同济大学
导师风采
刘志飞
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个人信息

Personal Information

  • 教授
  • 导师类别:硕士,博士生导师
  • 性别: 男
  • 学历:博士研究生
  • 学位:博士

联系方式

Contact Information

  • 所属院系:海洋与地球科学学院
  • 所属专业: 海洋科学
  • 邮箱 : lzhifei@tongji.edu.cn
  • 工作电话 : 021-65984877

个人简介

Personal Profile

国家杰出青年基金获得者,教育部“长江学者”特聘教授。1999年成都理工学院沉积学博士毕业,2001年同济大学海洋科学博士后出站、并留校任教至今;2001年评为副教授,2004年晋升教授;现任海洋地质国家重点实验室主任。主要从事南海深海沉积过程和南海陆源碎屑沉积物从源到汇的海陆结合研究,通过现代过程现场观测和大洋钻探长期记录分析,研究深海沉积动力过程的机理及其不同时间尺度的全球变化响应。主持国家自然科学基金重大研究计划项目、重点项目等10余项,代表性研究成果在Science、Earth-Science Reviews、Geology等期刊上发表。曾获法国国家棕榈学术骑士勋章。


  • 研究方向Research Directions
海洋沉积学,深海沉积动力学,环境演变与全球变化,沉积物源汇过程,粘土矿物与碳循环,海洋观测系统
2. 机电结构优化与控制 研究内容:在对机电结构进行分析和优化的基础上,运用控制理论进行结构参数的调整,使结构性能满足设计要求。1. 仿生结构材料拓扑优化设计, 仿生机械设计 研究内容:以仿生结构为研究对象,运用连续体结构拓扑优化设计理论和方法,对多相仿生结构(机构)材料进行2. 机电结构优化与控制 研究内容:在对机电结构进行分析和优化的基础上,运用控制理论进行结构参数的调整,使结构性能满足设计要求。1. 仿生结构材料拓扑优化设计, 仿生机械设计 研究内容:以仿生结构为研究对象,运用连续体结构拓扑优化设计理论和方法,对多相仿生结构(机构)材料进行整体布局设计。 整体布局设计。
项目情况

在研科研项目


1. “南海南部深海沉积搬运过程及其对海洋碳循环影响的锚系观测研究”(编号42130407),2022.1-2026.12,国家自然科学基金重点项目。

项目简介:陆源和海源颗粒有机碳向深海的搬运过程,是海洋碳循环的关键组成部分,对全球气候的多尺度变化产生重要影响。但是,前人研究多忽视了陆源颗粒有机碳向深海的侧向搬运过程,而这种过程在发育大量陆源物质输入的边缘海尤其重要。本项目选择南海南部湄公河岸外和巽他陆架以北的深海区域,通过布设深海锚系,原位观测深层海流和沉积搬运动力过程的连续时间变化序列;通过沉积物捕集器样品的陆源/海源颗粒通量、稳定/放射性有机碳同位素、粘土矿物、锶/钕同位素、微区层析成像等测试分析,研究南海南部深海陆源和海源颗粒有机碳的侧向搬运和垂向沉降作用、陆源粘土矿物的源汇搬运过程、以及粘土矿物与陆源/海源颗粒有机碳的相互作用,定量评估世界级大型河流(湄公河)和宽广陆架(巽他陆架)输入南海深海颗粒有机碳效率,揭示深海沉积搬运过程对颗粒有机碳保存或降解的影响机制。本项研究对于探索深海过程影响海洋碳循环和全球气候变化机理具有重要的科学意义。


2. “国际大洋钻探计划合作研究”(编号20590780200),2020.10-2023.9,上海市“科技创新行动计划”国际科技合作项目。

项目简介:国际大洋钻探计划(IODP)是地球科学领域迄今规模最大、影响最深、历时最久的国际大科学计划,五十多年来取得的科学成就,为地球系统科学的发展做出巨大贡献。目前,美国、日本和欧洲作为平台提供者共同领导IODP。中国是IODP大家庭的积极成员,近期提出成为与美、日、欧并驾齐驱的IODP平台提供者并进入IODP领导层的发展目标。本项目围绕中国IODP的这一战略目标,利用我国在东南亚和“一带一路”国家合作的优势,与美国、印度尼西亚、马来西亚和泰国建立国际科技合作伙伴关系,提出在南海南部巽他陆架实施大洋钻探航次,回答热带低纬地区的海平面变化、流域演化和全球碳循环等国际前沿科学问题。该航次的组织和实施将是中国作为第四个钻探平台自主执行的第一个IODP航次,将有力地促成中国成为IODP国际大科学计划的领导成员,推动我国实施创新驱动发展战略,对解决全球变化等人类命运共同体面对的可持续发展问题具有重要意义。


3. “青藏高原典型河流沉积物源汇过程及其对极端气候变化的响应研究”(编号2019QZKK020403),2019.11-2024.10,第二次青藏高原综合科学考察研究任务二子专题。

项目简介:河流沉积物从源头到边缘海盆地输送过程中所组成的“源-汇”系统,对于全球物质循环、碳循环及水循环都具有重要的意义。而“亚洲水塔”青藏高原是全球主要大河的发源地,每年向周边海洋输送大量的物质。要理解这一巨大的“源-汇”系统的动力机制及其对全球气候和环境的影响,不仅需要对河流上游的青藏高原开展工作,也要同时在河流下游及边缘海盆地开展样品采集分析和动力观测工作。本子专题将全流域河流沉积物的矿物学和地球化学分析与流域关键地区、河口和临近深海沉积动力观测有机结合,旨在获取雅鲁藏布江—布拉马普特拉河和澜沧江—湄公河等流域河流沉积物从源到汇输送过程中沉积物的组成成分及动力条件等的空间变化,从而研究青藏高原河流沉积物从源到汇输入过程和动力机制,特别是河口及河流下游等沉积物汇区的沉积动力过程和机制,评估其对边缘海盆地的沉积贡献。利用河口和临近深海实时观测系统所获数据和悬浮沉积物样品,捕捉台风、强降雨等极端天气事件的信号,对比其与背景天气条件下的异同,从而评估河流沉积物源汇过程对极端天气事件的响应,并评估极端天气事件对观测地区水土保持、农业活动等的影响。


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科研项目

在研科研项目

1. “南海南部深海沉积搬运过程及其对海洋碳循环影响的锚系观测研究”(编号42130407),2022.1-2026.12,国家自然科学基金重点项目,负责人;
2. “国际大洋钻探计划合作研究”(编号20590780200),2020.10-2023.9,上海市“科技创新行动计划”国际科技合作项目,负责人;
3. “青藏高原典型河流沉积物源汇过程及其对极端气候变化的响应研究”(编号2019QZKK020403),2019.11-2024.10,第二次青藏高原综合科学考察研究任务二子专题,负责人;


研究成果

主要刊物论文

2024

Bertaz,J., Liu, Z.*, Colin, C.*, Dapoigny, A., Lin, A.T.-S., Li, Y., Jian, Z.,2024. Climatic and environmental impacts on the sedimentation of the SW Taiwanmargin since the last deglaciation: Geochemical and mineralogicalinvestigations. Paleoceanography and Paleoclimatology, 39: e2023PA004745. https://doi.org/10.1029/2023PA004745.

Ling,C., Liu, Z.*, Yu, X.*, Zhao, Y., Siringan, F.P., Le, K.P., Sathiamurthy,E., You, C.-F., Chen, K., 2024. Clay minerals control silicon isotopevariations of fine-grained river sediments: Implication for the trade-offbetween physical erosion and chemical weathering. Chemical Geology, 662: 122249.https://doi.org/10.1016/j.chemgeo.2024.122249.

Zhang,X., Liu, Z.*, Li, D.*, Zhao, Y., Zhang, Y., 2024. Turbidity currentsregulate the transport and settling of microplastics in a deep-sea submarinecanyon. Geology. https://doi.org/10.1130/G52116.1.

Shu,W., Colin, C.*, Liu, Z.*, Dapoigny, A., 2024. Late Oligocene-Mioceneevolution of deep-water circulation in the abyssal South China Sea: insightsfrom Nd isotopic records of fossil fish teeth. Geology. https://doi.org/10.1130/G52042.1.

Wang,W., Liu, Z.*, Zhao, Y., Lin, B., Zhang, X., Zhang, J., Li, J., Cao, J., Song,H., 2024. Mesoscale eddy-strengthened deep-sea topographic Rossby waves in thesouthwestern South China Sea. Scientific Reports, 14: 11362. https://doi.org/10.1038/s41598-024-62040-z.

Paradis,S.*, Diesing, M., Gies, H., Haghipour, N., Narman, L., Magill, C., Wagner, T., Galy,V.V., Hou, P., Zhao, M., Kim, J.-H., Shin, K.-H., Lin, B., Liu, Z., Wiesner,M.G., Stattegger, K., Chen, J., Zhang, J., Eglinton, T.I., 2024. Unravelingenvironmental forces shaping surface sediment geochemical “isodrapes” in theEast Asian marginal seas. Global Biogeochemical Cycles, 38: e2023GB007839.https://doi.org/10.1029/2023GB007839

Cao,J., Liu, Z.*, Lin, B., Zhao, Y., Li, J., Wang, H., Zhang, X., Zhang, J.,Song, H., 2024. Temporal and vertical variations in carbon flux and export of zooplanktonfecal pellets in the western South China Sea. Deep-Sea Research Part I, 207:104283. https://doi.org/10.1016/j.dsr.2024.104283.

Lin,B., Liu, Z.*, Eglinton, T.I., Wiesner, M.G., Blattmann, T.M., Haghipour,N., 2024. Organic carbon sources in surface sediments on the northern SouthChina Sea. Journal of Geophysical Research: Biogeosciences, 129: e2023JG007909.https://doi.org/10.1029/2023JG007909.

Song,H., Liu, Z.*, Lin, B., Zhao, Y., Siringan, F.P., You, C.-F., 2024. Claymineral nanostructures regulate sequestration of organic carbon in typicalfluvial sediments. Heliyon, 10: e25825. https://doi.org/10.1016/j.heliyon.2024.e25825.

Huang,Y., Colin, C.*, Liu, Z., Joffrey, B., Dapoigny, A., Douville, E., Yu, Z.,Lin, A.T.-S., 2024. Roles of changes in land weathering intensity in the Ndcycle of the South China Sea during the past 30 kyr as inferred from neodymiumisotopic composition in foraminifera. Chemical Geology, 648: 121954. https://doi.org/10.1016/j.chemgeo.2024.121954.

Zhao,Y.*, Liu, Z., Zhang, Y., Zhang, X., Ma, P., Yu, X., Ling, C., Lin, B.,Zhang, J., 2024. Formation mechanism of drift-moat contourite systems revealedby in-situ observations in the South China Sea. Earth and Planetary ScienceLetters, 628: 118585. https://doi.org/10.1016/j.epsl.2024.118585.

You,C.-F.*, Liao, W.-L., Huang, K.-F., Chung, C.-H., Liu, Z., 2024. Sedimentsource variation using REEs, Sr, and Nd isotopic compositions: A case study inMD05-2901, northwestern South China Sea. Frontiers in Marine Science, 10: 1292802.https://doi.org/10.3389/fmars.2023.1292802.

Zhao,H., Liu, Z.*, Zhao, Y., 2024. Sea-level and East Asian monsooninfluenced chemical weathering records in the southern South China Sea over thepast 21 ka. Global and Planetary Change, 232: 104324. https://doi.org/10.1016/j.gloplacha.2023.104324.

2023

Wang,H., Liu, Z.*, Li, J., Lin, B., Zhao, Y., Zhang, X., Cao, J., Zhang, J.,Song, H., Wang, W., 2023. Sinking fate and carbon export of zooplankton fecalpellets: insights from time-series sediment trap observations in the northernSouth China Sea. Biogeosciences, 20: 5109–5123.https://doi.org/10.5194/bg-20-5109-2023.

Wu,L., Zhao, Y.*, Liu, Z., Ma, P., Zhang, Y., 2023. Sedimentary processesin the bottom boundary layer of a contourite drift in the northern South ChinaSea. Frontiers in Marine Science, 10: 1217216. https://doi.org/10.3389/fmars.2023.1217216.

Wu,K., Liu, S., Shi, X.*, Colin, C.*, Zhang, H., Bassinot, F., Liu, Z., Fang,X., Miska, S., Nouet, J., Pinna-Jamme, R., Dapoigny, A., Mohamed, C.A.R., Khokiattiwong,S., Kornkanitnan, N., 2023. The impact of changes in sea level and East Asian monsoonon sediment transport on the Sunda Shelf since the last deglaciation. Journalof Geophysical Research: Earth Surface, 128: e2023JF007335.https://doi.org/10.1029/2023JF007335.

Huang,Y., Colin, C.*, Liu, Z., Douville, E., Dapoigny, A., Haurine, F., Wu, Q.,Lin, A.T.-S., 2023. Impacts of nepheloid layers and mineralogical compositionsof oceanic margin sediments on REE concentrations and Nd isotopic compositions ofseawater. Geochimica et Cosmochimica Acta, 359: 57-70. https://doi.org/10.1016/j.gca.2023.08.026.

Shu,W., Liu, Z.*, Colin, C.*, Ma, P., Huang, B., Dapoigny, A., 2023. Terrigenousprovenance of late Oligocene–Miocene sediments in the central basin of theSouth China Sea and its implications for chemical weathering and climate change.Marine Geology, 462: 107098. https://doi.org/10.1016/j.margeo.2023.107098.

Huang,H., Liu, Z.*, Zhao, Y., Zhao, H., Fernandez, A.R., Colin, C., Lin,A.T.-S., 2023. Clay mineral assemblages of late Holocene turbidites in theGaoping Submarine Canyon of the northeastern South China Sea and their responsesto typhoon activities. Palaeogeography, Palaeoclimatology, Palaeoecology, 624: 111650.https://doi.org/10.1016/j.palaeo.2023.111650.

Zhao,H., Liu, Z.*, Zhao, Y., Wu, J., Colin, C., 2023. Lunar nodal tidal cycleinfluences on the input of coarse sediments during the last glaciation in thedeep South China Sea. Quaternary Science Reviews, 310: 108114. https://doi.org/10.1016/j.quascirev.2023.108114.

Lin,B., Liu, Z.*, Zhao, M., Sompongchaiyakul, P., Zhang, H., Blattmann,T.M., Feng, S., Wiesner, M.G., Le, K.P., Meas, R., Sathiamurthy, E., 2023. Compositionsand sources of sedimentary organic carbon on the tropical epicontinental sea. Geochimicaet Cosmochimica Acta, 351: 32-44. https://doi.org/10.1016/j.gca.2023.04.030.

Zhao,Y.*, Wang, Y., Liu, Z., Li, X., Wang, W., 2023. Deep-water circulationintensity and stratification in the South China Sea since the last glaciation.Marine Geology, 457: 107004. https://doi.org/10.1016/j.margeo.2023.107004.

Cheng,Z.*, Wu, J., Luo, C., Liu, Z., Huang, E., Zhao, H., Dai, L., Weng, C.*, 2023.Coexistence of savanna and rainforest on the ice-age Sunda Shelf revealed bypollen records from southern South China Sea. Quaternary Science Reviews, 301: 107947.https://doi.org/10.1016/j.quascirev.2022.107947.

2022

Wu,Q.*, Liu, Z., Colin, C., Douville, E., Zhao, Y., Wu, J., Dapoigny, A.,Bordier, L., Ma, P., Huang, Y., 2022. Dissolved rare earth element and neodymiumisotope distributions in the South China Sea: Water mass source versus particledissolution. Frontiers in Marine Science, 9: 1003749. https://doi.org/10.3389/fmars.2022.1003749.

Li,J., Liu, Z.*, Lin, B., Zhao, Y., Cao, J., Zhang, X., Zhang, J., Ling,C., Ma, P., Wu, J., 2022. Zooplankton fecal pellet characteristics andcontribution to the deep-sea carbon export in the southern South China Sea.Journal of Geophysical Research: Oceans, 127: e2022JC019412.https://doi.org/10.1029/2022JC019412.

Zhang,X., Liu, Z.*, Zhao, Y., Ma, P., Colin, C., Lin, A.T.-S., 2022.Distribution and controlling factors of microplastics in surface sediments oftypical deep-sea geomorphological units in the northern South China Sea.Frontiers in Marine Science, 9: 1047078. https://doi.org/10.3389/fmars.2022.1047078.

Yu,X.*, Liu, Z., Wu, J., An, Y.-J., Shi, J.-H., 2022. Iron isotopicvariations in basalts from oceanic crust due to low-temperature seawateralteration. Marine Geology, 454: 106949. https://doi.org/10.1016/j.margeo.2022.106949.

Ma,P.*, Liu, Z., Jiang, M., Cheng, H., Zhang, L., Cai, D., 2022. Carbonsequestration of the middle Miocene Sunda Shelf facilitated global climatechange. Geophysical Research Letters, 49, e2022GL100638.https://doi.org/10.1029/2022GL100638.

You,C.-F.*, Lin, P.-Y., Huang, K.-F., Chung, C.-H., Liu, Z., 2022. Ocean acidificationin the Western Pacific: Boron isotopic composition recorded in a tropicalmassive coral core from Lanyu Islet SE Taiwan. Frontiers in Marine Science, 9: 877810.https://doi.org/10.3389/fmars.2022.877810.

Yu,X.*, Liu, Z., Zeng, G., Cao, W., Meas, R., Hoang, V.L., Sang, P.N.,2022. Mantle plume-stagnant slab interaction controls the generation of a mixedmantle source for continental intraplate basalts. Lithos, 426–427: 106795. https://doi.org/10.1016/j.lithos.2022.106795.

Sang,P.N.*, Liu, Z.*, Colin, C., 2022. Chemical weathering of the MekongRiver basin with implication for East Asian monsoon evolution during lateQuaternary: Marine sediment records in the southern South China Sea. Frontiersin Earth Science, 10: 885547. https://doi.org/10.3389/feart.2022.885547.

Jiwarungrueangkul,T.*, Liu, Z., Sompongchaiyakul, P., Jirapinyakul, A., Stattegger, K.,2022. Multi-proxy reconstructions of productivity on the continental slope offthe Mekong River in the southern South China Sea over the past 30,000 years.Palaeogeography, Palaeoclimatology, Palaeoecology, 597: 111005. https://doi.org/10.1016/j.palaeo.2022.111005.

Lyu,X., Liu, Z.*, Wu, Q.*, Colin, C., Yu, X., Liu, C., Li, Q., 2022.Quantifying iron oxide mineral contents in Miocene oceanic red beds for thedeep-sea oxidation evolution in the South China Sea. Frontiers in EarthScience, 10: 875292. https://doi.org/10.3389/feart.2022.875292.

Wu, J.*, Liu, Z., Michard, A., Tachikawa,K., Filippidi, A., He, Z., Hennekam, R., Yang, S., Davies, G.R., de Lange,G.J., 2022. Effect of barite-bound Sr on detrital Sr isotope systematics inmarine sediments. Chemical Geology, 587: 120613. https://doi.org/10.1016/j.chemgeo.2021.120613.

2021

Wu, J.*, Liu,Z.*, Yu, X., 2021. Plagioclase-regulated hydrothermal alteration ofbasaltic rocks with implications for the South China Sea rifting. ChemicalGeology, 585: 120569. https://doi.org/10.1016/j.chemgeo.2021.120569.

Lin,B., Liu, Z.*, Eglinton, T.I.*, Blattmann, T.M., Kandasamy, S.,Haghipour, N., Siringan, F.P., 2021. Organic matter compositions and loadingsin river sediments from humid tropical volcanic Luzon island of thePhilippines. Journal of Geophysical Research: Biogeosciences, 126:e2020JG006192. https://doi.org/10.1029/2020JG006192.

Nayak,K., Lin, A.T.-S.*, Huang, K.-F., Liu, Z., Babonneau, N., Ratzov, G.,Pillutla, R.K., Das, P., Hsu, S.-K., 2021. Clay-mineral distribution in recentdeep-sea sediments around Taiwan: Implications for sediment dispersalprocesses. Tectonophysics, 814: 228974. https://doi.org/10.1016/j.tecto.2021.228974.

Blattmann,T.M.*, Liu, Z.*, 2021. Proposing a classic clay mineral proxy forquantifying kerogen reburial in the geologic past. Applied Clay Science, 211:106190. https://doi.org/10.1016/j.clay.2021.106190.

Wang,H., Kandasamy, S.*, Liu, Q., Lin, B., Lou, J.-Y., Veeran, Y., Lei, H., Liu,Z., Chen, C.-T. A., 2021. Roles of sediment supply, geochemical compositionand monsoon on organic matter burial along the longitudinal mud belt in theEast China Sea in modern times. Geochimica et Cosmochimica Acta, 305: 66-86.https://doi.org/10.1016/j.gca.2021.04.025.

Jiwarungrueangkul,T., Liu, Z.*, 2021. East Asian monsoon and sea-level controls on claymineral variations in the southern South China Sea since the Last GlacialMaximum. Quaternary International, 592: 1-11. https://doi.org/10.1016/j.quaint.2021.04.033.

Zhao,S.*, Cai, F., Liu, Z., Cao, C.*, Qi, H., 2021. Disturbed climate changespreserved in terrigenous sediments associated with anthropogenic activitiesduring the last century in the Taiwan Strait, East Asia. Marine Geology, 437:106499. https://doi.org/10.1016/j.margeo.2021.106499.

Colin, C.*, Duhamel, M., Siani, G.,Dubois-Dauphin, Q., Ducassou, E., Liu, Z., Wu, J., Revel, M., Dapoigny,A., Douville, E., Taviani, M., Montagna, P., 2021. Changes in the intermediatewater masses of the Mediterranean Sea during the last climatic cycle—Newconstraints from neodymium isotopes in foraminifera. Paleoceanography andPaleoclimatology, 36, e2020PA004153. https://doi.org/10.1029/2020PA004153.

Gao, Y.*, Gao, Y.F., Ibarra, D.E., Du, X.,Dong, T., Liu, Z., Wang, C., 2021. Clay mineralogical evidence formid-latitude terrestrial climate change from the latest Cretaceous through theearliest Paleogene in the Songliao Basin, NE China. Cretaceous Research, 124:104827. https://doi.org/10.1016/j.cretres.2021.104827.

Sang, P.N., Liu,Z.*, 2021. Terrigenous sediment variations in the western South China Seaand their implications to East Asian monsoon evolution during the lastglacial-interglacial cycle. Quaternary International, 580: 1-10.https://doi.org/10.1016/j.quaint.2021.02.008.

Wu, L., Wilson, D.J., Wang, R.*, Passchier, S.,Krijgsman, W., Yu, X., Wen, T., Xiao, W., Liu, Z., 2021. Late Quaternarydynamics of the Lambert Glacier-Amery Ice Shelf system, East Antarctica.Quaternary Science Reviews, 252: 106738.https://doi.org/10.1016/j.quascirev.2020.106738.

2020

Ma, P.*, Liu,Z.*, Huang, B., Zhao, Y., Shu, W., Li, Y., 2020. Oligocene evolution of theoutermost continental margin in response to breakup and early spreading of theSouth China Sea. Marine Geology, 427: 106241.https://doi.org/10.1016/j.margeo.2020.106241.

Yu,X.*, Liu, Z.*, 2020. Non-mantle-plume process caused the initialspreading of the South China Sea. Scientific Reports, 10: 8500.https://doi.org/10.1038/s41598-020-65174-y.

Duhamel, M., Colin, C.*, Revel, M., Siani, G.,Dapoigny, A., Douville, E., Wu, J., Zhao, Y., Liu, Z., Montagna, P.,2020. Variations in eastern Mediterranean hydrology during the last climaticcycle as inferred from neodymium isotopes in foraminifera. Quaternary ScienceReviews, 237: 106306. https://doi.org/10.1016/j.quascirev.2020.106306.

Lin, B., Liu,Z.*, Eglinton, T.I.*, Kandasamy, S., Blattmann, T.M., Haghipour, N., Huang,K.-F., You, C.F., 2020. Island-wide variation in provenance of riverine sedimentaryorganic carbon: A case study from Taiwan. Earth and Planetary Science Letters,539: 116238. https://doi.org/10.1016/j.epsl.2020.116238.

Liu,Z., Yang, S.,Zhao, Y., Ma, P., de Boer, P., 2020. Source-to-sink systems: From orogenicbelts to marginal sea basins. In: Wang, C.S., Immenhauser, A., Ogg, J., et al.,A Roadmap of Sedimentology in China until 2030: Sedimentology at the Crossroadof New Frontiers. International Associations of Sedimentologists (IAS).

2019

Jiwarungrueangkul,T., Liu, Z.*, Stattegger, K., Sang, P.N., 2019. Reconstructing chemicalweathering intensity in the Mekong River basin since the Last Glacial Maximum.Paleoceanography and Paleoclimatology, 34: 1710-1725. https://doi.org/10.1029/2019PA003608.

Blattmann,T.M.*, Liu, Z.*, Zhang, Y., Zhao, Y., Haghipour, N., Montluçon, D.B.,Plötze, M., Eglinton, T.I., 2019. Mineralogical control on the fate ofcontinentally derived organic matter in the ocean. Science, 366: 742-745.https://doi.org/10.1126/science.aax5345.

Zhou, X., Lyu,X., Liu, C.*, Liu, Z., Li, Q., Jin, X., Zhang, H., Dadd, K., 2019.Depositional mechanisms for upper Miocene sediments in the South China Seacentral basin: Evidence from calcareous nannofossils. Marine Micropaleontology,151: 101768. https://doi.org/10.1016/j.marmicro.2019.101768.

Jin, X.B., Liu, C.L.*, Zhao, Y.L., Zhang, Y.W.,Wen, K., Lin, S., Li, J.R., Liu, Z.F., 2019. Two production stages ofcoccolithophores in winter as revealed by sediment traps in the northern SouthChina Sea. Journal of Geophysical Research: Biogeosciences, 124.https://doi.org/10.1029/2019JG005070.

Lin, B., Liu, Z.*, Eglinton, T.I.*,Kandasamy, S., Blattmann, T.M., Haghipour, N., de Lange, G.J., 2019.Perspectives on provenance and alteration of suspended and sedimentary organicmatter in the subtropical Pearl River system, South China. Geochimica etCosmochimica Acta, 259: 270-287. https://doi.org/10.1016/j.gca.2019.06.018.

Sang, P.N., Liu, Z.*, Stattegger,K., 2019. Weathering and erosion in central Vietnam over the Holocene andYounger Dryas: Clay mineralogy and elemental geochemistry from the VietnamShelf, western South China Sea. Journal of Asian Earth Sciences, 179: 1-10.https://doi.org/10.1016/j.jseaes.2019.04.008.

Ma, R.*, Sépulcre, S., Licari, L., Bassinot,F., Liu, Z., Tisnérat-Laborde, N., Kallel, N., Yu, Z., Colin, C., 2019.Changes in intermediate circulation in the Bay of Bengal since the Last GlacialMaximum as inferred from benthic foraminifera assemblages and geochemicalproxies. Geochemistry Geophysics Geosystems, 20: 1592-1608.https://doi.org/10.1029/2018GC008179.

Jiwarungrueangkul, T., Liu, Z.*, Zhao, Y., 2019. Terrigenous sediment input responding tosea level change and East Asian monsoon evolution since the last deglaciationin the southern South China Sea. Global and Planetary Change, 174: 127-137.https://doi.org/10.1016/j.gloplacha.2019.01.011.

Ali, S.*, Stattegger, K., Liu, Z.,Khélifi, N., Kuhnt, W., 2019. Paleoclimatic and paleoenvironmentalreconstruction at Tarfaya Atlantic coastal basin (Morocco) based on claymineral records from Upper Cretaceous to Quaternary. Arabian Journal ofGeosciences, 12 (6). https://doi.org/10.1007/s12517-018-4156-4.

2018

Blattmann, T.M.*, Zhang, Y.*, Zhao, Y., Wen,K., Lin, S., Li, J., Wacker, L., Haghipour, N., Ploze, M., Liu, Z., Eglinton, T.I., 2018. Contrasting fates of petrogenic andbiospheric carbon in the South China Sea. Geophysical Research Letters, 45:9077-9086. https://doi.org/10.1029/2018GL079222.

Larsen, H.C.*, Mohn, G.*, Nirrengarten, M.,Sun, Z., Stock, J., Jian, Z., Klaus, A., Alvarez-Zarikian, C.A., Boaga, J.,Bowden, S.A., Briais, A., Chen, Y., Cukur, D., Dadd, A., Ding, W., Dorais, M.,Ferré, E.C., Ferreira, F., Furusawa, A., Gewecke, A., Hinojosa, J., Höfig,T.W., Hsiung, K.H., Huang, B., Huang, E., Huang, X.L., Jiang, S., Jin, H.,Johnson, B.G., Kurzawski, R.M., Lei, C., Li, B., Li, L., Li, Y., Lin, J., Liu,C., Liu, C., Liu, Z., Luna, A.J., Lupi,C., McCarthy, A., Ningthoujam, L., Osono, N., Peate, D.W., Persaud, P., Qiu,N., Robinson, C., Satolli, S., Sauermilch, I., Schindlbeck, J.C., Skinner, S., Straub,S., Su, X., Su, C., Tian, L., van der Zwan, F.M., Wan, S., Wu, H., Xiang, R., Yadav,R., Yi, L., Yu, P.S., Zhang, C., Zhang, J., Zhang, Y., Zhao, N., Zhong, G.,Zhong, L., 2018. Rapid transition from continental breakup to igneous oceaniccrust in the South China Sea. Nature Geoscience, 11: 782-789.https://doi.org/10.1038/s41561-018-0198-1.

Zhang, Y.*, Liu, Z., Zhao, Y., Colin, C., Zhang, X., Wang, M., Zhao, S.,Kneller, B., 2018. Long-term in situobservations on typhoon-triggered turbidity currents in the deep sea. Geology,46: 675-678. https://doi.org/10.1130/G45178.1.

Sang, P.N., Liu, Z.*, Zhao, Y., Zhao, X., Pha, P.D., Long, H.V., 2018. Chemicalweathering in central Vietnam from clay mineralogy and major-elementgeochemistry of sedimentary rocks and river sediments. Heliyon, 4, e00710. https://doi.org/10.1016/j.heliyon.2018.e00710.

Zhao, S., Liu,Z.*, Colin, C., Zhao, Y., Wang, X., Jian, Z., 2018. Responses of the EastAsian summer monsoon in the low-latitude South China Sea to high-latitudemillennial-scale climatic changes during the last glaciation: Evidence form ahigh-resolution clay mineralogical record. Paleoceanography and Paleoclimatology,33. https://doi.org/10.1029/2017PA003235.

Rahman, M.M., Sathiamurthy, E.*, Zhong, G.,Geng, J., Liu, Z., 2018. Variationsof fluvial patterns and infilling history of a paleoincised valley systemduring Late Pleistocene to Holocene, Offshore Pahang River, PeninsularMalaysia. Interpretation, 6 (1): T39-T50.http://dx.doi.org/10.1190/INT-2016-0055.1.

2017

Liu,Z.*, Li, C.-F., Kulhanek, D., 2017. Preface: Evolution of thedeep South China Sea: Integrated IODP Expedition 349 results. Marine Geology,394: 1-3. https://doi.org/10.1016/j.margeo.2017.11.009.

Wu, Q.*, Colin, C., Liu, Z., Bassinot, F., Dubois-Dauphin, Q., Douville, E., Thil, F.,Siani, G., 2017. Foraminiferal eNd in the deepnorth-western subtropical Pacific Ocean: Tracing changes in weathering inputover the last 30,000 years. Chemical Geology, 470: 55-66.http://dx.doi.org/10.1016/j.chemgeo.2017.08.022.

Joussain, R.*, Liu, Z., Colin, C., Duchamp-Alphonse, S., Yu, Z., Morénoc, E.,Fournier, L., Zaragosi, S., Dapoigny, A., Meynadier, L., Bassinot, F., 2017.Link between Indian monsoon rainfall and physical erosion in the Himalayansystem during the Holocene. Geochemistry Geophysics Geosystems, 18,doi:10.1002/2016GC006762.

Chen, Q.*, Kissel, C., Liu, Z., 2017. Late Quaternary climatic forcing on the terrigenoussupply in the northern South China Sea: Input from magnetic studies. Earth andPlanetary Science Letters, 471: 160-171.http://dx.doi.org/10.1016/j.epsl.2017.04.047.

Wu, J.*, Liu,Z., Stuut, J.-B. W., Zhao, Y., Schirone, A., de Lange, G.J., 2017.North-African paleodrainage discharges to the central Mediterranean during thelast 18,000 years: A multiproxy characterization. Quaternary Science Reviews,163: 95-113. http://dx.doi.org/10.1016/j.quascirev.2017.03.015.

Chen, Q.*, Liu,Z., Kissel, C. 2017. Clay mineralogical and geochemical proxies of the EastAsian summer monsoon evolution in the South China Sea during Late Quaternary.Scientific Reports, 7, 42083, doi:10.1038/srep42083.

Dubois-Dauphin,Q., Montagna, P., Siani, G., Douville, E., Wienberg, C., Hebbeln, D., Liu, Z., Kallel, N., Dapoigny, A.,Revel, M., Pons-Branchu, E., Taviani, M., Colin, C.*, 2017. Hydrologicalvariations of the intermediate water masses of the western Mediterranean Seaduring the past 20 ka inferred from neodymium isotopic composition in foraminiferaand cold-water corals. Climate of the Past, 13, 17-37.doi:10.5194/cp-13-17-2017.

Kissel, C.*, Liu, Z., Li, J., Wandres, C., 2017.Magnetic signature of river sediments drained into the southern and easternpart of the South China Sea (Malay Peninsula, Sumatra, Borneo, Luzon andTaiwan). Sedimentary Geology, 347: 10-20.http://dx.doi.org/10.1016/j.sedgeo.2016.11.007.

Sun, Q.*, Colin, C., Liu, Z., Mischke, S.,Duchamp-Alphonse, S., Zhang, C., Chen, F., 2017. Climate changes of thenortheastern Tibetan Plateau since the late glaciation inferred from claymineralogy of sediments in Kuhai Lake. Quaternary International, 440: 24-34. http://dx.doi.org/10.1016/j.quaint.2016.08.009.

2016

Joussain, R.*, Colin, C., Liu, Z., Meynadier, C., Fournier, L., Fauquembergue, K., Zaragosi,S., Schmidt, F., Rojas, V., Bassinot, F., 2016. Climatic control of sedimenttransport from the Himalayas to the proximal NE Bengal Fan during the lastglacial-interglacial cycle. Quaternary Science Reviews, 148: 1-16.http://dx.doi.org/10.1016/j.quascirev.2016.06.016.

Kissel, C.*, Liu, Z., Li, J., Wandres, C., 2016. Magnetic minerals in threeAsian rivers draining into the South China Sea: Pearl, Red, and Mekong Rivers,Geochemistry Geophysics Geosystems, 17: 1678-1693. doi:10.1002/2016GC006283.

Chen, Q.*, Kissel, C., Govin, A., Liu, Z., Xie, X., 2016. Correction ofinterstitial water changes in calibration methods applied to XRF core-scanningmajor elements in long sediment cores: Case study from the South China Sea. GeochemistryGeophysics Geosystems, 17, doi:10.1002/2016GC006320.

Liu,Z.*, Zhao, Y., Colin, C., Stattegger, K., Wiesner, M.G., Huh,C.-A., Zhang, Y., Li, X., Sompongchaiyakul, P., You, C.-F., Huang, C.-Y., Liu,J.T., Siringan, F.P., Le, K.P., Sathiamurthy, E., Hantoro, W.S., Liu, J., Tuo,S., Zhao, S., Zhou, S., He, Z., Wang, Y., Bunsomboonsakul, S., Li, Y., 2016.Source-to-sink processes of fluvial sediments in the South China Sea. Earth-ScienceReviews, 153: 238-273. http://dx.doi.org/10.1016/j.earscirev.2015.08.005.

Yu, Z.*, Wan, S.*, Colin, C., Yan, H., Bonneau,L., Liu, Z., Song, L., Sun, H., Xu,Z., Jiang, X., Li, A., Li, T., 2016. Co-evolution of monsoonal precipitation inEast Asia and the tropical Pacific ENSO system since 2.36 Ma: New insights fromhigh-resolution clay mineral records in the West Philippine Sea. Earth andPlanetary Science Letters, 446: 45-55.

Zhao, Y.*, Colin, C., Liu, Z., Bonneau, L., Siani, G., 2016. Climate forcing ofterrigenous sediment input to the central Mediterranean Sea since the earlyPleistocene. Palaeogeography, Palaeoclimatology, Palaeoecology. 442: 23-25.

Lu, H.*, Li, Y., Xu, X., Li, J., Liu, Z.,Li, X., Yang, J., Serikawa, S., 2106. Underwater image enhancement method usingweighted guided trigonometric filtering and artificial light correction.Journal of Visual Communication and Image Representation, 38: 504-516.

2015

Gao, Y., Wang,C.*, Liu, Z., Du, X., Ibarra, D.E.,2015. Diagenetic and paleoenvironmental controls on Late Cretaceous clayminerals in the Songliao Basin, northeast China. Clays and Clay Minerals, 63:469-484.

Wu, Q.*, Colin, C., Liu, Z., Douville, E., Dubois-Dauphin, Q., Frank, N., 2015. Newinsights into hydrological exchange between the South China Sea and the westernPacific Ocean based on the Nd isotopic composition of seawater. Deep-SeaResearch II, 122: 25-40.

Zhang, Y.*, Liu, Z., Zhao, Y., Li, J., Liang, X., 2015. Effect of surfacemesoscale eddies on deep-sea currents and mixing in the northeastern SouthChina Sea. Deep-Sea Research II, 122: 6-14.

Wu, Q., Colin, C.*, Liu, Z., Thil, F., Dubois-Dauphin, Q., Frank, N., Tachikawa, K., Bordier,L., Douville, E., 2015. Neodymium isotopic composition in foraminifera andauthigenic phases of the South China Sea sediments: Implications for thehydrology of the North Pacific Ocean over the past 25 kyr. Geochemistry GeophysicsGeosystems, 16, doi:10.1002/2015GC005871.

Zhao, Y.*, Liu,Z., Zhang, Y., Li, J., Wang, M., Wang, W., Xu, J., 2015. In situ observation of contour currentsin the northern South China Sea: Applications for deepwater sediment transport.Earth and Planetary Science Letters, 430: 477-485.

Schroeder, A.*, Wiesner, M.G., Liu, Z., 2015. Fluxes of clay mineralsin the South China Sea. Earth and Planetary Science Letters, 430: 30-42.

Li, C.-F.*, Li, J., Ding, W., Franke, D., Yao, Y.,Shi, H., Pang, X., Cao, Y., Lin, J., Kulhanek, D.K., Williams, T., Bao, R., Briais,A., Brown, E.A., Chen, Y., Clift, P.D., Colwell, F.S.., Dadd, K.A., Almeida, I.H.,Huang, X.-L., Hyun, S., Jiang, T., Koppers, A.A.P., Li, Q., Liu, C., Liu, Q., Liu, Z., Nagai, R.H., Peleo-Alampay, A.,Su, X., Sun, Z., Tejada, M.L.G., Trinh, H.S., Yeh, Y.-C., Zhang, C., Zhang, F.,Zhang, G.-L., Zhao, X., 2015. Seismic stratigraphy of the central South ChinaSea basin and implications for neotectonics. Journal of Geophysical Research: SolidEarth, 120: 1377-1399. doi:10.1002/2014JB011686.

2014

Zhang, Y., Liu,Z.*, Zhao, Y., Wang, W., Li, J., Xu, J., 2014. Mesoscale eddies transportdeep-sea sediments. Scientific Reports, 4, 5937, doi:10.1038/srep05937.

Liu,Z.*, Stattegger, K., 2014. South China Sea fluvial sediments:An introduction. Journal of Asian Earth Sciences, 79: 507-508.

Li, C.-F.*, Xu, X., Lin, J., Sun, Z., Zhu, J.,Yao, Y., Zhao, X., Liu, Q., Kulhanek, D.K., Wang, J., Song, T., Zhao, J., Qiu,N., Guan, Y., Zhou, Z., Williams, T., Bao, R., Briais, A., Brown, E.A., Chen, Y.,Clift, P.D., Colwell, F.S., Dadd, K.A., Ding, W., Almeida, I.H., Huang, X.-L., Hyun,S., Jiang, T., Koppers, A.A.P., Li, Q., Liu, C., Liu, Z., Nagai, R.H., Peleo-Alampay, A., Su, X., Tejada, M.L.G., Trinh,H.S., Yeh, Y.-C., Zhang, C., Zhang, F., Zhang, G.-L., 2014. Ages and magneticstructures of the South China Sea constrained by deep tow magnetic surveys andIODP Expedition 349. Geochemistry Geophysics Geosystems, 15, doi:10.1002/2014GC005567.

Colin, C.*, Siani, G., Liu, Z., Blamart, D., Skonieczny, C., Zhao, Y., Bory, A., Frank,N., Duchamp-Alphonse, S., Thil, F., Richter, T., Kissel, C., Gargani, J., 2014.Late Miocene to early Pliocene climate variability off NW Africa (ODP Site 659).Palaeogeography, Palaeoclimatology, Palaeoecology, 401: 81-95.

Huang, K.-F.*, You, C.-F., Chung, C.-H., Lin,Y.-H., Liu, Z., 2014. Tracing the Ndisotope evolution of North Pacific Intermediate and Deep Waters through thelast deglaciation from South China Sea sediments. Journal of Asian EarthSciences, 79: 564-573.

2013

Wu, J.*, Liu,Z.*, Zhou, C., 2013. Provenance and supply of Fe-enriched terrigenoussediments in the western equatorial Pacific and their relation to precipitationvariations during the late Quaternary. Global and Planetary Change, 108: 56-71.

Gao, Y., Wang, C.*, Liu, Z., Zhao, B., Zhang, X., 2013. Clay mineralogy of the middleMingshui Formation (upper Campanian to lower Maastrichtian) from the SKInborehole in the Songliao Basin, NE China: Implications for palaeoclimate andprovenance. Palaeogeography, Palaeoclimatology, Palaeoecology, 385: 162-170.

2012

Zhao, Y.*, Colin, C., Liu, Z., Paterne, M., Siani, G., Xie, X., 2012. Reconstructingprecipitation changes in northeastern Africa during the Quaternary by claymineralogical and geochemical investigations of Nile deep-sea fan sediments.Quaternary Science Reviews, 57: 58-70.

Liu,Z.*, Wang, H., Hantoro, W.S., Sathiamurthy, E., Colin, C.,Zhao, Y., Li, J., 2012. Climatic and tectonic controls on chemical weatheringin tropical Southeast Asia (Malay Peninsula, Borneo, and Sumatra). ChemicalGeology, 291: 1-12.

Wang, C.*, Li, X., Liu, Z., Li, Y., Jansa, L., Dai, J., Wei, Y., 2012. Revision of theCretaceous-Paleogene stratigraphic framework, facies architecture andprovenance of the Xigaze forearc basin along the Yarlung Zangbo suture zone.Gondwana Research, 22: 415-433.

Hebert, R.*, Bezard, R., Guilmette, C., Dostal,J., Wang, C.S., Liu, Z.F., 2012. TheIndus-Yarlung Zangbo ophiolites from Nanga Parbat to Namche Barwa syntaxes,southern Tibet: First synthesis of petrology, geochemistry, and geochronologywith incidences on geodynamic reconstructions of Neo-Tethys. Gondwana Research,22: 377-397.

2011

Zhao, Y.*, Liu,Z., Colin, C., Paterne, M., Siani, G., Cheng, X., Duchamp-Alphonse, S.,Xie, X., 2011. Variations of the Nile suspended discharges during the last 1.75Myr. Palaeogeography, Palaeoclimatology, Palaeoecology, 311: 230-241.

Liu, H.-C., You, C.-F.*, Chung, C.-H., Huang,K.-F., Liu, Z.-F., 2011. Sourcevariability of sediments in the Shihmen Reservoir, Northern Taiwan: Sr isotopicevidence. Journal of Asian Earth Sciences, 41: 297-306.

2010-2000

Liu,Z.*, Colin, C., Li, X., Zhao, Y., Tuo, S., Chen, Z.,Siringan, F.P., Liu, J.T., Huang, C.-Y, You, C.-F., Huang, K.-F., 2010. Claymineral distribution in surface sediments of the northeastern South China Seaand surrounding fluvial drainage basins: Source and transport. Marine Geology, 277:48-60.

Colin, C.*, Siani, G., Sicre, M.-A., Liu, Z., 2010. Impact of the East Asianmonsoon rainfall changes on the erosion of the Mekong River basin over the past25,000 yr. Marine Geology, 271: 84-92.

Liu,Z.*, Zhao, Y., Colin, C., Siringan, F.P., Wu, Q., 2009. Chemicalweathering in Luzon, Philippines from clay mineralogy and major-elementgeochemistry of river sediments. Applied Geochemistry, 24: 2195-2205.

Liu,Z.*, Huang, W., Li, J., Wang, P., Wang, R., Yu, K., Zhao, J.,2009. Sedimentology. In: Wang, P., Li, Q. (eds.), The South China Sea –Paleoceanography and Sedimentology, Springer. 171-295.

Liu,Z.*, Tuo, S., Colin, C., Liu, J.T., Huang, C.-Y., Selvaraj,K., Chen, C.-T.A., Zhao, Y., Siringan, F.P., Boulay, S., Chen, Z., 2008.Detrital fine-grained sediment contribution from Taiwan to the northern SouthChina Sea and its relation to regional ocean circulation. Marine Geology, 255:149-155.

Wang, C.*, Zhao, X.*, Liu, Z., Lippert, P.C., Graham, S.A., Coe, R.S., Yi, H., Zhu, L.,Liu, S., Li, Y., 2008. New constraints on the early uplift history of theTibetan Plateau. Proceedings of the NationalAcademy of Sciences of the United States of America(PNAS), 105 (13): 4987-4992.

Colin, C.*, Siani, G., Segueni, F., Blamart,D., Giunta, S., Suc, J.-P., Liu, Z.,Frank, N., Briqueu, L., 2008. Restitution de l’histoire de la moussonnord-africaine entre 6,2 et 4,9 Ma et relations possibles avec les événementstardi-Miocène. C. R. Geoscience, 340: 749-760.

Liu,Z.*, Colin, C., Huang, W., Le, K.P., Tong,S., Chen, Z., Trentesaux, A., 2007. Climatic and tectonic controls onweathering in South China and the IndochinaPeninsula: clay mineralogical andgeochemical investigations from the Pearl, Red,and Mekong drainage basins. GeochemistryGeophysics Geosystems, 8, Q05005, doi:10.1029/2006GC001490.

Boulay, S.*, Colin, C., Trentesaux,A., Clain, S., Liu, Z., Lauer-LereddeC., 2007. Sedimentary responses to the Pleistocene climatic variations recordedin the South China Sea. Quaternary Research, 68: 162-172.

Liu, Z.*,Colin, C., Trentesaux, A, 2006. Major element geochemistry of glass shards andminerals of the Youngest Toba Tephra in the southwestern South China Sea.Journal of Asian Earth Sciences, 27 (1): 99-107.

Boulay, S.*,Colin, C., Trentesaux, A., Frank, N., Liu, Z., 2005. Sediment sources andEast Asian monsoon intensity over the last 450 ky. Mineralogical andgeochemical investigations on South China Sea sediments. Palaeogeography,Palaeoclimatology, Palaeoecology, 228: 260-277.

Liu, Z.*,Colin, C., Trentesaux, A., Siani, G., Frank, N., Blamart, D., Farid, S., 2005.Late Quaternary climatic control on erosion and weathering in the easternTibetan Plateau and the Mekong Basin. Quaternary Research, 63 (3): 316-328.

Liu, Z.*, Colin, C., Trentesaux,A., Blamart, D., Bassinot, F., Siani, G., Sicre, M.-A., 2004. Erosionalhistory of the eastern Tibetan Plateau since 190 kyr ago: clay mineralogicaland geochemical investigations from the southwestern South China Sea. MarineGeology, 209 (1-4): 1-18.

Hébert,R.*, Huot, F., Wang, C., Liu, F.,2003. Yarlung Zangbo ophiolites (Southern Tibet)revisited: geodynamic implications from the mineral record. In: Dilek, Y.,Robinson, P. T. (eds.), Ophiolites in Earth History, Geological Society, London, SpecialPublictions, 218: 165-190.

Liu, Z.*,Trentesaux, A., Clemens, S. C., Colin, C., Wang, P., Huang, B., Boulay, S.,2003. Claymineral assemblages in the northern South China Sea: implications for EastAsian monsoon evolution over the past 2 million years. Marine Geology, 201(1-3): 133-146.

Liu, Z., Zhao, X.*, Wang, C., Liu, S., Yi, H.,2003. Magnetostratigraphy of Tertiary sediments from the Hoh Xil Basin: implications for the Cenozoictectonic history of the Tibetan plateau. Geophysical Journal International, 154(2): 233-252.

Trentesaux, A.*, Liu,Z., Colin, C., Boulay, S., Wang, P., 2003. Data report: Pleistocene paleoclimaticcyclicity of southern China: clay mineral evidence recorded in the South ChinaSea (ODP Site 1146). In: Prell, W.L., Wang, P., Blum, P., Fea, D.K., Clemens,S.C. (Eds.), Proceedings of Ocean Drilling Program, Scientific Results, 184:1-10 [Online]. Available from World Wide Web:<http://www-odp.tamu.edu/publications/184_SR/volume/ chapters/210.pdf>.

Huot,F.*, Hébert, R., Varfalvy, V., Beaudoin G., Wang, C., Liu, Z., Cotton, J., Dostal, J., 2002. The Beimarang mélange(southern Tibet)brings additional constraints in assessing the origin, metamorphic evolutionand obduction processes of the Yarlung Zangbo ophiolite. Journal of Asian EarthSciences, 21: 307-322.

Wang,C.*, Liu, Z., Yi, H., Liu, S., Zhao,X., 2002. Tertiary crustal shortening and peneplanation in the Hoh Xil region:implications for the tectonic history of the northern Tibetan plateau. Journalof Asian Earth Sciences, 20 (3): 211-223.

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(*Corresponding author)


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