松辽盆地北部龙虎泡地区铁钛氧化物与砂岩型铀矿化关系探讨
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摘要
龙虎泡铀矿化区的发现是近年来根据油田资料二次开发和钻探验证而取得的重要创新成果之一,矿化区位于松辽盆地北部龙虎泡-大安阶地北,西与泰康隆起区和西部超覆区相邻。本文在详实的野外工作基础之上,利用偏光显微镜、电子显微镜、能谱、背散射、点化学分析及元素面扫描分析等手段,对龙虎泡地区含铀砂岩中以钛铁矿及其相关蚀变矿物为代表的铁钛氧化物与砂岩型铀矿化之间的关系进行了研究探讨,结果表明:①以富铀-铁钛氧化物-钛氧化物-黄铁矿为代表的蚀变矿物共生组合记录和保留了有关砂岩型铀矿成矿流体和成矿环境的重要信息,含矿砂岩中钛铁矿及其蚀变相关的富铀-铁钛氧化物、钛氧化物、黄铁矿等矿物的不同产出类型和不同蚀变矿物共生组合关系对比分析指示,龙虎泡地区铀成矿受到了后期含铀富铁的氧化性流体与富H_2S的还原性流体混合作用影响,成矿环境偏强还原;②与铀矿化关系最为密切的铁钛氧化物是蚀变程度高且富镁的钛铁矿,富铀-铁钛氧化物即是这些强蚀变钛铁矿与后期成矿流体发生氧化还原作用形成的,钛铁矿内部溶蚀裂隙为含矿流体的蚀变和铀的沉淀富集提供了良好的容矿空间,蚀变钛铁矿和黄铁矿为铀的沉淀富集分别提供了良好的矿物尺度上的氧化障和还原障,在含矿流体与富H_2S还原性流体混合过程中,铀得以在蚀变钛铁矿与黄铁矿的氧化还原界面附近沉淀富集。
The Longhupao uranium mineralization area,which is located in the north of Longhupao-Da'an terrace and adjacent to Taikang uplift and Western overlap in the west,is one of the important new achievements in northern Songliao Basin based on the secondary development and drilling verification of Daqing Oilfield wells. Based on detailed field work and using experimental means such as polarizing microscope,electron probe energy spectrum,backscattering,chemical analysis and distribution analysis of elements,the authors aimed to explore the relationship between the Fe-Ti oxides represented by ilmenite and sandstone-hosted uranium mineralization in Longhupao area. The study shows that the assemblage of altered minerals represented by U-rich Fe-Ti oxide-titanium oxidepyrite has recorded the important information about ore-forming fluid and metallogenic environment in the process of sandstone-hosted uranium mineralization. The comparative analysis of different occurrences and assemblages for ilmenites and other altered minerals as U-rich Fe-Ti oxide,titanium oxide and pyrite reveals that the uranium mineralization in the Longhupao area was affected by the later oxidative fluid including U/Fe and the reductive fluid including H_2 S,and the metallogenic environment was strongly reductive. These strongly altered and Mg-rich ilmenites were closely related to the uranium mineralization,and the U-rich Fe-Ti oxides were formed in the redox reaction between these altered ilmenites and the later ore-bearing fluid. The corrosion fissures in these altered ilmenites provided favorable space for further alteration by ore-bearing fluid and uranium precipitation. The altered ilmenite offered a profitable mineral-scale oxidation barrier,and the pyrite offered a reduction barrier for uranium precipitation. During the fluid mixing of ore-forming and H_2 S-rich fluid,the uranium precipitated near the interface of reduction oxidation between altered ilmenites and pyrites.
The Longhupao uranium mineralization area,which is located in the north of Longhupao-Da'an terrace and adjacent to Taikang uplift and Western overlap in the west,is one of the important new achievements in northern Songliao Basin based on the secondary development and drilling verification of Daqing Oilfield wells. Based on detailed field work and using experimental means such as polarizing microscope,electron probe energy spectrum,backscattering,chemical analysis and distribution analysis of elements,the authors aimed to explore the relationship between the Fe-Ti oxides represented by ilmenite and sandstone-hosted uranium mineralization in Longhupao area. The study shows that the assemblage of altered minerals represented by U-rich Fe-Ti oxide-titanium oxidepyrite has recorded the important information about ore-forming fluid and metallogenic environment in the process of sandstone-hosted uranium mineralization. The comparative analysis of different occurrences and assemblages for ilmenites and other altered minerals as U-rich Fe-Ti oxide,titanium oxide and pyrite reveals that the uranium mineralization in the Longhupao area was affected by the later oxidative fluid including U/Fe and the reductive fluid including H_2 S,and the metallogenic environment was strongly reductive. These strongly altered and Mg-rich ilmenites were closely related to the uranium mineralization,and the U-rich Fe-Ti oxides were formed in the redox reaction between these altered ilmenites and the later ore-bearing fluid. The corrosion fissures in these altered ilmenites provided favorable space for further alteration by ore-bearing fluid and uranium precipitation. The altered ilmenite offered a profitable mineral-scale oxidation barrier,and the pyrite offered a reduction barrier for uranium precipitation. During the fluid mixing of ore-forming and H_2 S-rich fluid,the uranium precipitated near the interface of reduction oxidation between altered ilmenites and pyrites.
引文
Amini A and Anketell J M.2015.Textural and geochemical studies of detrital Fe-Ti oxides and test of their validity in provenance determination,a case study from Central Iran[J].Journal of African Earth Sciences,103:140~152.
Bacon C R and Hirschmann M M.1988.Mg/Mn partitioning as a test for equilibrium between coexisting Fe-Ti oxides[J].American Mineralogist,73(1~2):57~61.
Bailey S W,Weege R J,Cameron E N,et al.1956.The alteration of ilmenite in beach sands[J].Economic Geology,51(3):263~279.
Castillo O M,Melgarejo J C,GalíS,et al.2017.Use and misuse of Mgand Mn-rich ilmenite in diamond exploration:A petrographic and trace element approach[J].Lithos,292~293:348~363.
Chen Debing,Bai Jingping and Zhang Shuyi.2007.Elementary analysis on the hydrodynamic system and uranium mineralization type in Songliao basin[J].Uranium Geology,23(5):283~288(in Chinese with English abstract).
Chen Lulu,Chen Yin,Guo Hu,et al.2018.Alteration characteristics of titanium-bearing minerals and new knowledge about their relationship to uranium occurrence in uraniferous sandstone of Nalinggou area,Ordos Basin[J].Geology in China,45(2):408~409(in Chinese).
Darby D A.1990.Evidence for the Hudson River as the dominant source of sand on the US Atlantic Shelf[J].Nature,6 287(346):828~831.
Davies R V,Kennedy J,Mcilroy R W,et al.1964.Extraction of uranium from sea water[J].Nature,203(4 950):1 110~1 115.
Dymkov Y M,Doinikova O A and Volkov N I.2003.Finding of U-Fe-ZrTi-S-P gel at the exogenic epigenetic Khokhlovskoe Uranium Deposit,Southern Transural Region[J].Geochemistry International,41(11):1 126~1 133.
Eglizaud N,Miserque F,Simoni E,et al.2006.Uranium(Ⅵ)interaction with pyrite(Fe S2):Chemical and spectroscopic studies[J].Radiochimica Acta,94(9~11):651~656.
Frost B R and Donald H L.1991.Occurrence of iron-titanium oxides in igneous rocks[J].Reviews in Mineralogy and Geochemistry,25(1):433~468.
Frost M T.1983.The dependence of alumina and silica contents on the extent of alteration of weathered ilmenites from Western Australia[J].Mineralogical Magazine,47:201~208.
Gruner J W.1959.The decomposition of ilmenite:Discussion[J].Economic Geology,54(7):1 315~1 316.
Guo Yufeng,LüYanan,Jiang Tao,et al.2010.Effect of pre-oxidation on Pangzhihua ilmenite in solid state reduction process[J].Journal of University of Science and Technology Beijing,32(4):413~419(in Chinese with English abstract).
Hu Wangshui,LüBingquan,Zhang Wenjun,et al.2005.An approach to tectonic evolution and dynamics of the Songliao Basin[J].Chinese Journal of Geology,40(1):16~31(in Chinese with English abstract).
Ismail M G M U,Hirano S I and Sōmiya S.1989.Decomposition of ilmenite under hydrothermal condition(preliminary work)[A].Hydrothermal Reactions for Materials Science and Engineering[C].Springer Netherlands,190~193.
Janeczek J and Ewing R C.1992.Coffinitization-A mechanism for the alteration of UO2under reducing conditions[J].Materials Research Society Symposia Proceedings,257:497~504.
Kolker A.1982.Mineralogy and geochemistry of Fe-Ti oxide and apatite(nelsonite)deposits and evaluation of the liquid i Immiscibility hypothesis[J].Economic Geology,77(5):1 146~1 158.
Li Jin,Zhu Xiangkun and Tang Suohan.2012.Equilibrium fractionation of Fe isotopes during Fe(Ⅲ)hydrolysis[J].Acta Petrologica et Mineralogica,31(6):891~896(in Chinese with English abstract).
Lindsley D H and Epler N.2017.Do Fe-Ti-oxide magmas exist?Probably not![J].American Mineralogist,102:2 157~2 169.
Mcguire M M,Jallad K N,Ben A D,et al.2001.Bacterial and thermochemical sulfate reduction in diagenetic settings-Old and new insights[J].Applied Surface Science,178(1):105~115.
Morad S and Aldahan A A.1986.Alteration of detrital Fe-Ti oxides in sedimentary rocks[J].Geological Society of America Bulletin,97(5):567~578.
Mücke A and Chaudhuri J N B.1991.The continuous alteration of ilmenite through pseudorutile to leucoxene[J].Ore Geology Reviews,6(1):25~44.
Noubactep C,Sch Ner A,Dienemann H,et al.2006.Release of coprecipitated uranium from iron oxides[J].Journal of Radioanalytical and Nuclear Chemistry,267(1):21~27.
Parnell J.2004.Titanium mobilization by hydrocarbon fluids related to sill intrusion in a sedimentary sequence,Scotland[J].Ore Geology Reviews,24(1~2):155~167.
Ren Qijiang,Guilbert J M,Lei Bingshun,et al.1987.Manganese content in ilmenite from intermediate-acid intrusions and its implication for petrogenesis[J].Acta Petrologica et Mineralogica,6(3):235~246(in Chinese with English abstract).
Reynolds R L and Goldhaber M B.1978a.Iron-titanium oxide minerals and associated alteration phases in some uranium-bearing sandstones[J].Journal of Resrarch of the U.S.Geological Suevey,6(6):707~714.
Reynolds R L and Goldhaber M B.1978b.Origin of a south Texas roll-type uranium deposit[J].Economic Geology,73(8):1 677~1 689.
Reynolds R L,Rosenbaum J G and Thompson R S.2008.Mineralogic causes of variations in magnetic susceptibility of Late Pleistocene and Holocene sediment from Great Salt Lake,Utah[J].U.S.Geological Survey Open-File Report 2008~1352,1~17.
Saager R and Stupp H G.1983.U-Ti phases from precambrian quartzpebble conglomerates of the Elliot Lake Area,Canada,and the Pongola Basin,South Africa[J].Tschermaks Mineralogische und Petrographische Mitteilungen,32(2~3):83~102.
Scott T B,Riba Tort O and Allen G C.2007.Aqueous uptake of uranium onto pyrite surfaces:Reactivity of fresh versus weathered material[J].Geochimica et Cosmochimica Acta,71(21):5 044~5 053.
Sevastjanova I,Hall R and Alderton D.2012.A detrital heavy mineral viewpoint on sediment provenance and tropical weathering in SE Asia[J].Sedimentary Geology,280:179~194.
Shellnutt J G,Zhou M F and Zellmer G F.2009.The role of Fe-Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap:An example from the Permian Baima igneous complex,SW China[J].Chemical Geology,259(3~4):204~217.
Shi Wanchao.2017.Study on Layer-lithology Traps Recognition and Evaluate of K2y in the Taikang Uplift Belt Songliao Basin[D].Daqing:Master Thesis of Northeast Petroleum University,7~13(in Chinese with English abstract).
Sun Jian,Zhu Xiangkun and Li Shizhen.2015.Fe isotope biogeochemistry and its applications[J].Acta Petrologica et Mineralogica,34(5):777~784(in Chinese with English abstract).
Tang Chao,Jin Ruoshi,Gu Shefeng,et al.2018.Discovery and significance of industrial uranium ore in Sifangtai Formation,north Songliao basin[J].Geological Survey and Research,41(1):1~8(in Chinese with English abstract).
Tang H B and Liu Y M.2013.Decomposition of ilmenite by ammonium hydroxide[J].Advanced Materials Research,813:484~488.
Tang Zhenguo.2015.The Accumulation Research of Lithology and Structural-lithologic Reservoirs in the Western Slope of the Northern Songliao Basin[D].Chengdu:Doctoral Thesis of Chengdu University of Technology,22~42(in Chinese with English abstract).
Temple A K.1966.Alteration of ilmenite[J].Economic Geology,61(4):695~714.
Teufer G and Temple A K.1966.Pseudorutile-A new mineral intermediate between ilmenite and rutile in the N alteration of ilmenite[J].Nature,211(5 045):179~181.
Vinokurov S F and Nesterova M V.2010.New mechanism of the formation of the uranium-titanium association in ores of paleovalley deposits[J].Doklady Earth Sciences,431(1):380~385.
Wan Shuangshuang.2012.The Study on Tectonic Evolution in North Songliao Basin[D].Chengdu:Master Thesis of Chengdu University of Technology,34~56(in Chinese with English abstract).
Wang Man,Tan Jun,Chen Qiyuan,et al.2012.Effect of oxidizationreduction-mechanical activation process on leaching behavior of Panxi Ilmenite[J].Nonfereous Metals(Extractive Metallurgy),(5):1~4(in Chinese with English abstract).
Wang Shibo.2013.Research of Structural Feature and Basin-forming Dynamic in the North of Songliao Basin[D].Chengdu:Doctoral Thesis of Chengdu University of Technology,60~90(in Chinese with English abstract).
Wang Y and Yuan Z.2006.Reductive kinetics of the reaction between a natural ilmenite and carbon[J].International Journal of Mineral Processing,81(3):133~140.
Wei Jialin,Tang Chao,Xu Zenglian,et al.2018.Research on sandstone-hosted uranium mineralization of the Sifangtai Formation in southern Daqing placanticline[J].Geological Survey and Research,41(1):9~17(in Chinese with English abstract).
Wu Jianhua,Guo Guolin,Guo Jialei,et al.2017.Spatial-temporal distribution of Mesozoic igneous rockand their relationship with hydrothermal uranium deposits in eastern China[J].Acta Petrologica Sinica,33(5):1 591~1 614(in Chinese with English abstract).
Xi Haiyin,Ma Chao,Lu Shengjun,et al.2017.Metallogenic condition and prospecting orientation of uranium deposits in the middle district of Daxinganling mountains[J].Journal of East China University of Technology(Natural Science),40(3):237~245(in Chinese with English abstract).
Yang Chengzhi.2014.Comparative Study on Late Cretaceous Tectonic Inversion of Songliao Basin-Great Sanjiang Basin and Its genetic Relationships[D].Wuhan:Doctoral Thesis of China University of Geosciences,31~52(in Chinese with English abstract).
Yang Haibo,Zhu Yanping and Gu Shefeng.2012.Reversal tectonic characteristics and their contribution to mineralizing uranium in North Songliao Basin[J].Petroleum Geology and Oilfield Development in Daqing,31(5):7~11(in Chinese with English abstract).
Yao Zhongwen,Wan Shuangshuang,Zheng Zhiyi,et al.2017.Reservoir accumulation mechanism of Aogula-Talaha fault zone in the Songliao Basin[J].J.Mineral Petrol.,31(1):66~73(in Chinese with English abstract).
Yue Shuqin,Fang Yelong and Sun Shuqiong.1982.Iron-titanium oxides and their equilibrium temperatures[J].J.Mineral.Petrol.,2:15~17(in Chinese with English abstract).
Yurkova R M.1970.Comparison of post-sedimentary alterations of oil-,gas-and water-bearing rocks[J].Sedimentology,15:53~68.
Zhang Fanghou.1987.Secondary migration of hydrocarbon from Qijia-Gulong Sag to Longhupao oil field[J].Petroleum Geology&Oilfield Development in Daqing,6(4):11~19(in Chinese with English abstract).
Zhang Mingxue,Dai Haotian and Li Zhandong.2018.Characteristics behind tectonic evolution and optimization of favorable oil and gas areas in Longhupao area[J].Journal of Heilongjiang University of Science&Technology,28(2):163~167(in Chinese with English abstract).
Zheng Yixing.1986.Research on the Fe-Ti oxides in the uraniferous sandstone[J].Uranium Geology Abroad,1:12~16(in Chinese).
Zhong Yanqiu and Ma Wenjuan.2011.Mesozoic,Cenozoic tectonic movements and the control on sandstone-hosted uranium deposit in north Songliao Basin[J].Contributions to Geology and Mineral Resources Research,26(4):411~416(in Chinese with English abstract).
陈德兵,白景萍,张书义.2007.松辽盆地水动力系统和铀矿化类型浅析[J].铀矿地质,23(5):283~288.
陈路路,陈印,郭虎,等.2018.鄂尔多斯盆地纳岭沟地区含铀砂岩中含钛类矿物蚀变特征及与铀赋存关系新认识[J].中国地质,45(2):408~409.
郭宇峰,吕亚男,姜涛,等.2010.预氧化在攀枝花钛铁矿固态还原过程中的作用[J].北京科技大学学报,32(4):413~419.
胡望水,吕炳全,张文军,等.2005.松辽盆地构造演化及成盆动力学探讨[J].地质科学,40(1):16~31.
李津,朱祥坤,唐索寒.2012.Fe(Ⅲ)水解过程中的Fe同位素分馏研究[J].岩石矿物学杂志,31(6):891~896.
任启江,Guilbert J M,雷秉舜,等.1987.中-酸性侵入岩中钛铁矿的锰含量及其岩石成因意义[J].岩石矿物学杂志,6(3):235~246.
石万超.2017.松辽盆地北部泰康隆起带姚家组岩性圈闭识别及评价研究[D].大庆:东北石油大学硕士论文,7~13.
孙剑,朱祥坤,李世珍.2015.生物过程中的铁同位素地球化学行为及应用[J].岩石矿物学杂志,34(5):777~784.
汤超,金若时,谷社峰,等.2018.松辽盆地北部四方台组工业铀矿体的发现及其意义[J].地质调查与研究,41(1):1~8.
唐振国.2015.松辽盆地北部西斜坡岩性及构造-岩性油藏成藏规律研究[D].成都:成都理工大学博士论文,22~42.
万双双.2012.松辽盆地北部构造演化研究[D].成都:成都理工大学硕士论文,34~56.
王曼,谭军,陈启元,等.2012.氧化还原-机械活化对攀西钛铁矿浸出行为的影响[J].有色金属(冶炼部分),5:1~4.
王始波.2013.松辽盆地北部构造特征与成盆动力学研究[D].成都:成都理工大学博士论文,60~90.
魏佳林,汤超,徐增连,等.2018.大庆长垣南部四方台组砂岩型铀矿化特征研究[J].地质调查与研究,41(1):9~17.
巫建华,郭国林,郭佳磊,等.2017.中国东部中生代岩浆岩的时空分布及其与热液型铀矿的关系[J].岩石学报,33(5):1 591~1 614.
席海银,马超,卢胜军,等.2017.大兴安岭中段铀成矿地质条件及找矿方向[J].东华理工大学学报(自然科学版),40(3):237~245.
杨承志.2014.松辽盆地-大三江盆地晚白垩世构造反转作用对比及其成因联系[D].武汉:中国地质大学博士论文,31~52.
杨海波,朱彦平,谷社峰.2012.松辽盆地北部反转构造特征及对铀成矿的作用[J].大庆石油地质与开发,31(5):7~11.
么忠文,万双双,郑治义,等.2017.松辽盆地敖古拉-他拉哈断裂带成藏机制[J].矿物岩石,31(1):66~73.
岳树勤,方业龙,孙淑琼.1982.铁钛氧化物及其平衡温度[J].矿物岩石,2:15~17.
张方吼.1987.齐家-古龙凹陷向龙虎泡油田的油气二次运移[J].大庆石油地质与开发,6(4):11~19.
张明学,戴昊天,李占东.2018.龙虎泡地区构造演化特征与油气有利区优选[J].黑龙江科技大学学报,28(2):163~167.
郑一星.1986.含铀砂岩中的铁-钛氧化物研究[J].国外铀矿地质,1:12~16.
钟延秋,马文娟.2011.松辽盆地北部中、新生代构造运动特征及对砂岩型铀矿的控制作用[J].地质找矿论丛,26(4):411~416.
Bacon C R and Hirschmann M M.1988.Mg/Mn partitioning as a test for equilibrium between coexisting Fe-Ti oxides[J].American Mineralogist,73(1~2):57~61.
Bailey S W,Weege R J,Cameron E N,et al.1956.The alteration of ilmenite in beach sands[J].Economic Geology,51(3):263~279.
Castillo O M,Melgarejo J C,GalíS,et al.2017.Use and misuse of Mgand Mn-rich ilmenite in diamond exploration:A petrographic and trace element approach[J].Lithos,292~293:348~363.
Chen Debing,Bai Jingping and Zhang Shuyi.2007.Elementary analysis on the hydrodynamic system and uranium mineralization type in Songliao basin[J].Uranium Geology,23(5):283~288(in Chinese with English abstract).
Chen Lulu,Chen Yin,Guo Hu,et al.2018.Alteration characteristics of titanium-bearing minerals and new knowledge about their relationship to uranium occurrence in uraniferous sandstone of Nalinggou area,Ordos Basin[J].Geology in China,45(2):408~409(in Chinese).
Darby D A.1990.Evidence for the Hudson River as the dominant source of sand on the US Atlantic Shelf[J].Nature,6 287(346):828~831.
Davies R V,Kennedy J,Mcilroy R W,et al.1964.Extraction of uranium from sea water[J].Nature,203(4 950):1 110~1 115.
Dymkov Y M,Doinikova O A and Volkov N I.2003.Finding of U-Fe-ZrTi-S-P gel at the exogenic epigenetic Khokhlovskoe Uranium Deposit,Southern Transural Region[J].Geochemistry International,41(11):1 126~1 133.
Eglizaud N,Miserque F,Simoni E,et al.2006.Uranium(Ⅵ)interaction with pyrite(Fe S2):Chemical and spectroscopic studies[J].Radiochimica Acta,94(9~11):651~656.
Frost B R and Donald H L.1991.Occurrence of iron-titanium oxides in igneous rocks[J].Reviews in Mineralogy and Geochemistry,25(1):433~468.
Frost M T.1983.The dependence of alumina and silica contents on the extent of alteration of weathered ilmenites from Western Australia[J].Mineralogical Magazine,47:201~208.
Gruner J W.1959.The decomposition of ilmenite:Discussion[J].Economic Geology,54(7):1 315~1 316.
Guo Yufeng,LüYanan,Jiang Tao,et al.2010.Effect of pre-oxidation on Pangzhihua ilmenite in solid state reduction process[J].Journal of University of Science and Technology Beijing,32(4):413~419(in Chinese with English abstract).
Hu Wangshui,LüBingquan,Zhang Wenjun,et al.2005.An approach to tectonic evolution and dynamics of the Songliao Basin[J].Chinese Journal of Geology,40(1):16~31(in Chinese with English abstract).
Ismail M G M U,Hirano S I and Sōmiya S.1989.Decomposition of ilmenite under hydrothermal condition(preliminary work)[A].Hydrothermal Reactions for Materials Science and Engineering[C].Springer Netherlands,190~193.
Janeczek J and Ewing R C.1992.Coffinitization-A mechanism for the alteration of UO2under reducing conditions[J].Materials Research Society Symposia Proceedings,257:497~504.
Kolker A.1982.Mineralogy and geochemistry of Fe-Ti oxide and apatite(nelsonite)deposits and evaluation of the liquid i Immiscibility hypothesis[J].Economic Geology,77(5):1 146~1 158.
Li Jin,Zhu Xiangkun and Tang Suohan.2012.Equilibrium fractionation of Fe isotopes during Fe(Ⅲ)hydrolysis[J].Acta Petrologica et Mineralogica,31(6):891~896(in Chinese with English abstract).
Lindsley D H and Epler N.2017.Do Fe-Ti-oxide magmas exist?Probably not![J].American Mineralogist,102:2 157~2 169.
Mcguire M M,Jallad K N,Ben A D,et al.2001.Bacterial and thermochemical sulfate reduction in diagenetic settings-Old and new insights[J].Applied Surface Science,178(1):105~115.
Morad S and Aldahan A A.1986.Alteration of detrital Fe-Ti oxides in sedimentary rocks[J].Geological Society of America Bulletin,97(5):567~578.
Mücke A and Chaudhuri J N B.1991.The continuous alteration of ilmenite through pseudorutile to leucoxene[J].Ore Geology Reviews,6(1):25~44.
Noubactep C,Sch Ner A,Dienemann H,et al.2006.Release of coprecipitated uranium from iron oxides[J].Journal of Radioanalytical and Nuclear Chemistry,267(1):21~27.
Parnell J.2004.Titanium mobilization by hydrocarbon fluids related to sill intrusion in a sedimentary sequence,Scotland[J].Ore Geology Reviews,24(1~2):155~167.
Ren Qijiang,Guilbert J M,Lei Bingshun,et al.1987.Manganese content in ilmenite from intermediate-acid intrusions and its implication for petrogenesis[J].Acta Petrologica et Mineralogica,6(3):235~246(in Chinese with English abstract).
Reynolds R L and Goldhaber M B.1978a.Iron-titanium oxide minerals and associated alteration phases in some uranium-bearing sandstones[J].Journal of Resrarch of the U.S.Geological Suevey,6(6):707~714.
Reynolds R L and Goldhaber M B.1978b.Origin of a south Texas roll-type uranium deposit[J].Economic Geology,73(8):1 677~1 689.
Reynolds R L,Rosenbaum J G and Thompson R S.2008.Mineralogic causes of variations in magnetic susceptibility of Late Pleistocene and Holocene sediment from Great Salt Lake,Utah[J].U.S.Geological Survey Open-File Report 2008~1352,1~17.
Saager R and Stupp H G.1983.U-Ti phases from precambrian quartzpebble conglomerates of the Elliot Lake Area,Canada,and the Pongola Basin,South Africa[J].Tschermaks Mineralogische und Petrographische Mitteilungen,32(2~3):83~102.
Scott T B,Riba Tort O and Allen G C.2007.Aqueous uptake of uranium onto pyrite surfaces:Reactivity of fresh versus weathered material[J].Geochimica et Cosmochimica Acta,71(21):5 044~5 053.
Sevastjanova I,Hall R and Alderton D.2012.A detrital heavy mineral viewpoint on sediment provenance and tropical weathering in SE Asia[J].Sedimentary Geology,280:179~194.
Shellnutt J G,Zhou M F and Zellmer G F.2009.The role of Fe-Ti oxide crystallization in the formation of A-type granitoids with implications for the Daly gap:An example from the Permian Baima igneous complex,SW China[J].Chemical Geology,259(3~4):204~217.
Shi Wanchao.2017.Study on Layer-lithology Traps Recognition and Evaluate of K2y in the Taikang Uplift Belt Songliao Basin[D].Daqing:Master Thesis of Northeast Petroleum University,7~13(in Chinese with English abstract).
Sun Jian,Zhu Xiangkun and Li Shizhen.2015.Fe isotope biogeochemistry and its applications[J].Acta Petrologica et Mineralogica,34(5):777~784(in Chinese with English abstract).
Tang Chao,Jin Ruoshi,Gu Shefeng,et al.2018.Discovery and significance of industrial uranium ore in Sifangtai Formation,north Songliao basin[J].Geological Survey and Research,41(1):1~8(in Chinese with English abstract).
Tang H B and Liu Y M.2013.Decomposition of ilmenite by ammonium hydroxide[J].Advanced Materials Research,813:484~488.
Tang Zhenguo.2015.The Accumulation Research of Lithology and Structural-lithologic Reservoirs in the Western Slope of the Northern Songliao Basin[D].Chengdu:Doctoral Thesis of Chengdu University of Technology,22~42(in Chinese with English abstract).
Temple A K.1966.Alteration of ilmenite[J].Economic Geology,61(4):695~714.
Teufer G and Temple A K.1966.Pseudorutile-A new mineral intermediate between ilmenite and rutile in the N alteration of ilmenite[J].Nature,211(5 045):179~181.
Vinokurov S F and Nesterova M V.2010.New mechanism of the formation of the uranium-titanium association in ores of paleovalley deposits[J].Doklady Earth Sciences,431(1):380~385.
Wan Shuangshuang.2012.The Study on Tectonic Evolution in North Songliao Basin[D].Chengdu:Master Thesis of Chengdu University of Technology,34~56(in Chinese with English abstract).
Wang Man,Tan Jun,Chen Qiyuan,et al.2012.Effect of oxidizationreduction-mechanical activation process on leaching behavior of Panxi Ilmenite[J].Nonfereous Metals(Extractive Metallurgy),(5):1~4(in Chinese with English abstract).
Wang Shibo.2013.Research of Structural Feature and Basin-forming Dynamic in the North of Songliao Basin[D].Chengdu:Doctoral Thesis of Chengdu University of Technology,60~90(in Chinese with English abstract).
Wang Y and Yuan Z.2006.Reductive kinetics of the reaction between a natural ilmenite and carbon[J].International Journal of Mineral Processing,81(3):133~140.
Wei Jialin,Tang Chao,Xu Zenglian,et al.2018.Research on sandstone-hosted uranium mineralization of the Sifangtai Formation in southern Daqing placanticline[J].Geological Survey and Research,41(1):9~17(in Chinese with English abstract).
Wu Jianhua,Guo Guolin,Guo Jialei,et al.2017.Spatial-temporal distribution of Mesozoic igneous rockand their relationship with hydrothermal uranium deposits in eastern China[J].Acta Petrologica Sinica,33(5):1 591~1 614(in Chinese with English abstract).
Xi Haiyin,Ma Chao,Lu Shengjun,et al.2017.Metallogenic condition and prospecting orientation of uranium deposits in the middle district of Daxinganling mountains[J].Journal of East China University of Technology(Natural Science),40(3):237~245(in Chinese with English abstract).
Yang Chengzhi.2014.Comparative Study on Late Cretaceous Tectonic Inversion of Songliao Basin-Great Sanjiang Basin and Its genetic Relationships[D].Wuhan:Doctoral Thesis of China University of Geosciences,31~52(in Chinese with English abstract).
Yang Haibo,Zhu Yanping and Gu Shefeng.2012.Reversal tectonic characteristics and their contribution to mineralizing uranium in North Songliao Basin[J].Petroleum Geology and Oilfield Development in Daqing,31(5):7~11(in Chinese with English abstract).
Yao Zhongwen,Wan Shuangshuang,Zheng Zhiyi,et al.2017.Reservoir accumulation mechanism of Aogula-Talaha fault zone in the Songliao Basin[J].J.Mineral Petrol.,31(1):66~73(in Chinese with English abstract).
Yue Shuqin,Fang Yelong and Sun Shuqiong.1982.Iron-titanium oxides and their equilibrium temperatures[J].J.Mineral.Petrol.,2:15~17(in Chinese with English abstract).
Yurkova R M.1970.Comparison of post-sedimentary alterations of oil-,gas-and water-bearing rocks[J].Sedimentology,15:53~68.
Zhang Fanghou.1987.Secondary migration of hydrocarbon from Qijia-Gulong Sag to Longhupao oil field[J].Petroleum Geology&Oilfield Development in Daqing,6(4):11~19(in Chinese with English abstract).
Zhang Mingxue,Dai Haotian and Li Zhandong.2018.Characteristics behind tectonic evolution and optimization of favorable oil and gas areas in Longhupao area[J].Journal of Heilongjiang University of Science&Technology,28(2):163~167(in Chinese with English abstract).
Zheng Yixing.1986.Research on the Fe-Ti oxides in the uraniferous sandstone[J].Uranium Geology Abroad,1:12~16(in Chinese).
Zhong Yanqiu and Ma Wenjuan.2011.Mesozoic,Cenozoic tectonic movements and the control on sandstone-hosted uranium deposit in north Songliao Basin[J].Contributions to Geology and Mineral Resources Research,26(4):411~416(in Chinese with English abstract).
陈德兵,白景萍,张书义.2007.松辽盆地水动力系统和铀矿化类型浅析[J].铀矿地质,23(5):283~288.
陈路路,陈印,郭虎,等.2018.鄂尔多斯盆地纳岭沟地区含铀砂岩中含钛类矿物蚀变特征及与铀赋存关系新认识[J].中国地质,45(2):408~409.
郭宇峰,吕亚男,姜涛,等.2010.预氧化在攀枝花钛铁矿固态还原过程中的作用[J].北京科技大学学报,32(4):413~419.
胡望水,吕炳全,张文军,等.2005.松辽盆地构造演化及成盆动力学探讨[J].地质科学,40(1):16~31.
李津,朱祥坤,唐索寒.2012.Fe(Ⅲ)水解过程中的Fe同位素分馏研究[J].岩石矿物学杂志,31(6):891~896.
任启江,Guilbert J M,雷秉舜,等.1987.中-酸性侵入岩中钛铁矿的锰含量及其岩石成因意义[J].岩石矿物学杂志,6(3):235~246.
石万超.2017.松辽盆地北部泰康隆起带姚家组岩性圈闭识别及评价研究[D].大庆:东北石油大学硕士论文,7~13.
孙剑,朱祥坤,李世珍.2015.生物过程中的铁同位素地球化学行为及应用[J].岩石矿物学杂志,34(5):777~784.
汤超,金若时,谷社峰,等.2018.松辽盆地北部四方台组工业铀矿体的发现及其意义[J].地质调查与研究,41(1):1~8.
唐振国.2015.松辽盆地北部西斜坡岩性及构造-岩性油藏成藏规律研究[D].成都:成都理工大学博士论文,22~42.
万双双.2012.松辽盆地北部构造演化研究[D].成都:成都理工大学硕士论文,34~56.
王曼,谭军,陈启元,等.2012.氧化还原-机械活化对攀西钛铁矿浸出行为的影响[J].有色金属(冶炼部分),5:1~4.
王始波.2013.松辽盆地北部构造特征与成盆动力学研究[D].成都:成都理工大学博士论文,60~90.
魏佳林,汤超,徐增连,等.2018.大庆长垣南部四方台组砂岩型铀矿化特征研究[J].地质调查与研究,41(1):9~17.
巫建华,郭国林,郭佳磊,等.2017.中国东部中生代岩浆岩的时空分布及其与热液型铀矿的关系[J].岩石学报,33(5):1 591~1 614.
席海银,马超,卢胜军,等.2017.大兴安岭中段铀成矿地质条件及找矿方向[J].东华理工大学学报(自然科学版),40(3):237~245.
杨承志.2014.松辽盆地-大三江盆地晚白垩世构造反转作用对比及其成因联系[D].武汉:中国地质大学博士论文,31~52.
杨海波,朱彦平,谷社峰.2012.松辽盆地北部反转构造特征及对铀成矿的作用[J].大庆石油地质与开发,31(5):7~11.
么忠文,万双双,郑治义,等.2017.松辽盆地敖古拉-他拉哈断裂带成藏机制[J].矿物岩石,31(1):66~73.
岳树勤,方业龙,孙淑琼.1982.铁钛氧化物及其平衡温度[J].矿物岩石,2:15~17.
张方吼.1987.齐家-古龙凹陷向龙虎泡油田的油气二次运移[J].大庆石油地质与开发,6(4):11~19.
张明学,戴昊天,李占东.2018.龙虎泡地区构造演化特征与油气有利区优选[J].黑龙江科技大学学报,28(2):163~167.
郑一星.1986.含铀砂岩中的铁-钛氧化物研究[J].国外铀矿地质,1:12~16.
钟延秋,马文娟.2011.松辽盆地北部中、新生代构造运动特征及对砂岩型铀矿的控制作用[J].地质找矿论丛,26(4):411~416.
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