salt Lake Research, 2009, 17(4): 6-12.
[30]
肖应凯, Shirodkar P V, 刘卫国, 等. 青海柴达木盆地盐湖硼同位素 地球化学研究[J]. 自然科学进展. 1999, 9(7): 612-618. Xiao Yingkai, Shirodkar P V, Liu Weiguo, et al. The boron isotope geochemical studyof salt lakes in Qaidam basin, Qinghai[J]. Progress in Natural Science, 1999, 9(7): 612-618.
[31]
Vengosh A, Kolodny Y, Starinsky A, et al. Coprecipitation and isotopic fractionation of boron in modern biogenic carbonates[J]. Geochemical Cosmochimica Acta, 1991, 55: 2591-2606.