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个人简介

刘汇川,男,河南开封人,1986年出生,博士(后),副教授,博士生导师。2009年获中国矿业大学学士,2014年获中国科学院广州地球化学研究所博士学位。主要从事构造地质和地球化学相关研究和教学工作,目前发表学术论文29篇,其中以第一和通讯作者发表SCI论文13篇。 【工作经历】 (1)2014/12-2018/09,中山大学地球科学与工程学院,博士后,特聘四级研究员; (2)2018/10至今,中国石油大学(北京)地球科学学院,副教授。 【在研项目】 (1)中国石油大学(北京)优秀青年学者科研启动基金,主持; (2)油气资源与探测国家重点实验室青年人才培育课题,主持; (3)国家自然科学基金青年科学基金项目:滇老泰毗邻区早古生代中基性岩浆岩成因及对原特提斯东缘演化的制约(41502210),主持; (4)中国博士后基金面上项目:蛇绿岩形成过程Re-Os和铂族元素联合示踪(2015M582456),主持; (5)国家自然科学基金联合基金项目:华南陆壳结构与南海北部地质过程研究(U1701641),参与; (6)973项目华南大规模低温成矿作用子课题:华南大规模低温成矿的构造背景(2014CB440901),参与; (7)国家自然科学基金青年科学基金项目:广东二叠-三叠系充填格架、物源示踪及印支构造属性限定(41602232),参与; (8)国家自然科学基金青年科学基金项目:中缅地区高级变质岩始新世变质作用及对碰撞时序约束(41402193),参与;

研究领域

(1)同位素示踪技术在岩浆岩成因、油气成藏和沉积地层”源-汇”系统特征研究中的应用; (2)特提斯洋东南缘单向俯冲过程及陆陆碰撞(硬碰撞)机制; (3)古亚洲洋东南缘古大洋双向俯冲及弧陆碰撞(软碰撞)机制。

近期论文

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(1)Liu,H.C.,Bi,M.W.*,Guo,X.F.,Zhou,Y.Z.,andWang,Y.K.,2019a,PetrogenesisofLateSilurianvolcanisminSWYunnan(China)andimplicationsforthetectonicreconstructionofnorthernGondwana:InternationalGeologyReview. (2)Liu,H.C.,Li,Y.L.*,Wu,L.W.,Huangfu,P.P.,andZhang,M.,2019b,Geochemistryofhigh-Nbbasalt-andesiteintheErgunaMassif(NEChina)andimplicationsfortheearlyCretaceousback-arcextension:GeologicalJournal,v.54,p.291-307. (3)Liu,H.C.,Li,Y.L.*,He,H.Y.,Huangfu,P.P.,andLiu,Y.Z.,2018a,Two-phasesouthwardsubductionoftheMongol-OkhotskoceanicplateconstrainedbyPermian-JurassicgranitoidsintheErgunaandXing'anmassifs(NEChina):Lithos,v.304,p.347-361. (4)Liu,H.C.*,Peng,T.P.,andGuo,X.F.,2018b,GeochronologicalandgeochemicalconstraintsonthecoexistentN-MORB-andSSZ-typeophiolitesinBabuarea(SWChina)andtectonicimplications:JournaloftheGeologicalSociety,v.175,p.667-678. (5)Liu,H.C.*,Wang,Y.J.,Li,Z.H.,Zi,J.W.,andHuangfu,P.P.,2018c,GeodynamicsoftheIndosinianorogenybetweentheSouthChinaandIndochinablocks:InsightsfromlatestPermian-Triassicgranitoidsandnumericalmodeling:GeologicalSocietyofAmericaBulletin,v.130,p.1289-1306. (6)Liu,H.C.*,Xia,X.P.,Lai,C.K.,Gan,C.S.,Zhou,Y.Z.,andHuangfu,P.P.,2018d,Break-awayofSouthChinafromGondwana:InsightsfromtheSilurianhigh-NbbasaltsandassociatedmagmaticrocksintheDiancangshan-Ailaoshanfoldbelt(SWChina):Lithos,v.318–319,p.194–208. (7)Li,Y.L.,Liu,H.C.*,Huangfu,P.P.,He,H.Y.,andLiu,Y.Z.,2018,EarlycretaceouslowercrustalreworkinginNEChina:insightsfromgeochronologyandgeochemistryoffelsicigneousrocksfromtheGreatXing'anrange:InternationalJournalofEarthSciences,v.107,p.1955-1974. (8)Xu,G.,Liu,H.C.*,Li,Y.L.,Xu,Z.,andXie,Y.,2018,EarlyPermianSunidyouqisuprasubduction-zoneophiolitesinthecentralSolonkersuturezone(InnerMongolia,China):GeoscienceFrontiers,v.2018,p.1-11. (9)Wang,Y.J.*,Qian,X.,Cawood,P.A.,Liu,H.C.,Feng,Q.L.,Zhao,G.C.,Zhang,Y.H.,He,H.Y.,andZhang,P.Z.,2018,ClosureoftheEastPaleotethyanOceanandamalgamationoftheEasternCimmerianandSoutheastAsiacontinentalfragments:Earth-ScienceReviews,v.186,p.195-230. (10)Liu,H.C.,Wang,Y.J.*,Cawood,P.A.,andGuo,X.F.,2017a,Episodicslabrollbackandback-arcextensionintheYunnan-Burmaregion:InsightsfromCretaceousNb-enrichedandoceanic-islandbasalt-likemaficrocks:GeologicalSocietyofAmericaBulletin,v.129,p.698-714. (11)Liu,H.C.,Wang,Y.J.*,Guo,X.F.,Fan,W.M.,andSong,J.J.,2017b,LateTriassicpost-collisionalslabbreak-offalongtheAilaoshansuture:insightsfromOIB-likeamphibolitesandassociatedfelsicrocks:InternationalJournalofEarthSciences,v.106,p.1359-1373. (12)Liu,H.C.,Wang,Y.J.*,andZi,J.W.,2017c,PetrogenesisoftheDalongkaiultramafic-maficintrusionanditstectonicimplicationforthePaleotethyanevolutionalongtheAilaoshantectoniczone(SWChina):JournalofAsianEarthSciences,v.141,p.112-124. (13)Wang,Y.J.*,Zhou,Y.Z.,Cai,Y.F.,Liu,H.C.,Zhang,Y.Z.,andFan,W.M.,2016,GeochronologicalandgeochemicalconstraintsonthepetrogenesisoftheAilaoshangraniticandmigmatiterocksanditsimplicationsonNeoproterozoicsubductionalongtheSWYangtzeBlock:PrecambrianResearch,v.283,p.106-124. (14)Liu,H.C.,Wang,Y.J.*,Cawood,P.A.,Fan,W.M.,Cai,Y.F.,andXing,X.W.,2015,RecordofTethyanoceanclosureandIndosiniancollisionalongtheAilaoshansuturezone(SWChina):GondwanaResearch,v.27,p.1292–1306. (15)Fan,W.M.*,Wang,Y.J.*,Zhang,Y.H.,Zhang,Y.Z.,Jourdan,F.,Zi,J.W.,andLiu,H.C.,2015,PaleotethyansubductionprocessrevealedfromTriassicblueschistsintheLancangtectonicbeltofSouthwestChina:Tectonophysics,v.662,p.95-108. (16)Liu,H.C.,Wang,Y.J.*,Fan,W.M.,Zi,J.W.,Cai,Y.F.,andYang,G.L.,2014,PetrogenesisandtectonicimplicationsofLate-TriassichighE>(Nd)(t)-E>(Hf)(t)granitesintheAilaoshantectoniczone(SWChina):ScienceChina-EarthSciences,v.57,p.2181-2194. (17)Cai,Y.F.,Wang,Y.J.*,Cawood,P.A.,Fan,W.M.,Liu,H.C.,Xing,X.W.,andZhang,Y.Z.,2014,NeoproterozoicsubductionalongtheAilaoshanzone,SouthChina:Geochronologicalandgeochemicalevidencefromamphibolite:PrecambrianResearch,v.245,p.13-28. (18)Ma,L.Y.,Wang,Y.J.*,Fan,W.M.,Geng,H.Y.,Cai,Y.F.,Zhong,H.,Liu,H.C.,andXing,X.W.,2014,PetrogenesisoftheearlyEoceneI-typegranitesinwestYingjiang(SWYunnan)anditsimplicationfortheeasternextensionoftheGangdesebatholiths:GondwanaResearch,v.25,p.401-419. (19)Zheng,H.,Huang,Q.T.,Cai,Z.R.,Zhang,K.J.,Liu,H.C.,Li,C.C.,Lu,L.J.,Yang,B.,andYu,S.R.,Inpress,EarlyCretaceousarcgranitoidsfromthecentralLhasasubterrane:ProductionofthenorthwardsubductionofYarlungZangboNeo‐TethyanOcean?:GeochemicalJournal. (20)Huang,Q.T.,Cai,Z.R.,Xia,B.,Li,J.F.,Xia,L.Z.,andLiu,H.C.,2016,Geochronology,geochemistry,andSr-Nd-PbisotopesofCretaceousgranitoidsfromwesternTibet:petrogenesisandtectonicimplicationsfortheevolutionoftheBangongMeso-Tethys:InternationalGeologyReview,v.58,p.95-111. (21)赵国锋,刘汇川*,钱鑫,张爱梅,何景文,何慧莹,王岳军,2018,琼东南晚二叠世Ⅰ型花岗岩成因及其构造指示:地球科学,v.43,p.1321-1332. (22)郭小飞,王岳军,刘汇川*,张玉芝,2017,哀牢山深变质带内两类晚渐新世花岗岩成因及其构造指示:中山大学学报(自然科学版),v.56,p.1-14. (23)何慧莹,王岳军*,刘汇川,张玉芝,2016,海南枫木地区基性岩的年代学、地球化学及其构造意义:中山大学学报(自然科学版),p.146-157. (24)甘成势,王岳军*,蔡永丰,刘汇川,张玉芝,宋菁菁,郭小飞,2016,南岭地区温公岩体的岩石成因及其构造指示:地球科学,p.17-34. (25)邢晓婉,张玉芝*,王岳军,刘汇川,2015,西盟地区奥陶纪花岗片麻岩的锆石U-Pb年代学、Hf同位素组成特征及其大地构造意义:大地构造与成矿学,v.39,p.470-480. (26)刘汇川,王岳军*,范蔚茗,訾建威,蔡永丰,杨光林,2014,滇西哀牢山地区晚三叠世高ε_(Nd)(t)-ε_(Hf)(t)花岗岩的构造指示:中国科学:地球科学,p.2373-2388. (27)蔡永丰,王岳军*,刘汇川,马莉燕,邢晓婉,刘雷,2014,哀牢山新元古代斜长角闪岩的形成时代、地球化学特征及其大地构造意义:大地构造与成矿学,p.168-180. (28)刘汇川,王岳军*,蔡永丰,马莉燕,邢晓婉,范蔚茗,2013,哀牢山构造带新安寨晚二叠世末期过铝质花岗岩锆石U-Pb年代学及Hf同位素组成研究:大地构造与成矿学,v.37,p.87-98. (29)马莉燕,范蔚茗,王岳军*,蔡永丰,刘汇川,2013,那邦地区花岗片麻岩的锆石U-Pb年代学及Hf同位素组成特征:大地构造与成矿学,v.37,p.273-283.

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