Yuan Wei, Liu Guang-di, Luo Wen-bin, Li Chao-zheng, Xu Li-ming, Niu Xiao-bing, Ai Jia-yi . Species and formation mechanism of apatites in the 7^th member of Yanchang Formation organic-rich shale of Ordos Basin,China[J]. Natural Gas Geoscience, 2016 , 27(8) : 1399 -1408 . DOI: 10.11764/j.issn.1672-1926.2016.08.1399

[1]Liu Yu.Mineralogical Spectroscopy of Apatites[D].Guangzhou:Sun Yat-sen University,2006.[刘羽.磷灰石的矿物谱学研究[D].广州:中山大学,2006.]
[2]Liu Kuiwu.The evolution of apatite minerals in the diagenetic processes[J].Acta Geologica Sinica,1989,63(4):310-321.[刘魁梧.成岩作用中磷灰石矿物的演变[J].地质学报,1989,63(4):310-321.]
[3]Qin Yan,Zhang Wenzheng,Peng Ping’an,et al.Occurrence and concentration of uranium in the hydrocarbon source rocks of Chang 7 member of Yanchang Formation,Ordos Basin[J].Acta Petrologica Sinica,2009,25(10):2469-2476.[秦艳,张文正,彭平安,等.鄂尔多斯盆地延长组长7段富铀烃源岩的铀赋存状态与富集机理[J].岩石学报,2009,25(10):2469-2476.]
[4]Zhang Benhao,Wu Bailin,Liu Chiyang,et al.Occurrence of uranium in hydrocarbon of Chang 7 member of Yanchang Formation of Ordos Basin[J].Northwestern Geology,2011,44(2):124-130.[张本浩,吴柏林,刘池阳,等.鄂尔多斯盆地延长组长7富铀烃源岩铀的赋存状态[J].西北地质,2011,44(2):124-130.]
[5]Yang Hua,Zhang Wenzheng.Leading effect of the seventh member high-quality source rock of Yanchang Formation in Ordos Basin during the enrichment of low-penetrating oil-gas accumulation:Geology and geochemistry[J].Geochemica,2005,34(2):147-153.[杨华,张文正.论鄂尔多斯盆地长7段优质油源岩在低渗透油气成藏富集中的主导作用:地质地球化学特征[J].地球化学,2005,34(2):147-153.]
[6]Chen Anqing,Chen Hongde,Hou Mingcai,et al.The middle-late Triassic event sediments in Ordos Basin:Indicators for episode I of the Indosinian movement[J].Acta Geologica Sinica,2011,85(10):1681-1689.[陈安清,陈洪德,侯明才,等.鄂尔多斯盆地中—晚三叠世事件沉积对印支运动Ⅰ幕的指示[J].地质学报,2011,85(10):1681-1689.]
[7]Deng Xiuqin,Li Wenhou,Liu Xinshe,et al.Discussion on the stratigraphic boundary between Middle Triassic and Upper Triassic[J].Acta Geologica Sinica,2009,83(8):1089-1095.[邓秀芹,李文厚,刘新社,等.鄂尔多斯盆地中三叠统与上三叠统地层界线讨论[J].地质学报,2009,83(8):1089-1095.]
[8]Xia Qingsong,Tian Jingchun,Huang Changwu.Study on the recognition marks of seismites in Upper Triassic Yanchang Formation Ordos Basin,China[J].Journal of Chengdu University of Technology:Science & Technology Edition,2007,34(3):312-316.[夏青松,田景春,黄昌武.鄂尔多斯盆地上三叠统延长组震积岩识别标志研究[J].成都理工大学学报:自然科学版,2007,34(3):312-316.]
[9]Xia Qingsong,Tian Jingchun.Characteristics and geological significance of Seismites of the Yanchang Formation,Upper triassic,Ordos Basin[J].Acta Sedimentologica Sinica,2007,25(2):246-252.[夏青松,田景春.鄂尔多斯盆地南部上三叠统延长组震积岩的发现及地质意义[J].沉积学报,2007,25(2):246-252.]
[10]Li Yuanhao,Liu Chiyang,Wang Xiujuan.Discovery and significance of seismites in Late Triassic Yanchang Formation of Ordos Basin[J].Acta Sedimentologica Sinica,2008,26(5):772-778.[李元昊,刘池洋,王秀娟.鄂尔多斯盆地三叠系延长组震积岩特征研究[J].沉积学报,2008,26(5):772-778.]
[11]Yang Hua,Dou Weitan,Liu Xianyang,et al.Analysis on sedimentary facies of member 7 in Yanchang Formation of Triassic in Ordos Basin[J].Acta Sedimentologica Sinica,2010,28(2):254-262.[杨华,窦伟坦,刘显阳,等.鄂尔多斯盆地三叠系延长组长7沉积相分析[J].沉积学报,2010,28(2):254-262.]
[12]Qin Xinwei.Characteristics and Dynamic Settings of Yanchang Period Hydrocarbon-rich Depression in Ordos Basin,China[D].Xi’an:Northwestern University,2011.[邱欣卫.鄂尔多斯盆地延长期富烃凹陷特征及其形成的动力学环境[D].西安:西北大学,2011.]
[13]Qiu Xinwei,Liu Chiyang,Li Yuanhao,et al.Distribution characteristics and geological significances of tuff interlayers in Yangchang Formation of Ordos Basin[J].Acta Sedimentologica Sinica,2009,27(6):1138-1145.[邱欣卫,刘池洋,李元昊,等.鄂尔多斯盆地延长组凝灰岩夹层展布特征及其地质意义[J].沉积学报,2009,27(6):1138-1145.]
[14]Qiu Xinwei,Liu Chiyang,Mao Guangzhou,et al.Enrichment feature of thorium element in tuff interlayers of Upper Triassic Yangchang Formation in Ordos Basin,China[J].Geological Bulletin of China,2010,29(8):1185-1191.[邱欣卫,刘池洋,毛光周,等.鄂尔多斯盆地上三叠统延长组凝灰岩夹层Th元素的富集特征[J].地质通报,2010,29(8):1185-1191.]
[15]Zhang Wenzheng,Yang Hua,Peng Ping’an,et al.The influence of late Triassic volcanism on the development of Chang 7 high grade hydrocarbon source rock in Ordos Basin[J].Geochemica,2009,38(6):573-582.[张文正,杨华,彭平安,等.晚三叠世火山活动对鄂尔多斯盆地长7优质烃源岩发育的影响[J].地球化学,2009,38(6):573-582.]
[16]Zhang Wenzheng,Yan Hua,Xie Liqin,et al.Lake-bottom hydrothermal activities and their influences on the high-quality source rock development:A case from Chang 7 source rocks in Ordos Basin[J].Petroleum Exploration and Development,2010,37(4):424-428.[张文正,杨华,解丽琴,等.湖底热水活动及其对优质烃源岩发育的影响-以鄂尔多斯盆地长7烃源岩为例[J].石油勘探与开发,2010,37(4):424-428.]
[17]Yang Hua,Deng Xiuqin.Deposition of Yanchang Formation deep-water sandstone under the control of tectonic events Ordos Basin[J].Petroleum Exploration and Development,2013,40(5):513-520.[杨华,邓秀芹.构造事件对鄂尔多斯盆地延长组深水砂岩沉积的影响[J].石油勘探与开发,2013,40(5):513-520.]
[18]Liu Xuan,Gui Xiaojun,Ding Xiaoqi,et al.Coupling research of event deposition and Qinling orogesis of Late Triassic,south Ordos Basin[J].Journal of Northeast Petroleum University,2014,38(4):59-66.[刘璇,桂小军,丁晓琪,等.鄂尔多斯盆地南部晚三叠世事件沉积_秦岭造山耦合分析[J].东北石油大学学报,2014,38(4):59-66.]
[19]Han Peng,Feng Shengbin,Li Xuemei,et al.Geological evidence of “the Archaic Uplift” of  late Triassic in western margin of Ordos Basin and identification of original boundary in the west of Ordos Basin[J].Journal of Oil and Gas Technology,2014,36(3):1-5.[韩鹏,冯胜斌,李雪梅,等.鄂尔多斯盆地西缘晚三叠世“古脊梁”隆升地质证据及盆地原型西部边界的确定[J].石油天然气学报,2014,36(3):1-5.]
[20]Dong Ye.Genetic theory evolution and development trend of marine phosphate rock[J].Chemical Geology,1992,14(3):3-7.[东野脉兴.海相磷块岩成因理论的沿革与发展趋势[J].化工地质,1992,14(3):3-7.]
[21]Wu Xianghe.A model for marine phosphate circulation late Precambrian in Guizhou[J].Guizhou Geology,1996,13(2):172-176.[吴祥和.贵州晚前寒武世海相磷酸盐循环模式[J].贵州地质,1996,13(2):172-176.]
[22]Smith M A,White M.Observations on lakes near Mount St.Helens:Phytoplankton[J].J.Arch.Hydrobiol.,1985,104(3):345-363.
[23]Risacher F,Alonso H.Geochemistry of ash leachates from the 1993 Lascar eruption,northern Chile.Implication for recycling of ancient evaporates[J].Journal of Volcanology and Geothermal Research,2001,109(4):319-337.
[24]Jones M T,Gislason S R.Rapid releases of metal salts and nutrients following the deposition of volcanic ash into aqueous environments[J].Geochim.Cosmochim.Acta,2008,72(15):3661-3680.
[25]Bia G,Borgnino L,Gaiero D,et al.Arsenic-bearing phases in South Andean volcanic ashes:Implications for As mobility in aquatic environments[J].Chemical Geology,2015,(393/394):26-35.
[26]Gromet L P,Dymek R F,Haskin L A,et al.The ‘North America shale composite’:Its compilation,major and trace element characteristic[J].Geochimica et Cosmochimica Acta,1984,48(12):2469-2482.
[27]Yang Binhu,Ba Haiqiang,Dai Yaquan,et al.Provenance and depositional systems during the depositional period of interval 8 of Upper Triassic Yangchang Formation in Qingyang area,Ordos Basin[J].Journal of Palaeogeography,2008,10(3):251-258.[杨斌虎,白海强,戴亚权,等.鄂尔多斯盆地庆阳地区晚三叠世延长期长8沉积期物源与沉积体系研究[J].古地理学报,2008,10(3):251-258.]
[28]Chen Meng’e,Liu Kuiwu.The geological significance of newly discovered microfossils form the Upper Sinian(Doushantuo age)phosphorites[J].Acta Geologica Sinica,1986,21(1):46-52.[陈孟莪,刘魁梧.晚震旦世陡山沱期磷块岩中微体化石的发现及其地质意义[J].地质科学,1986,21(1):46-52.]
[29]Chen Qiying.The biological effect in the process of sedimentary mineralization[J].Advances in Earth Science,1990,5(3):12-14.[陈其英.沉积成矿过程中的生物作用[J].地球科学进展,1990,5(3):12-14.]
[30]Chen Qiying.Microbiological processes in genesis of phosphorite deposits[J].Acta Geologica Sinica,1995,30(2):153-157.[陈其英.磷块岩形成过程中的生物作用[J].地质科学,1995,30(2):153-157.]
[31]Chen Qiying,Chen Meng’e,Li Juying.Microbial organic affection formation of the sedimentary apatite[J].Acta Geologica Sinica,2000,35(3):316-324.[陈其英,陈孟莪,李菊英.沉积磷灰石形成中的生物有机质因素[J].地质科学,2000,35(3):316-324.]