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张宏福
中国科学院院士，浙江大学教授，中国科学院地质与地球物理研究所研究员
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详细介绍
张宏福
中国科学院院士，浙江大学教授，中国科学院地质与地球物理研究所研究员
个人履历：
张宏福：男，1962年9月出生，陕西山阳县人，岩石地球化学家，中国科学院院士，浙江大学地球科学学院教授、博士生导师，中国科学院地质与地球物理研究所研究员，西北大学大陆动力学国家重点实验室常务副主任，国家杰出青年科学基金获得者，享受国务院政府特殊津贴，国家有突出贡献专家。1985年从西北大学地质系本科毕业；1988年获得武汉地质学院北京研究生部硕士学位后，进入西北大学工作，先后担任助教、讲师；1998年获得英国伦敦大学皇家霍洛威学院地质学系理学博士学位，之后回国进入中国科学院地质与地球物理研究所工作；2002年获得国家杰出青年科学基金资助；2010年担任西北大学大陆动力学国家重点实验室常务副主任；2017年当选为中国科学院院士。张宏福院士长期从事岩石圈地幔和下地壳研究。以深源岩石及其捕虏体为对象，探索地幔与地壳、软流圈与岩石圈相互作用的内在机理和外部因素，揭示大陆岩石圈的演化过程。在大陆深部物质和能量交换的内在机理、外部控制因素、非传统稳定同位素三个方面取得系统性创新成就。特别是提出并论证了证明橄榄岩—熔体相互作用造成的岩石圈地幔组成的变化是导致古老克拉通能够被破坏的本质。先后承担多项国家、中国科学院和部委重大研究计划、重点、“百人计划”等项目；先后发表论文189篇，其中SCI收录152篇。论文被SCI引用5731次（他引4590次），H-index为38；为6篇ISI地球科学Top1%高引用率论文作者。曾获国家自然科学奖二等奖两项和中国科学院杰出科技成就奖。
论文代表：
Neoarchean recycling of 18O-enriched supracrustal materials into the lower crust: Zircon record from the North China Craton. Precambrian Research 248(2014), 60-71.
Hadean to Neoarchean episodic crustal growth: Detrital zircon records in Paleoproterozoic quartzites from the southern North China Craton. Precambrian Research 254(2014), 245-257.
The meta-gabbroic complex of Fushui in north Qinling orogen: A case of syn-subduction mafic magmatism. Gondwana Research (2014), dx.doi.org/10.1016/j.gr.2014.04.010.
Construction and destruction of cratons: Preface. Gondwana Research 23(2013), 1-3.
Episodic widespread magma underplating beneath the North China Craton in the Phanerozoic: Implications for craton destruction. Gondwana Research 23(2013), 95-107.
Episodic growth of Precambrian lower crust beneath the North China Craton: A synthesis. Precambrian Research 222-223(2012), 255-264.
Melt-peridotite interaction in the Pre-Cambrian mantle beneath the western North China Craton: Petrology, geochemistry and Sr, Nd and Re isotopes. Lithos 149(2012), 100-114.
Destruction of ancient lower crust through magma underplating beneath Jiaodong Peninsula, North China Craton: U-Pb and Hf isotopic evidence from granulite xenoliths. Gondwana Research 21(2012), 281-292.
Evolution of the Archean and Paleoproterozoic lower crust beneath the Trans-North China Orogen and the Western Block of the North China Craton. Gondwana Research 22(2012), 73-85.
Santosh M. Phanerozoic reactivation of the Archean North China Craton through episodic magmatism: Evidence from zircon U-Pb geochronology and Hf isotopes from the Liaodong Peninsula. Gondwana Research 19(2011), 446-459.
Melt/rock interaction in remains of refertilized Archean lithospheric mantle in Jiaodong Peninsula, North China Craton: Li isotopic evidence. Contributions to Mineralogy and Petrology 160(2010), 261-277.
The origin of Mengyin and Fuxian diamondiferous kimberlites from the North China Craton: Implication for Palaeozoic subducted oceanic slab-mantle interaction. Journal of Asian Earth Sciences 37(2010), 425-437.
Recycled crustal melt injection into lithospheric mantle: implication from cumulative composite and pyroxenite xenoliths. International Journal of Earth Sciences 99(2010), 1167-1186.
Comprehensive refertilization of lithospheric mantle beneath the North China Craton: further Os-Sr-Nd isotopic constraints. Journal of the Geological Society, London 166(2009), 249-259.
Evolution of subcontinental lithospheric mantle beneath eastern China: Re-Os isotopic evidence from mantle xenoliths in Paleozoic kimberlites and Mesozoic basalts. Contributions to Minerology and Petrology 155(2008), 271-293.
Importance of melt circulation and crust-mantle interaction in the lithospheric evolution beneath the North China Craton: Evidence from Mesozoic basalt-borne clinopyroxene xenocrysts and pyroxenite xenoliths. Lithos 96(2007), 67-89.
Transformation of subcontinental lithospheric mantle through peridotite-melt reaction: Evidence from a highly fertile mantle xenolith from the North China Craton. International Geology Review 49(2007), 658-679.
Transformation of lithospheric mantle through peridotite-melt reaction: a case of Sino-Korean craton. Earth and Planetary Science Letters 237(2005), 768-780.
Geochemical constraints on the origin of Mesozoic alkaline intrusive complexes from the North China Craton and tectonic implications. Lithos 81(2005), 297-317.
Highly heterogeneous Late Mesozoic lithospheric mantle beneath the North China Craton: evidence from Sr-Nd-Pb isotopic systematics of mafic igneous rocks. Geological Magazine 141(2004), 55-62.
Secular evolution of the lithosphere beneath the eastern North China Craton: evidence from Mesozoic basalts and high-Mg andesites. Geochimica et Cosmochimica Acta 67(22)(2003), 4373-4387.
Mixed mantle provenance: diverse garnet compositions in polymict peridotites, Kaapvaal craton, South Africa. Earth and Planetary Science Letters 216(2003), 329-346.
Mesozoic lithosphere destruction beneath the North China Craton: evidence from major, trace element, and Sr-Nd-Pb isotope studies of Fangcheng basalts. Contributions to Mineralogy and Petrolology 144(2002), 241-253.
Geochemistry of Mesozoic basalts and mafic dikes in southeastern North China Craton, and tectonic implication. International Geology Review 44(2002), 370-382.
Cratonic peridotites and silica-rich melts: Diopside-enstatite relationships in polymict xenoliths, Kaapvaal, South Africa. Geochimica et Cosmochimica Acta 65(2001), 3365-3377.
Mineralogy and geochemistry of oxide minerals in polymict xenoliths from the Bultfontein kimberlites, South Africa: implication for low bulk-rock oxygen isotopic ratios. Contributions to Mineralogy and Petrology 141(2001), 367-379.
Geochemical significance of a garnet lherzolite from the Dahongshan kimberlite, Yangtze Craton, southern China. Geochemical Journal 35(2001), 315-331.
Recent fluid processes in the Kaapvaal Craton, South Africa: coupled oxygen isotope and trace element disequilibrium in polymict peridotites. Earth and Planetary Science Letters 176(2000), 57-72.
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