[52] Lu W., Wang X.*, Wan Q., Hu W., Chou I-M., Wan Y. (2023) In situ Raman spectroscopic measurement of the 13C/12C ratio in CO2: Experimental calibrations on the effects of fluid pressure, temperature and composition. Chemical Geology,  615, 121201, doi: https://doi.org/10.1016/j.chemgeo.2022.121201

[51] Zuo Z., Cao J.*, Hu W., Shi C., Wang X., Yao S., Luo B. (2022) Characterizing the maturity of highly evolved organic matter based on aromatic hydrocarbons and optimization with pyrobitumen reflectance and Raman spectral parameters. Science China Earth Sciences, https://doi.org/10.1007/s11430-022-9955-7

[50] Qiu Y., Wang X.*, Lu J., Chou I-M., Wan Y., Zhang R., Zhang W., Sun R. (2022) In situ observations of tungsten speciation and partitioning behavior during fluid exsolution from granitic melt. Sci. Bull., 67: 2358-2368, doi: https://doi.org/10.1016/j.scib.2022.10.024

[49] Sun F., Hu W., Cao J., Wang X., Zhang Z., Ramezani J., Shen S. (2022) Sustained and intensified lacustrine methane cycling during Early Permian climate change. Nature Communications, 13(1): 4856

[48] Zuo Z., Cao J., Wang X., Luo B., Zhong Y., Li K., Hu K. (2022) Characterizing maturity of reservoir pyrobitumen with strong anisotropy: A calibration between reflectance and laser Raman spectral parameters. AAPG Bulletin, 106: 1373-1401.

[47] Wang X.*, Hu W., Qiu Y., Liu Y., Jia D., Cao J., Liu X., Li Y.* (2022) Fluid inclusion evidence for extreme overpressure induced by gas generation in sedimentary basins. Geology, 50: 765-770. Doi: 10.1130/G49848.1

[46] Wu H., Hu W., Wang Y., Tao K., Tang Y., Cao J., Wang X., Kang X. (2021) Depositional conditions and accumulation models of tight oils in the middle Permian Lucaogou Formation in Junggar Basin, northwestern China: New insights from geochemical analysis. AAPG Bulletin, 105(12): 2477-2518.

[45] Yang S., Hu W.*, Wang X., Fan J. (2021) Nitrogen isotope evidence for a redox-stratified ocean and eustasy-driven environmental evolution during the Ordovician-Silurian transition. Global and Planetary Change, 207, 103682. https://doi.org/10.1016/j.gloplacha.2021.103682

[44] Wan Y., Chou I-M.*, Wang X.*, Sun X. (2021) Explorations on footprints of salt-rich fluid and salt-depleted fluid immiscibility in hydrothermal systems: Insights from divergent partitioning of sulfate and perchlorate in the ZnSO4-Zn(ClO4)2-H2O system. Chemical Geology, 584: article no. 120520.

[43] Cui H., Zhong R.*, Xie Y., Wang X.*, Chen H. (2021) Melt–Fluid and Fluid–Fluid Immiscibility in Na2SO4–SiO2–H2O System and Its Implications for the Formation of Rare Earth Deposits. Acta Geologica Sinica (English Edition), 10.1111/1755-6724.14795.

[42] Wan Y., Wang X*, Chou I-M.*, Li X. (2021) Role of sulfate in the transport and enrichment of REE in hydrothermal systems. Earth and Planetary Science Letters, 569: article no. 117068.

[41] Yu Y., Hu W.*, Chou I-M., Jiang L., Wan Y., Li Y., Xin Y., Wang X.* (2021) Species of sulfur in sour gas reservoir: Insights from in situ Raman spectroscopy of S-H2O-CH4-H2O system and its subsystems from 20 to 250 C. Geofluids, 2021: 6658711

[40] Qiu Y., Zhang R., Chou I-M., Wang X.*, Hu W., Zhang W., Lu J., Li G., Li Z. (2021) Boron-rich ore-forming fluids in hydrothermal W-Sn deposits from South China: insights from in situ Raman spectroscopic characterization of fluid inclusions. Ore Geology Reviews, 132: 104048 https://doi.org/10.1016/j.oregeorev.2021.104048

[39] Xie D., Yao S.*, Cao J., Hu W., Wang X., Zhu N. (2021) Diagenetic alteration and geochemical evolution during sandstones bleaching of deep red-bed induced by methane migration in petroliferous basins. Marine and Petroleum Geology, 127: 104940

[38] Yang S., Hu W.*, Wang X. (2021) Mechanism and implications of upwelling from the late Ordovician to early Silurian in the Yangtze region, South China. Chemical Geology, 565: 120074. DOI:10.1016/j.chemgeo.2021.120074

[37] Kang X., Hu W., Tan J., Li Z., Xiang B., Wang J., Wang X. (2021) Hydrogen isotopic responses to thermochemical oxidation of light hydrocarbon gases in deep clastic reservoirs of the Junggar Basin, China. Chemical Geology, 563: 120052.

[36] Sun F., Hu W., Wu H., Fu B., Wang X., Tang Y., Cao J., Yang S., Hu Z. (2021) Two-stage mineral dissolution and precipitation related to organic matter degradation: Insights from in situ C–O isotopes of zoned carbonate cements. Marine and Petroleum Geology, 124: article no. 104812

[35] Wang X.*, Wan Y., Chou I-M. (2021) Fate of sulfate in seafloor hydrothermal systems: Insights from in situ observation of the liquid-liquid phase separation in hydrothermal fluids. Solid Earth Sciences,  https://doi.org/10.1016/j.sesci.2020.12.001

[34] Wan Y., Bourdet J., Hu W., Kang X., Heath C., Qiu Y., Gao W., Wang X*. (2021) Experimental investigation on the thermochemical oxidation of n-alkane and alcohol compounds by MnO2 and Fe2O3 at temperatures up to 325 C. Chemical Geology, 559: article no. 119982. 

[33] Sun F., Hu W.*, Wang X., Cao J., Fu B., Wu H., Yang S. (2021) Methanogen microfossils and methanogenesis in Permian lake deposits. Geology, 49: 13-18.

[32] Wang X.*, Qiu Y., Chou I-M., Zhang R., Li G., Zhong R. (2020) Effects of pH and salinity on the hydrothermal transport of tungsten: Insights from in situ Raman spectroscopic characterization of K2WO4-NaCl-HCl-CO2 solutions at temperatures up to 400 C. Geofluids, article ID 2978984, p1-12

[31] Qiu Y., Yang Y., Wang X.*, Wan Y., Hu W., Lu J., Tao G., Li Z., Meng F. (2020) In situ Raman spectroscopic quantification of aqueous sulfate: Experimetal calibration and application to natural fluid inclusions. Chemical Geology, 533: article no. 119447.

[30] Wang X.*, Qiu Y., Lu J., Chou I-M., Zhang W., Li G., Hu W., Li Z., Zhong R.* (2020) In situ Raman spectroscopic investigation of the hydrothermal speciation of tungsten: Implications for the ore-forming process. Chemical Geology, 532: article no. 119299.

[29] Wang L., Hu W.*, Wang X.*, Cao J., Yao S. (2020)  Halogens (Cl, Br, I) geochemistry in Middle Triassic carbonates: Implications for salinity and diagenetic alteration of I/(Ca + Mg) ratios. Chemical Geology, 533: article no. 119444.

[28] Qiu Y., Wang X.-L.*, Liu X., Cao J., Liu Y.-F., Xi B.-B., Gao W.-L. (2020) In situ Raman spectroscopic quantification of CH4-CO2 mixture: application to fluid inclusions hosted in quartz veins from the Longmaxi shales in Sichuan Basin, southwestern China. Petroleum Science, 17: 23 - 25 (Cover article).

[27] Chang C.*, Hu W., Wang X., Huang K.-J., Yang A., Zhang X. (2019) Nitrogen isotope evidence for an oligotrophic shallow ocean during the Cambrian Stage 4. Geochim. Cosmochim. Acta, 257: 49 - 67.

[26] Yang S., Hu W.*, Wang X., Jiang B., Yao S., Sun F., Huang Z., Zhu F. (2019) Duration, evolution, and implications of volcanic activity across the Ordovician-Silurian transition in the Lower Yangtze region, South China.Earth Planet. Sci. Lett., 518: 13 - 25.

[25] Hu W.-X., Kang X., Cao J., Wang X.-L., Fu B., Wu H.-G. (2018) Thermochemical oxidation of methane induced by high-valence metal oxides in a sedimentary basin. Nature Commumications, 2018(9): 5131.  

[24] Hu W.*, Wang X., Zhu D., You D., Wu H. (2018) An overview of types and characterization of hot fluids associated with reservoir formation in petroliferous basins. Energy Exploration & Exploitation, 36: 1359 – 1375.

[23] Chang C., Hu W., Fu Q., Cao J., Wang X., Wan Y., Yao S. (2018) Characteristics and formation processes of (Ba, K, NH₄)-feldspar and cymrite from a lower Cambrian black shale sequence in Anhui Province, South China. Mineralogical Magazine, DOI: https://doi.org/10.1180/minmag.2017.081.017.

[22] Wang X.*, Song Y., Chou I-M.*, Qiu Y. (2018) Raman spectroscopic characterization of cracking and hydrolysis of n-pentane and n-octadecane at 300 - 375 C with geological implications.Energy Exploration & Exploitation, doi: 10.1177/0144598717748762.

[21] Chang C., Hu W., Wang X., Yu H., Yang A., Cao J., Yao S. (2017) Carbon isotope stratigraphy of the lower to middle Cambrian on the eastern Yangtze Platform, South China. Palaeogeography, Palaeoclimatology, Palaeoecology 479, 90-101

[20] Wu H., Hu W., Tang Y., Cao J.,Wang X., Wang Y., Kang X. (2017) The impact of organic fluids on the carbon isotopic compositions of carbonate-rich reservoirs: case study of the Lucaogou Formation in the Jimusaer Sag, Junggar Basin, NW China. Marine and Petroleum Geology85, 136-150.

[19] Wan Y.,Wang X.*, Chou I-M., Hu W., Zhang Y., and Wang X. (2017) An Experimental Study of the Formation of Talc through CaMg(CO3)2–SiO2–H2O Interaction at 100–200°C and Vapor-Saturation Pressures. Geofluids, 3942826, 1-14. doi:10.1155/2017/3942826.

[18] Wan Y., Wang X.*, Hu W., Chou I-M., Wang X., Chen Y., Xu Z. (2017) In situ optical and Raman spectroscopic observations of the effects of pressure and fluid composition on liquid–liquid phase separation in aqueous cadmium sulfate solutions (
400
C, 50 MPa) with geological and geochemical implications. Geochimica et Cosmochimica Acta 211, 133-152.

[17] Wang X.*, Wang X., Chou I-M., Hu W., Wan Y., and Li Z. (2017) Properties of lithium under hydrothermal conditions revealed by in situ Raman spectroscopic characerization of Li2O-SO3-H2O(D2O) systmes at temperatures up to 420 C. Chemical Geology 451, 104-115.

 [16] Wang X., Wang X.*, Hu W., Wan Y., Cao J., Lv C., Wang R., Cui M. (2017) Supercritical CO2-involved water-rock interactions at 85 C and partial pressures of 10-20 MPa: Sequestration and enhanced oil recovery. Energy Exploration & Exploitation, 35(2): 237-258.

[15] WangX.*, Wan Y., Hu W., Chou I-M., Cao J., Wang X., Wang M. and Li Z. (2016) In situ observations of liquid–liquid phase separation in aqueous ZnSO₄ solutions at temperatures up to 400° C: Implications for Zn²⁺–SO₄²⁻ association and evolution of submarine hydrothermal fluids. Geochimica et Cosmochimica Acta 181, 126-143.

[14] WangX.*, Chou I.M., Hu W., Yuan S., Liu H., Wan Y. and Wang X. (2016) Kinetic inhibition of dolomite precipitation: Insights from Raman spectroscopy of Mg²⁺–SO₄²⁻ ion pairing in MgSO₄/MgCl₂/NaCl solutions at temperatures of 25 to 200° C. Chemical Geology 435, 10-21.

[13] WangX.*, Wan Y., Hu W., Chou I-M., Cai S., Lin N., Zhu Q. and Li Z., (2016) Visual and in situ Raman spectroscopic observations of the liquid–liquid immiscibility in aqueous uranyl sulfate solutions at temperatures up to 420° C. The Journal of Supercritical Fluids 112, 95-102.

[12] Wu H., Hu W., Cao J., Wang X., Wang X., Liao Z. (2016) A unique lacustrine mixed dolomitic-clastic sequence for tight oil reservoir within the middle Permian Lucaogou Formation of the Junggar Basin, NW China: Reservoir characteristics and origin. Marine and Petroleum Geology 76, 115-132.

[11] Chang C., Hu W., Fu Q., Cao J., Wang X. and Yao S. (2016) Characterization of trace elements and carbon isotopes across the Ediacaran-Cambrian boundary in Anhui Province, South China: Implications for stratigraphy and paleoenvironment reconstruction. Journal of Asian Earth Sciences 125, 58-70.

[10] Liao Z., Hu W., Cao J., Wang X., Yao S. and Wan Y. (2016) Permian–Triassic boundary (PTB) in the Lower Yangtze Region, southeastern China: A new discovery of deep-water archive based on organic carbon isotopic and U–Pb geochronological studies.Palaeogeography, Palaeoclimatology, Palaeoecology 451, 124-139.

[9] Liao Z., Hu W., Cao J., Wang X., Yao S., Wu H. and Wan Y. (2016) Heterogeneous volcanism across the Permian–Triassic Boundary in South China and implications for the Latest Permian Mass Extinction: New evidence from volcanic ash layers in the Lower Yangtze Region. Journal of Asian Earth Sciences 127, 197-210

[8] Wan Y., WangX.*, Hu W. and Chou I-M. (2015) Raman Spectroscopic Observations of the Ion Association between Mg²⁺ and SO₄^2– in MgSO₄-Saturated Droplets at Temperatures of ≤ 380° C. The Journal of Physical Chemistry A 119, 9027-9036.

[7] Wang L., Hu W.*, Wang X., Cao J., Chen Q., Seawater normalized REE patterns of dolomite in Geshan and Panlongdong sections, China: Implications for tracing dolomitization and diagenetic fluids, Marine and Petroleum Geology, 2014, 56: 63-73

[6] Yuan S., Chou I.-M., Burruss R.C.,Wang X., and Li J. (2013) Disproportionation and thermochemical sulfate reduction reactions in S-H2O-CH4 and S-D2O-CH4 systems from 200 to 300 C. Geochimica et Cosmochimica Acta118, 263-275. 

[5] Wang X.*, Hu W., and Chou I.-M. (2013) Raman spectroscopic characterization on the OH stretching bands in NaCl-Na2CO3-Na2SO4-CO2-H2O systems: Implications for the measurement of chloride concentrations in fluid inclusions. Journal of Geochemical Exploration132, 111-119.

[4] Wang X.*,  Chou I.-M., Hu W., and Burruss R.C. (2013) In-situ observations of liquid-liquid phase separation in aqueous MgSO4 solutions. Geochimica et Cosmochimica Acta103, 1-10.

[3] Wang X.*,  Chou I.-M., Hu W., Burruss R.C., Sun Q. and Song Y. (2011) Raman spectroscopic measurements of CO2 density: Experimental calibration with high-pressure optical cell (HPOC) and fused silica capillary capsule (FSCC) with application to fluid inclusion observations. Geochimica et Cosmochimica Acta75, 4080-4093.

[2] Wang X.,  Hu W., Yao S., Chen Q. and Xie X. (2011) Carbon and strontium isotopes and global correlation of Cambrian Series 2-Series 3 carbonate rocks in the Keping area of the northwestern Tarim Basin, NW China. Marine and Petroleum Geology28, 992-1002.

[1] Wang X.,Jin Z., Hu W., Zhang J., Qian Y., Zhu J. and Li Q. (2009) Using in situ REE analysis to study the origin and diagenesis of dolomite of Lower Paleozoic, Tarim Basin. Science in China Series D-Earth Sciences 52, 681-693.

**************************************************************************************************************

(B) 中文核心期刊论文

[25] 杨源显, 陈强路, 丘靥, 尤东华, 王小林* . 方解石与含硅流体的水-岩反应实验及其对“硅化”碳酸盐岩"储层成因的启示. 高校地质学报, 2021, 27(2): 218 - 228.

[24] 丘靥，王小林*，陆建军，胡文瑄，万野，高婉露，李真. 基于原位拉曼光谱分析揭示热液条件下钨的迁移方式. 地球化学, 2020, 49(4): 435-449.

[23] 高婉露, 王小林*, 丘靥, 席斌斌, 杨源显, 郑建帆, 曾世豪, 张婧玥, 李真. C-H-O-N体系挥发分的拉曼定量分析: 压力、温度和流体组成的影响. 地球化学, 2020, 49(2): 121-140

[22] 刘显, 陈强路, 王小林*，丘靥, 杨源显. 方解石晶体定向性对水的拉曼光谱影响的实验评估—天然包裹体盐度的测定. 南京大学学报(自然科学版), 2020, 56(3): 297-307

[21] 杨源显, 王小林*, 席斌斌, 丘靥, 高婉露, 万野, 李真. 应用拉曼光谱定量分析流体中硫酸盐质量摩尔浓度: 内标选择和流体组分对分析结果的影响. 地球化学, 2019, 48(4): 403 - 419.

[20] 王小林*, 万野, 胡文瑄, 尤东华, 曹剑, 朱东亚, 李真 . 白云石与富硅流体的水—岩反应实验及其储层地质意义. 地质论评, 2017, 63(6): 1639-1652.

[19] 王晓宇, 王小林*, 万野, 胡文瑄. 一种新的热台温度校准方法: 硫酸盐—水体系液—液相分离原位观测. 地球化学, 2017, 46(4), 319-332.

[18] 王小林*, 胡文瑄, 张军涛, 朱井泉, 万野.塔里木盆地和田1井中寒武统膏岩层段发现原生白云石, 地质论评, 2016, 62(2) : 419-433

[17] 廖志伟, 胡文瑄, 王小林, 曹剑, 姚素平和万野. 下扬子PTB界线深水相区粘土岩的火山成因研究及对LPME的指示意义. 地质学报90(4), 785-800. 

[16] 胡文瑄*，朱井泉，王小林，由雪莲，何凯，塔里木盆地柯坪地区寒武系微生物白云岩特征、成因及意义，石油与天然气地质，2014，35(6): 860-869

[15] 王利超，胡文瑄*，王小林，下扬子宜兴葛山三叠系周冲村组白云岩化过程及元素地球化学响应，地球化学，2014，43(3): 255-266

[14] 张军涛*，胡文瑄，王小林，塔里木盆地寒武系鞍状白云石孔隙充填物差异与成因，沉积学报，2013，32(2): 253-259

[13] 王小林，胡文瑄，李庆，朱井泉. (2011) 塔里木盆地蓬莱坝剖面寒武系第二统-第三统界线处碳同位素负异常及其地质意义.地质论评 57(1), 16-23.

[12] 张军涛，胡文瑄，王小林，钱一雄，吴世祥. (2011) 塔里木盆地西北缘寒武系中热水白云石团块特征及其成因研究. 地质学报85, 234-245.

[11] 王小林，胡文瑄，陈琪，李庆，朱井泉，张军涛. (2010) 塔里木盆地柯坪地区上震旦统藻白云岩特征及其成因机理.地质学报 84, 1479-1494.

[10] 李庆，胡文瑄，张军涛，王小林，朱井泉. (2010) 塔里木盆地西北缘中寒武统硅质岩特征与形成环境. 矿物学报 30, 293-303.

[9] 胡文瑄，陈琪，王小林，曹剑. (2010) 白云岩储层形成演化过程中不同流体作用的稀土元素判别模式. 石油与天然气地质31, 810-818. 

[8] 王小林，胡文瑄，钱一雄，张军涛，谢小敏，李庆. (2009) 塔里木盆地柯坪地区中寒武统藻白云岩去白云岩化研究.矿物学报 29, 56-62.

[7] 谢小敏，胡文瑄，王小林，钱一雄，张军涛，曹剑，李庆. (2009) 新疆柯坪地区寒武纪-奥陶纪碳酸盐岩沉积旋回的碳氧同位素研究.地球化学38, 75-88. 

[6] 吴仕强，朱井泉，胡文瑄，张军涛，王小林，苏永斌. (2009) 塔里木盆地寒武系-奥陶系白云岩稀土元素特征及其成因意义. 现代地质23, 638-647.

[5] 王小林，胡文瑄，张军涛，钱一雄，朱井泉，吴仕强. (2008) 白云岩物质组分与结构对微孔储集体系形成的制约-以塔里木盆地下古生界白云岩为例。天然气地球科学 19(3), 320-326.

[4] 张军涛，胡文瑄，钱一雄，王小林，谢小敏. (2008) 塔里木盆地白云岩储层类型划分、测井模型及其应用.地质学报82, 380-386. 

    (D) 学术会议论文

[16] Wang X (2017) In situ Raman spectroscopic observation of water-hydrocarbon-mineral interactions. Invited talk in International Forum in Organic-Inorganic Interaction During Hydrocarbon Accumulation, Beijing.

[15] 王小林 (2017) 液—液不混溶与元素迁移、富集. 口头报告, 固体地球科学重点实验室联盟2017年度联合学术委员会, 北京.

[14] 王小林 (2017) 富硅流体与白云石的水—岩反应实验及其储层地质意义. 口头报告, 第六届全国沉积学大会, 南京.

[13] 王小林, 胡文瑄, 万野, 王晓宇 (2016) 热液流体液—液不混溶及其地质意义. 口头报告, 第十八届全国包裹体及流体学术研讨会, 成都.

[12] 王小林 (2014) 硫酸盐—水体系高温相行为原位观测及意义. Invited talk. 三亚.

[11] 王小林, 胡文瑄, I-Ming Chou (2013) MgSO4-H2O体系高温相行为及离子络合作用原位观测与地质意义. 口头报告, 第七届世界华人地质科学研讨会, 成都.

[10] 王小林 (2012) 流体中Mg2+与SO42-的络合形式及其对白云石成因的启示. 口头报告, 第十七届包裹体及地质流体学术研讨会, 杭州.

[9] 王小林, 胡文瑄, 王利超, 张军涛 （2011）塔里木盆地震旦系—寒武系白云岩微生物成因及意义. 口头报告, 白云岩成因及油气储集层研讨会, 北京.

[8] Wang X., Chou I-M., Wan Y. (2017) Effect of pressure on liquid-liquid phase separation of aqueous sulfate solution observed in fused silica capillary tubes at elevated temperatures. Goldschmidt 2017, 2017001495.

[7] Wang X., Hu W., Xie X. (2010) Carbon, oxygen and strontium isotopic compositions of Lower to Middle Cambrian carbonates in the northwestern Tarim Basin, China. Geochimica et Cosmochimica Acta 74, A1108. 

[6] Hu W., Wang X., Li Q. (2010) The primary dolomite of microbial origin in the Late Neoproterozoic algal dolomite, Tarim Basin, China. Geochimica et Cosmochimica Acta 74, A426. 

[5] Zhang J., Hu W., Qian Y., Wang X., Zhu J. (2008) Petrography, geochemistry and origin of cement dolomite in the Lower Paleozoic dolomite of the Central uplift, Tarim Basin. Geochimica et Cosmochimica Acta 72, A15. 

[4] Wang X.L., Hu W.X., Zhang W.L., Zhang J.T. (2007) The composition and texture constraints on micro-porosities of dolomite reservoirs, Tarim Basin, NW China. Geochimica et Cosmochimica Acta71, A1087. 

[3] Hu W., Xie X., Zhang J., Wang X. (2007) Oxygen and Carbon isotope composition and implication of Early Palaeozoic dolomites in Keping, Tarim Basin. Geochimica et Cosmochimica Acta71, A421. 

[2] Zhang J., Hu W., Qian Y., Wang X., Cao J., Zhu J., Li Q., Xie X. (2009) Formation of saddle dolomites in Upper Cambrian carbonates, western Tarim Basin (northwest China): Implications for fault-related fluid flow. Marine and Petroleum Geology26, 1428-1440.

[1] Zhang X., Hu W., Jin Z., Zhang J., Qian Y., Zhu J., Zhu D., Wang X., Xie X. (2008) REE compositions of Lower Ordovician dolomites in Central and North Tarim Basin, NW China: A potential REE proxy for ancient seawater. Acta Geologica Sinica82, 610-621.