蔡春芳--博士生导师 长江大学地环学院楚天学者特聘教授

发布日期:2016/3/1 11:38:13     点击数:5103


   蔡春芳,1966年生于福建省福清市。现为长江大学地环学院楚天学者特聘教授、中科院地质与地球物理研究所研究员、博士生导师、国家杰出青年基金获得者。于19871990年分别获江汉石油学院学士和硕士学位; 2000年获得中科院地质与地球物理所博士学位。

    主要从事塔里木、四川、鄂尔多斯盆地储层/油藏流体(石油、天然气与地层水)与岩石之间相互作用(微生物与热化学硫酸盐作用TSR),以及应用有机硫同位素,来探讨高过成熟烃源岩—油气对比。给出证据显示最稳定的甲烷可以是TSR的主要反应物、阐明了其碳同位素分馏效应,提出TSR过程新产生了硫醇、噻吩和四氢噻吩等有机含硫化合物,研发了烃源岩有机硫含量和同位素测试方法,发现在快速埋藏的盆地中,可以应用未受次生改造的原油及其二苯并噻吩的硫同位素值来进行油—源对比,论证了塔里木盆地塔中古生界发生了穿层的热卤水流动,阐明原油来自寒武系,提出深埋白云岩优质储层形成于早期白云石化和后期TSR导致的硬石膏、白云石溶解作用;发现了铀矿硫酸盐还原细菌成因的微化石、硫和碳同位素证据,阐明其成矿模式;认为寒武纪生物大爆发与深海表层氧化水体扩大有关。

发表第一作者国际SCI论文18篇,三篇被SCI引文>65次,最高116次,H-index14,在国内同行中名列前茅。指导毕业了7名博士、硕博连读研究生(李洪涛、李开开、向雷、姜磊、贺训云、贾连奇、袁余洋)、1名硕士研究生(蔡蹓璐)。这些学生大多在国际著名刊物以第一作者发表了论文。合作指导博士后4人(姜红霞、李开开、姜磊、贾连奇)、博士生(刘玲)、硕士生2人(陈坤、陈双玲)。

学科类别:地质学

研究方向】

1) 沉积盆地不同存在形式硫之间转化及其机理

2) 有机硫/碳氮同位素应用于恢复古环境、生命演化以及高过成熟烃源岩-油气的对比研究;

3)碳酸盐岩中TSR及其他流体—岩石相互作用对有效储层形成与改造机理与油气成藏作用的关系;

4)深埋成岩期, BSRTSR成因的硫化物形成有机含硫化合物的机理及其识别;

5)硫酸盐还原菌降解油气与六价铀还原成矿的关系;

6)生物标志化合物、稳定同位素和流体包裹体在油气勘探和开发中的应用。 

承担科研项目情况:

【主持/主要参加的科研项目】

1.      塔中地区奥陶系硫化氢成因与分布。油田横向课题,2012.10-2014.06

2.      油气盆地硫参与的有机—无机相互作用, 国家杰出青年基金(41125009) , 2012.12015.12

3.      塔里木盆地碳酸盐岩埋藏岩溶储集体形成分布的主控因素与发育规律(2008ZX05008-0032011ZX05008-003), 国家科技重大专项子课题;2008. 62015.12

4.      埃迪卡拉纪-寒武纪过渡时期 富有机质烃源岩的微生物作用(2011CB808805),,国家973子课题; 2011.12015.12

5.      川东二叠-三叠系TSR对储层改造作用及气-源岩对比新方法(40839906),国家自然科学基金重点—中石化联合基金; 2009.1-2012.12

6.      微生物、油气在砂岩型铀矿床形成中的作用(KZCX2-YW-JC102),中科院知识创新工程重要方向项目;2010.1 - 2012.12

7.      “塔中塔北寒武—奥陶系碳酸盐岩流体地球化学与储层形成” 2006CB202304, 国家973项目子课题;2006.102011.10

8.      深埋成岩期有机含硫化合物形成机理(40573034),国家自然科学基金面上,2006.1-2008.12

9.      多种能源矿产共存成藏(矿)中流体—岩石相互作用研究(2003CB214605), 国家973子课题, 2003.12-2007.12

10.   沉积盆地富硫流体:成因、流动与硫酸盐还原作用(40173023),国家自然科学基金面上项目,2001.1-2004.12

11.   烃类的热化学硫酸盐还原作用与硫醇的成因,英国皇家学会Royal Fellowship 2001.1-2002.1

12.   沉积盆地微生物---岩相互作用研究,国家自然科学基金面上(49773198) 1998.1-2000.12

13.   储层中烃类蚀变对成岩作用的影响.,中石油中青年科技创新项目,1996.61999.3

14.   塔里木盆地烃—水—岩相互作用研究(96-111-01-02-07C),.国家95科技攻关项目, 1996-1999.

【获奖及荣誉】

1998年,第一作者论文获湖北省自然科学论文一、二等奖各一篇;

2004年,获全国百篇优秀博士学位论文奖;

2006年,获第十一届侯德封矿物岩石地球化学青年科学家奖

2011年,获得国家杰出青年基金;

2014年,研究成果获湖北省自然科学二等奖,排名第一 

【论著目录】

2015

Cai, C.F., Hu, G.Y., Li, H.X., Jiang, L.,He, W.X., Zhang, B.S., Jia, L.Q., Wang, T.K. Origins and fates of H2S in the Cambrianand Ordovician in Tazhong area: evidence from sulfur isotopes, fluid inclusionsand production data. Marine and Petroleum Geology, 2015c, 67, 408-418.

Cai, C.F., Zhang, C.M., Worden, R.H., Wang,T.K., Li, H.X., Jiang, L., Huang S.Y., Zhang, B.S. Application of sulfur andcarbon isotopes to oil–source rock correlation: A case study from the Tazhongarea, Tarim Basin, China. Organic Geochemistry, 2015b, 83-84,140-152.

Cai, C.F., Xiang, L., Yuan, Y.Y., He, X.Y.,Chu, X.L., Chen, Y., Xu, C.L. Marine C, S and N biogeochemical processes in theredox-stratified Early Cambrian Yangtze ocean. Journal of the GeologicalSociety (London). 2015a, 172 (3), 390-406.

Jiang, L., Cai, C.F., Worden, R.H., Li,K.K., Xiang, L., Chu, X.L., Shen, A.J., Li, W.J. Rare earth element and yttrium(REY) geochemistry in carbonate reservoirs during deep burial diagenesis:Implications for REY mobility during thermochemical sulfate reduction. ChemicalGeology, 2015, 415, 87–101.

Jiang, L., Worden, R.H., Cai, C.F.Generation of isotopically and compositionally distinct water duringthermochemical sulfate reduction (TSR) in carbonate reservoirs: TriassicFeixianguan Formation, Sichuan Basin, China. Geochimica et Cosmochimica Acta,2015, 169, 249-262.

Jiang, L., Pan, W., Cai, C.F., Jia, L.Q.,Pan, L., Wang, T.K., Li, H. X., Chen, S. L., Chen, Y. Fluid mixing induced byhydrothermal activity in the ordovician carbonates in Tarim Basin, China.Geofluids, 2015, 169, 249-262.

Jia, L.Q., Cai, C.F., Yang, H., Li, H.X.,Wang, T., Zhang, B., Jiang, L., Tao, X.W. Thermochemical and bacterial sulfatereduction in the Cambrian and Lower Ordovician carbonates in the Tazhong Area,Tarim Basin, NW China: Evidence from fluid inclusions, C, S and Sr isotopicdata. Geofluids, 2015, 15, 421–437.

2014

Wang, Z.M., Cai, C.F., Li, H. X., Yang,H.J., Wang, T.K., Zhang, K., Jia, L.Q., Chen, K. Origin of late charged gas andits effect on property of oils in the Ordovician in Tazhong area. Journal ofPetroleum Science and Engineering, 2014, 122, 83-93.

Cai, C.F., He, W.X., Jiang, L., Li, K.K.,Xiang, L., Jia, L.Q. Petrological and geochemical constraints on porositydifference between Lower Triassic sour- and sweet-gas carbonate reservoirs inthe Sichuan Basin. Marine and Petroleum Geology, 2014, 56, 34-50.

Jiang, L., Worden, R.H., Cai, C.F., Li,K.K., Xiang, L., Cai, L.L., He, X.Y. Dolomitization of gas reservoirs: theUpper Permian Changxing and Lower Triassic Feixianguan Formations, northeastSichuan Basin, China. Journal of Sedimentary Research, 2014, 84, 792-815.

Jiang, L., Worden, R.H., Cai, C.F.Thermochemical sulfate reduction and fluid evolution of the Lower TriassicFeixianguan Formation sour gas reservoirs: Northeast Sichuan Basin, China,American Association of Petroleum Geologists Bulletin, 2014, 98, 947-973.

Li, K.K., Cai, C.F., Hou, D.J., He, X.Y.,Jiang. L., Jia, L.Q., Cai, L.L., 2014. Origin of high H2S concentrations in theUpper Permian Changxing reservoirs of the Northeast Sichuan Basin, China.Marine and Petroleum Geology 57233-243.

Li, K.K., Cai, C.F., Jia, L.Q., Gao, Y.,Jiang, Z., Wang, T.K., Jiang, L., 2014. The role of thermochemical sulfatereduction in the genesis of high-quality deep marine reservoirs within thecentral Tarim Basin, western China. Arabian Journal of Geosciences, 1-14.

Yuan, Y.Y., Cai, C.F., Wang, T.K., Xiang,L., Jia, L.Q., Chen, Y., 2014. Deep-water basin redox conditions duringEdiacaran-Cambrian transition period in the Lower Yangtze, South China: Casestudy of iron speciation and δ13Corg in Diben Section, Zhejiang province.Chinese Science Bulletin72, 1-139.

2013

Cai, C.F., Zhang, C.M., He, H., Tang, Y.J.,2013. Carbon isotope fractionation during methane-dominated TSR in East SichuanBasin gas fields, China: A review. Marine and Petroleum Geology 48, 100-110.

Jiang, L., Cai, C.F., Worden, R.H., Li,K.K., Xiang, L., 2013. Reflux dolomitization of the Upper Permian ChangxingFormation and the Lower Triassic Feixianguan Formation, NE Sichuan Basin,China. Geofluids 13, 232-245.

贺训云, 蔡春芳, 姚根顺, 熊湘华, 沈安江, 向雷, 吴敬武, 2013. 黔南坳陷油苗来源: , 硫同位素及生物标志物证据. 岩石学报 29(3): 1059-1072.

2012

Li, K.K., Cai, C.F., Jiang, L., Cai, L.L.,Jia, L.Q., Zhang, B., Xiang, L., Yuan, Y.Y., 2012. Sr evolution in the UpperPermian and Lower Triassic carbonates, Northeast Sichuan Basin, China:constraints from chemistry, isotope and fluid inclusions. Applied Geochemistry27, 2409- 2424.

Jiang, L., Cai, C.F., Zhang, Y.D., Mao,S.Y., Sun, Y.G., Li, K.K., Xiang, L., Zhang, C.M., 2012. Lipids ofsulfate-reducing bacteria and sulfur-oxidizing bacteria found in the Dongshenguranium deposit. Chinese Science Bulletin 57, 1311-1319.

蔡春芳, 蔡镠璐, 张俊, 蔡勋育, 李开开, 2012. 川东北飞仙关组甲烷为主的 TSR 及其同位素分馏作用. 岩石学报 28(3): 889-894.

李开开, 蔡春芳, 蔡镏璐, 姜磊, 向雷, 2012. 塔河地区中下奥陶统储层硫化物成因分析. 岩石学报 28(3): 806-814.

向雷, 蔡春芳, 贺训云, 姜磊, 2012. 贵州渣拉沟剖面下寒武统黑色硅质岩微量元素富集机制. 岩石学报 28(3): 971-980.

杨海军, 李开开, 潘文庆, 肖中尧, 蔡春芳, 2012. 塔中地区奥陶系埋藏热液溶蚀流体活动及其对深部储层的改造作用. 岩石学报 28(3): 783-792.

张俊, 蔡镠璐, 向雷, 蔡春芳, 2012. 川东北地区飞仙关组成岩晚期白云石溶解作用. 石油与天然气地质 33(4): 599-606.

2011

Li, K.K., Cai, C.F., He, H., Jiang, L.,Cai, L.L., Xiang, L., Huang, S.J., Zhang, C.M., 2011. Origin of palaeo-watersin the Ordovician carbonates in Tahe oilfield, Tarim Basin: constraints fromfluid inclusions and Sr, C and O isotopes. Geofluids 11, 71-86.

Zhang, C.M., Zhang, Y.Q., Cai, C.F., 2011.Maturity effect on carbazole distributions in source rocks from the salinelacustrine settings, the western Qaidam Basin, NW China. Journal of Asian EarthSciences 42, 1288-1296.

Zhang, C.M., Zhang, Y.Q., Cai, C.F., 2011.Aromatic isoprenoids from the 25-65 Ma saline lacustrine formations in thewestern Qaidam Basin, NW China. Organic Geochemistry 42, 851-855.

2010

Cai, C.F., Li, K.K., Zhu, Y.M., Xiang, L.,Jiang, L., Tenger, Cai, X.Y., Cai, L.L., 2010. TSR origin of sulfur in thePermian and Triassic reservoir bitumen in East Sichuan Basin, China. OrganicGeochemistry 41 871-878.

2009

Cai, C.F., Zhang, C.M., Cai, L.L., Wu,G.H., Jiang, L., Xu, Z.M., Li, K.K., Ma, A.L., Chen, L.X., 2009c. Origins ofPalaeozoic oils in the Tarim Basin: Evidence from sulfur isotopes andbiomarkers. Chemical Geology 268197-210.

蔡春芳, 李开开, 李斌, 蔡镠璐, 姜磊,2009b.塔河地区奥陶系碳酸盐岩缝洞充填物的地球化学特征及其形成流体分析. 岩石学报 25(10), 2399-2404.

Cai, C.F., Li KK., Ma, A.L., Zhang, C.M.,Xu, Z.M., Worden, R.H., Wu, G.H., Zhang, B.S., Chen, L.X., 2009a. DistinguishingCambrian from Upper Ordovician source rocks: Evidence from sulfur isotopes andbiomarkers in the Tarim Basin. Organic Geochemistry 40, 755-768.

Cai, C.F., Li KK.,Jiang,L., Cai, L.L. 2009.Reservoir porosity enhancement by multiple stages of TSR in East Sichuan Basingas fields, China. Geochimica Cosmochimi Acta 73, Axxx.

2008

Cai, C.F., Li, KK, Li, H.T., Zhang, B.S.,2008.Evidence for cross formational hot brine flow from integrated 87Sr/86Sr,REE and fluid inclusions of the Ordovician veins in Central Tarim. AppliedGeochemistry 23, 2226-2235.

Cai, C.F., Li KK., 2008. Secular change indelta S-34 value of early palaeozoic kerogens from the Tarim Basin relative tomarine sulphates. Geochimica Cosmochimi Acta 72 (12), A128.

蔡春芳, 李宏涛,李开开,姜磊,2008. 油气厌氧氧化与铀还原的耦合关系-以东胜和钱家店铀矿床为例。 石油实验地质, 305),518-521.

李开开,蔡春芳,蔡镠鏴,2008. 塔中地区上奥陶统热液流体与热化学硫酸盐还原作用.石油与天然气地质,229):217222

Zhang CM, Zhang YQ, Zhang M, Chen ZY, PengDH, Sun WL, Cai, C.F., 2008. Compositional variabilities among crude oils fromthe southwestern part of the Qaidam Basin, NW China. Journal of PetroleumScience and Engineering 62, 87-92.

Zhang CM, Zhang YQ, Zhang M, Zhao HJ, Cai,C.F., 2008. Carbazole distributions in rocks from non-marine depositionalenvironments. Organic Geochemistry39, 868-878.

Jiang HX, Wu YS, Cai, C.F., 2008.Filamentous cyanobacteria fossils and their significance in thePermian-Triassic boundary section at Laolongdong, Chongqing. Chinese ScienceBulletin 53,1871-1879.

2007

Cai, C.F., Li, KK, Li, H.T., 2007. Evidencefor cross formation hot brine flow from integrated 87Sr/86Sr and REE data inCentral Tarim. Geochimica Cosmochimi Acta A139-A139 (SCI).

Cai, C.F., Li, KK, Li, H.T., 2007. Fluidinclusion and isotopic constraint for fluid evolution in the Ordovician veinsin Central Tarim, NW China. In: Bullen, T.D. and Wang, Y.C. (eds.), Water-RockInteraction, Taylor & Francis Group, London. p. 703-707.

蔡春芳,2007. 油气藏中热化学和微生物硫酸盐还原作用。矿物岩石地球化学通报,26 卷(增),pp. 260-262

蔡春芳、邬光辉、李开开、陈利新、李梅、李宏涛,2007. 塔中地区古生界热化学硫酸盐还原作用与原油中硫的成因。矿物岩石地球化学通报26(1), 44-48.

Cai, C.F., Li, H.T., Qin, MK., Luo, XR.,Wang, F.Y., Ou, G.X., 2007. Biogenic and petroleum-related ore-formingprocesses in Dongsheng uranium deposit, NW China. Ore Geology Reviews 32,262-274.PDF

Cai, C.F., Dong, H.L., Li, H.T., Xiao,X.K., Ou, G.X., Zhang, C.M., 2007. Mineralogical and geochemical evidence forcoupled bacterial uranium mineralization and hydrocarbon oxidation in theShashagetai deposit, NW China. Chemical Geology 236, 167-179.PDF

Wei, ZB, J. Moldowan, JM, Fago, F.,Dahl,J.E., Cai, C.F. and Peters, K.E., 2007. Origins of Thiadiamondoids andDiamondoidthiols in Petroleum. ASAP Energy Fuels, 21 (6): 3431-3436.

Zhang, CM, Zhao, H., Hu, M., Xiao, Q., Li,J., Cai, C.F., 2007. A simple correlation for the viscosity of heavy oils fromLiaohe Basin, NE China. Source. Journal of Canadian Petroleum Technology 46(4),8-11.

Li, HT, Cai, CF, He, H., Li,K.K.., 2007.Microbial uranium mineralization and hydrocarbon oxidation in the Qianjiadiandeposit, NE China. Geochimica Cosmochimi Acta 71, A570-A570.

Li, HT, Cai, CF, Li, KK, Luo, X.R., 2007.Biogenic spherical magnetite and coffinite from sandstone-type uranium depositin Dongsheng area. In: Bullen, T.D. and Wang, Y.C. (eds.), Water-RockInteraction, Taylor & Francis Group, London. p. 881-885.

李开开、蔡春芳、李宏涛,2007. 塔中奥陶系稀土元素与87Sr/86Sr分布及其意义。矿物岩石地球化学通报,26 卷(增),pp. 296-298

李宏涛、蔡春芳、李开开、罗晓容,2007.东胜砂岩型铀矿床低温微生物成矿模式探讨. 矿物岩石地球化学通报,26 卷(增),pp. 292-293

李宏涛、蔡春芳、李开开、罗晓容, 2007. 内蒙古东胜铀矿床球状磁铁矿的成因及意义. 地质论评,53(4), 564-570.

李宏涛、蔡春芳、罗晓容、李开开,2007. 鄂尔多斯北部直罗组中烃类包裹体地球化学特征及来源分析. 沉积学报253467-473.

李宏涛、蔡春芳、罗晓容、孙希勇, 2007. 内蒙古东胜地区中侏罗统砂岩沉积物源的地球化学证据. 地质科学, 42(2), 353-361.

2006

Worden, R.H., Cai, C.F., 2006. Discussion:Geochemical characteristics of the Zhaolanzhuang sour gas accumulation andthermochemical sulfate reduction in the Jixian Sag of Bohai Bay Basin by Zhanget al. (Organic Geochemistry 36, 1717-1730). Organic Geochemistry 37, 511-514.

Cai, C.F., Peng, L.C., Mei, B.W., Xiao,Y.K., 2006. B, Sr, O and H isotopic compositions of formation waters from theBachu Bulge, Tarim Basin. Acta Geological Sinica 80(4): 550-556.

2005

蔡春芳、李宏涛. 2005. 沉积盆地热化学硫酸盐还原作用评述. 地球科学进展,20(5), 14-19.

Cai, C.F., Hu, GY, He, H., Li, J, Li, JF,Wu, Y. S., 2005. Geochemical characteristics and origin of natural gas andthermochemical sulfate reduction in Ordovician carbonates in the Ordos Basin,China. Journal of Petroleum Science and Engineering 48(3/4), 209-226.

Cai, C.F., Worden, R. H., Wolff, G. A.,Bottrell, S. H., Wang, D.L., Li, X., 2005. Origin of sulfur rich oils and H2Sin Tertiary lacustrine sections of the Jinxian Sag, Bohai Bay Basin, China.Applied Geochemistry 20, 1427-1444.

2004

Cai, C.F., He, H., Mei, B.W.,Xiao,Y.K.,2004, Origin of brines from the Bachu Uplift, Tarim Basin, China:chemistry and d11B evidence. In: Wanty RB and Seal RR (Eds.), Water-RockInteraction 2004. London: Taylor and Francis Group, pp. 367-372

Cai, C.F., Xie, Z.Y., Worden, R.H., Hu,G.Y., Wang, L. S., He, H., 2004, Methane-dominated thermochemical sulphatereduction in the Triassic Feixianguan Formation East Sichuan Basin, China:towards prediction of fatal H2S concentrations. Marine and Petroleum Geology 21,1265-1279

向廷生、万家云、蔡春芳, 2004. 硫酸盐还原菌对原油的降解作用和硫化氢的生成. 天然气地球科学,15(2):171-173

向廷生、蔡春芳、付华娥, 2004. 不同温度、羧酸溶液中长石溶解模拟实验. 沉积学报22, 597-602.

2003

Cai, C.F., Worden, R. H., Bottrell, S. H.,Wang, L.S., and Yang, C.C., 2003. Thermochemical sulphate reduction and thegeneration of hydrogen sulphide and thiols (mercaptans) in Triassic carbonatereservoirs from the Sichuan Basin, China. Chemical Geology 202, 39-57.

2002

Cai, C.F., Worden, R. H., Wang, Q. H.,Xiang, T. S., Zhu, J. Q., Chu, X. L, 2002. Chemical and isotopic evidence forsecondary alteration of natural gases in the Hetianhe Field, Bachu Uplift ofthe Tarim Basin. Organic Geochemistry 33, 1415-1427.

2001

Cai, C.F., Wang, J. Y., Zeng, F. G. and He,H., 2001. Origin, migration and mixing of oilfield brines: Stable isotopicevidence from Kuqa Foreland Basin. Science in China Series E 44, 175-180.

Cai, C.F., Hu, W. S., Worden, R. H., 2001.Thermochemical sulphate reduction in Cambro-Ordovician carbonates in CentralTarim. Marine and Petroleum Geology 18, 729-741.

Cai, C.F., Franks, S. G. and Aagaard, P.,2001. Origin and migration of brines from Paleozoic strata in Central Tarim,China: constraints from 87Sr/86Sr, δD, δ18O and water chemistry. AppliedGeochemistry 16, 1269-1283.

Cai, C.F., He, H. and Xiang, T. S., 2001.Isotope evidence for the origin and mixing of brines from Kuqa Basin, China.In: Cidu, R. (Ed), The proceedings of the 10th Water-Rock Interactioninternational symposium on water-rock. A. A. Blackema, Lisse, 1493-1496.

蔡春芳、顾家裕、蔡洪美,2001. 塔中地区志留系烃类侵位对成岩作用的影响。沉积学报,19(1)60-65.

2000

蔡春芳,2000. 塔中古生界油田水混合和运移的证据. 地球化学 29(5)504-510.

蔡春芳、王国安、何 宏,2000. 库车前陆盆地流体化学、成因与流动. 地质地球化学28(1): 56-60.

1999

蔡春芳,1999. 塔里木盆地油田水87Sr/86Sr的分布及其成因意义. 地球学报 20(增),484-488

1998

Cai, C.F., Mei, B.W., Wang, J.Y., 1998.Fluid-rock interaction: its model and significance in Tarim Basin. China oiland gas 5(4) : 232-234.

蔡春芳、邱利瑞, 1998. 塔里木盆地油田水有机配合物的模拟计算. 新疆石油地质 19(1),32-34,87.

蔡春芳、马振芳、杨贤州, 1998. 圈闭中油气的次生蚀变作用. 中国海上油气(地质),12(2),122-12.

Hu, W. S., Cai, C.F., Wu, Z. Y., Li, J.,1998. Structural style and its relation to hydrocarbon exploration in theSongliao basin, northeast China: Marine and Petroleum Geology, 15(1), 41-55.

曾凡刚、妥进才、李源、蔡春芳,1998. 广西3种褐煤芳烃生物标志物组合特征. 北京大学学报(自然科学版), 34(6):793800.

1997

蔡春芳, 梅博文, 马亭,陈传平,李伟,刘常青,1997. 塔里木盆地流体-岩石相互作用研究。北京:地质出版社,155p. (专著)

Cai, C.F., Mei, B., Li, W., Zeng, F., 1997.Water-rock interaction in Tarim Basin: Constraints from oilfield watergeochemistry. Chinese Journal of Geochemistry 16(4), 289-303.

蔡春芳、博梅文、马 亭等,1997. 塔里木盆地油田水成因与演化.地质论评, 43(4): 650-657.

蔡春芳、博梅文、马 亭等, 1997. 塔里木盆地有机酸来源、分布及对成岩作用的影响.沉积学报, 15(3): 103-109.

蔡春芳、博梅文、李 伟等, 1997. 塔中地区古生界流体运聚和化学演化。石油勘探开发, 24(2)18-21. (EI)

蔡春芳、彭德堂、高振中、关银录、史永苏、李碧宁,1997. 民和盆地上侏罗统湿型冲积扇沉积. 矿物岩石17(2): 61-66.

蔡春芳、彭德堂、高振中、关银录、史永苏、李碧宁,1997. 民和盆地中下侏罗统沉积相分析, 青海地质6(2): 1421.

蔡春芳,1997. 油藏流体连通性水化学指纹分析. 断块油气田,4(2):33-35

蔡春芳,马亭,梅博文,李伟,1997.塔中地区石炭系水文地质与流体非均质性研究.江汉石油学院学报,193):3033

蔡春芳, 1997. 塔里木盆地流体-岩石相互作用及模式. 油气成藏机理及油气资源评价国际研讨会。石油工业出版社,149152

蔡春芳,1997. 水-岩相互作用地球化学模拟研究现状与进展. 油气成藏机理及油气资源评价国际研讨会。石油工业出版社,199-202

张敏、蔡春芳、张俊, 1997. 油气藏中沥青垫的研究进展. 地质科技情报,16(1):8184

曾凡刚、周世新、王关玉、李贤庆、霍永忠、蔡春芳,1997.广西第三系煤系地层油砂的地球化学特征.沉积学报,153):9195.

1996

Cai, C.F., Mei, B.W., Ma, T., Chen, C. P.,Liu C. Q., 1996. Hydrocarbon-water-rock interactions in the diageneticallyaltered system nearby unconformities of Tarim Basin. Chinese Science Bulletin41, 1631-1635.

蔡春芳, 1996. 沉积盆地中流体-岩石相互作用研究的现状. 地球科学进展, 11(6):575579.

蔡春芳、博梅文、马 亭等, 1996. 塔里木盆地油田水文地球化学. 地球化学, 25(6) : 314-323.

蔡春芳、赵红静、马亭、梅博文、方孝林,1996.塔里木盆地轮南地区油田水有机酸与矿物成岩作用.有机地球化学研究进展,重庆大学出版社,140145

蔡春芳、张敏、徐中一、张俊,1996.塔里木盆地储层沥青成因探讨. 有机地球化学研究进展,重庆大学出版社,1420.

1995

蔡春芳、博梅文、马 亭等,1995. 塔里木盆地不整合面附近成岩改造体系烃-水-岩相互作用. 科学通报 40(24): 2253-2256.

蔡春芳、博梅文、马 亭等,1995. 塔北侏罗-三叠系成岩反应。石油天然气地质,1995, 16(3):259-264.

陈传平、梅博文、易绍金、马亭、蔡春芳,1995. 地层水中低分子量有机酸成因分析. 石油学报,16(4):4854.

1994

陈传平、梅博文、马亭、蔡春芳, 1994. 水溶液中硅质絮状沉淀物的实验研究. 石油与天然气地质,15(4):316321.