[1]Xu Yajun,Du Yuansheng,Yang Jianghai.Prosepects of sediment provenance analysis[J].Geological Science and Technology Information,2007,26(3):26-32.[徐亚军,杜远生,杨江海.沉积物物源分析研究进展[J].地质科技情报,2007,26(3):26-32.]
[2]Yan Zhen,Fang Aimin,Pan Yusheng, et al. Detrital modal,geochemical characteristics and tectonic setting of Dajin marine clastic rocks,Tibet[J].Acta Petrologica Sincia,2006,22(4):949-960.[闫臻,方爱民,潘裕生,等.西藏达金海相碎屑岩的组成、地球化学特征及其构造背景[J].岩石学报,2006,22(4):949-960.]
[3]Bhatia M R.Plate tectonics and geochemical composition of sandstones[J].The Journal of Geology,1983,91(6):611-628.
[4]Bhatia M R.Rare earth elements geochemistry of Australian Paleozoic graywacks and mudstone:Provenance and tectonic control[J].Sedimentary Geology,1985,45:97-113.
[5]Roser,B P,Korsch R J.Plate tectonics and geochemical composition of sand-stones:A discussion[J].The Journal of Geology,1985,93:81-84.
[6]Bhatia M R,Crook K A.Trace-element characteristics of greywackes and tectonics setting discrimination of sedimentary basin[J].Contributions to Mineralogy and Petrollogy,1986,92:181-193.
[7]Roser B P,Korsch R J.Determination of tectonic setting of sandstone-mudstone suites using SiO2 content and K2O/Na2O ratio[J].The Journal of Geology,1986,94:635-650.
[8]McLennan S M,Taylor S R.Sedimentary rocks and crustal evolution:Tectonic setting and secular trends[J].The Journal of Geology,1991,99:1-21.
[9]Luo Yuan,Zhao Junxing,Lü Qiang, et al. Provenance analysis of Chang 6 formation in the Ningxian-Qingyang region,southwest Ordos Basin[J].Natural Gas Geoscience,2009,20(6):907-915.[罗媛,赵俊兴,吕强,等.鄂尔多斯盆地西南部宁县—庆阳地区长6期物源状况分析[J].天然气地球科学,2009,20(6):907-915.]
[10]Floyd P A,Winchester J A,Park R G.Geochemistry and tectonic setting of Lewisian clastic metasediments from the Early Proterozoic Loch Maree Group of Gairloch,N.W.Scotland[J].Precambrian Research,1989,45(1-3):203-214.
[11]Luo Jinglan,Li Zhongxing,Shi Cheng′en, et al. Depositional systems and provenance directions for the Chang 6 and Chang 8 reservoir groups of the Upper Triassic Yanchang Formation in the south western Ordos Basin,China[J].Geological Bulletin of China,2008,27(1):101- 111.[罗静兰,李忠兴,史成恩,等.鄂尔多斯盆地西南部上三叠统延长组长8、长6油层组的沉积体系与物源方向[J].地质通报,2008,27(1):101-111.]
[12]Liu Ruie,Wei Xiaofeng,Wang Yali, et al. The geochemical characteristics of RARAE earth elements of the shale rock in the geological signification of the analysis of the sedimentary provenance:An example in the Upper Paleozoic in the Ordos Basin[J].Natural Gas Geoscience,2005,16(6):788-791.[刘锐娥,卫孝峰,王亚丽,等.泥质岩稀土元素地球化学特征在物源分析中的意义——以鄂尔多斯盆地上古生界为例[J].天然气地球科学,2005,16(6):788-791.]
[13]Song Kai,Lü Jianwen,Du Jinliang, et al. Source direction analysis and delta depositional systems of Yanchang Formation of the Upper Triassic in the central Ordos Basin[J].Journal of Palaeogeography,2002,4(3):59-66.[宋凯,吕剑文,杜金良,等.鄂尔多斯盆地中部上三叠统延长组物源方向分析与三角洲沉积体系[J].古地理学报,2002,4(3):59-66.]
[14]Wei Bin,Wei Honghong,Chen Quanhong, et al. Sediment provenance analysis of Yanchang Formation in Ordos Basin[J].Journal of Northwest University:Natural Science Edition,2003,33(4):447-450.[魏斌,魏红红,陈全红,等.鄂尔多斯盆地上三叠统延长组物源分析[J].西北大学学报:自然科学版,2003,33(4):447-450.]
[15]Nie Yongsheng,Tian Jingchun,Xia Qingsong, et al. Source analysis of Yanchang Formation in Baibao-Jiyuan region,Ordos Basin[J].Petroleum Geology and Recovery Efficiency,2004,11(5):4-6.[聂永生,田景春,夏青松,等.鄂尔多斯盆地白豹一姬源地区上三叠统延长组物源分析[J].油气地质与采收率,2004,11(5):4-6.]
[16]Lü Qiang,Zhao Junxing,Chen Hongde, et al. Analysis of the provenance and basin bottom shape of Yanchang Epoch of Mesozoic in Ordos Basin,China[J].Journal of Chengdu University of Technology:Science &Technology Edition,2008,35(6):610-616.[吕强,赵俊兴,陈洪德,等.鄂尔多斯盆地南部中生界延长组物源与盆地底形分析[J].成都理工大学学报:自然科学版,2008,35(6):610-616.]
[17]Chen Fei,Fan Tailiang,Gao Zhiqian, et al. Analysis of the provenance direction and the depositional systems of Yanchang Formation of Upper Triassic in the southern Ordos Basin[J].Journal of Xi′an Shiyou University:Natural Science Edition,2009,24(6):24-32.[陈飞,樊太亮,高志前,等.鄂尔多斯盆地南部上三叠统延长组物源方向与沉积体系分析[J].西安石油大学学报:自然科学版,2009,24(6):24-32.]
[18]Zhu Zongliang,Li Wenhou,Li Keyong, et al. Provenance analysis ofLate Triassic sediments in the southern Ordos Basin[J].Geological Journal of China Universities,2010,16(4):547-555.[朱宗良,李文厚,李克永,等.鄂尔多斯盆地南部晚三叠世物源分析[J].高校地质学报,2010,16(4):547-555.]
[19]Deng Kun,Zhang Shaonan,Ding Xiaoqi, et al. Provenance analysis of Chang 8 and Chang 6 members of Yangchang Formation in Fuxian exploration area of Ordos Basin[J].Journal of Guilin University of Technology,2012,32(1):29-35.[邓昆,张哨楠,丁晓琪,等.鄂尔多斯盆地富县探区延长组长8长6物源分析来自岩石地球化学及重矿物的证据[J].桂林理工大学学报,2012,32(1):29-35.]
[20]Zhao Yunxiang,Wang Jianfeng,Ding Xiong, et al. Provenance analysis Upper Triassic Chang 9 reservoir in Ordos Basin[J].Journal of Oil and Gas Technology,2012,34(4):7-13.[赵云翔,王建峰,丁熊,等.鄂尔多斯盆地上三叠统长9油层组物源分析[J].石油天然气学报,2012,34(4):7-13.]
[21]Shang Ting,Chen Gang,Li Wenhou, et al. Provenance analysis of Chang 6 reservoir in Fuhuang exploration area of Ordos Basin[J].Geological Science and Technology Information,2012,31(1):33-40.[尚婷,陈刚,李文厚,等.鄂尔多斯盆地东南部富黄探区延长组长6 段物源分析[J].地质科技情报,2012,31(1):33-40.]
[22]Yang Hua,Liu Ziliang,Zhu Xiaomin, et al. Provenance and depositional systems of the Upper Triassic Yanchang Formation in the southwestern Ordos Basin,China[J].Earth Science Frontiers,2013,20(2):10-18.[杨华,刘自亮,朱筱敏,等.鄂尔多斯盆地西南缘上三叠统延长组物源与沉积体系特征[J].地学前缘,2013,20(2):10-18.]
[23]Xie Xiangyang,Heller P L.U-Pb Detrital zircon geochronology and its implications:The Early Late-Triassic Yanchang Formation,south Ordos Basin,China[J].Journal of Asian Earth Sciences,2013,64(5):86-98.
[24]Li Hongyan,Huang Xiaolong.Constraints on the paleogeographic evolution of the north China Craton during the Late Triassic-Jurassic[J].Journal of Asian Earth Sciences,2013,(70/71):308-320.
[25]Zhang Fuli.Relation of multicycles tool and natural gas in the Ordos Basin[J].Petroleum Geology and Experiment,2006,26(2):138-142.[张福礼.多旋回与鄂尔多斯盆地石油天然气[J].石油实验地质,2004,26(2):138-142.]
[26]Liu Chiyang,Zhao Hongge,Gui Xiaojun, et al. Space-Time coordinate of the evolution and reformation and mineralization response in Ordos Basin[J].Acta Geologica Sinica,2006,80(5):617-638.[刘池洋,赵红格,桂小军,等.鄂尔多斯盆地演化-改造的时空坐标及其成藏(矿)响应[J].地质学报,2006,80(5):617-638.]
[27]Zhang Yueqiao,Liao Changzhen.Transition of the Late Mesozoic-Cenozoic tectonic regimes and modification of the Ordos Basin[J].Geology China,2006,33(1):28-40.[张岳桥,廖昌珍.晚中生代—新生代构造体制转换与鄂尔多斯盆地改造[J].中国地质,2006,33(1):28-40.]
[28]Yang Minghui,Liu Chiyang,Zheng,Menglin, et al. The sequence contexture of two different kinds of margins in the Middle-Late Triassic in Ordos Basin and their response to tectonic activities[J].Science China:Series D,2007,37(supplement 1):173-184.[杨明慧,刘池洋,郑孟林,等.鄂尔多斯盆地中晚三叠世两种不同类型边缘层序构成及对构造活动响应[J].中国科学:D辑,2007,37(增1):173-184.]
[29]Liu Jun,Wu Xiaochun,Li Jinling.The first reptile from the Tongchuan Formation and its stratigraphical significance[J].Vertebrata Palasiatica,2001,39(1):67-71.[刘俊,吴肖春,李锦玲.北铜川组爬行动物化石的首次发现及其地层意义[J].古脊椎动物学报,2001,39(1):67-71.]
[30]Xie Xiangyang.Sedimentary Record of Mesozoic Intracontinental Deformation in the South Ordos Basin,China[D].Laramie:The University of Wyoming,2007.
[31]Wang Duoyun,Xin Bushe,Yang Hua, et al. Zircon SHRIMP U-Pb age and geological implications of tuff at the bottom of Chang-7 member of Yanchang Formation in Ordos Basin[J].Science China Earth Sciences, (in press).
[32]Mao Guangzhou,Liu Chiyang.Application of geochemistry in provenance and depositional setting analysis[J].Journal of Earth Sciences and Environment,2011,33(4):337-348.[毛光周,刘池洋.地球化学在物源及沉积背景分析中的应用[J].地球科学与环境学报,2011,33(4):337-348.]
[33]Sun S S,McDonough W F.Chemical and Isotopic Systematics of Oceanic Basalts:Implication for the Mantle Composition and Process[M].Saunder A D,Norry M J.London:Magmatism in the Ocean Basins Geological Society of London Special Publication,1989:313-345.
[34]Taylor S R,McLennan S M.The Continental Crust:Its Composition and Evolution[M].Oxford:Blackwell Scientific,1985:1-312.
[35]McLenna S M,Hemming S R,Taylor S R, et al. Early Proterozoic crustal evolution:Geochemical and Nd-Pb isotopic evidence from metasedimentary rocks,southwestern North America[J].Geochemical et Cosmochimica Acta,1995,59:1153-1177.
[36]Roser B P,Korsch R J.Provenance signatures of sandstone-mudstone suites determined using discriminant function analysis of major-element data[J].Chemical Geology,1988,67:119-139.
[37]Allegre C T.Quantitative models of trace planet[J].Earth and Pantetary Science Letters,1978,38(1):1-25.
[38]Li Hongyan,Xu Yigang,Huang Xiaolong, et al. Activation of northern margin of the north China Craton in Late Paleozoic:Evidence from U-Pb dating and Hf isotopes of detrital zircons from the Upper Carboniferous Taiyuan Formation in the Ningwu-Jingle Basin[J].Chinese Science Bulletin,2009,54(4):677-686.
[39]Zhao Yue,Chen Bin,Zhang Shuanghong, et al. Pre-Yanshanian geological events in the northern margin of the north China Craton and its adjacent areas[J].Geology in China,2010,37(4):900-915.[赵越,陈斌,张拴宏,等.华北克拉通北缘及邻区前燕山期主要地质事件[J].中国地质,2010,37(4):900-915.]
[40]Diwu Chunrong,Sun Yong,Zhang Hong, et al. Episodic tectonothermal events of the western north China Craton and north Qinling Orogenic Belt in central China:Constraints from detrital zircon U-Pb ages[J].Journal of Asian Earth Sciences,2012,47:107-122.
[41]Chen Zhihong,Lu Songnian,Li Huaikun, et al. Constraining the role of the Qinling orogen in the assembly and break-up of Rodinia:Tectonic implications for Neoproterozoic granite occurrences[J].Journal of Asian Earth Sciences,2006,(28):99-175.