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中文摘要：
拟综合采用传统的岩石学和现代地球化学分析方法和先进的微区原位分析技术，对华北克拉通不同地区古、中、新生代典型岩浆活动的产物及其携带的深源岩石捕虏体和矿物捕虏晶开展详细的岩石学与地球化学综合研究，尤其是对一些有争议的热点和难点问题组织联合野外考查和踪和诊断，进一步揭示华北地区岩浆活动及其所反映的岩石圈的时空演化规律。在此基础上，集成《华北克拉通破坏》重大研究计划启动以来获得的所有岩石学和地球化学观察结果，根据这些观察结果进一步厘定华北克拉通的破坏过程及其动力学，为最终揭示华北克拉通的破坏过程及其动力来源提供明确的岩石学和地球化学制约。结合地质学和地球物理学证据提出华北克拉通破坏过程及其动力学模型。力争提升人类对大陆形成与演化的认知水平。
英文摘要：
Integrated study；North China Craton；Compositional transformation of the lithosphere；Lower crust destruction；Pacific plate subduction
结论摘要：
本项目在华北大陆形成与演化、下地壳和岩石圈地幔改造与破坏、克拉通破坏机制等方面取得如下重要成果1、发现华北大陆壳最早形成于冥古宙（>40亿年），但太古代存在多期大陆形成与再造过程。正是始太古到新太古多期大规模地壳增生和再造过程强烈地破坏了冥太古－始太古克拉通核，导致冥太古－始太古地壳保存很少；2、发现华南最老岩石形成于33亿年；3、证明华北下地壳形成于晚太古，但显生宙以来类似于岩石圈地幔遭受了多期以岩浆底侵作用为代表的构造事件的改造和破坏。同时下地壳麻粒岩中太古代锆石的Hf-O同位素研究进一步证明太古代末期华北下地壳可能就存在上地壳物质的再循环；4、华北东南缘中生代发现下地壳加厚的证据，并首次提出了通道流模型；5、通过非传统稳定同位素（Li-Fe-Mg）、Re-Os同位素和全球对比研究进一步证明橄榄岩-熔体相互作用造成岩石圈地幔改造和破坏具有全球普适性；6、发现硅酸盐熔体交代和碳酸盐熔体交代造成的Li含量和同位素组成存在巨大差异；7、厘定了华北岩石圈地幔不同时期的水含量，证明中生代岩石圈地幔比新生代岩石圈地幔富水；8、发现中国东部中-新生代玄武岩源区中再循环洋壳组分，提供了太平洋板块俯冲影响东亚大陆岩石圈演化的关键证据；9、发表SCI论文59篇（其中第一标注12篇；第二标注30篇；第三标注15篇；第四标注2篇）；10、成功举办了“华北克拉通形成与破坏”国际学术研讨会，并在Lithos和Gondwana Resaerch上出版专辑两部。
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期刊论文
Process and mechanism of mountain-root removal of the Dabie Orogen－Constraints from geochronology an
Fe isotope evidence for multistage melt-peridotite interactions in the lithospheric mantle of the ea
Triassic “adakitic” rocks in an extensional setting (North China): Melts from the cratonic lower cru
The Cretaceous adakitic-basaltic- granitic magma sequence in south-eastern margin of the North China
Breakdown of orthopyroxene contributing to melt pockets in mantle peridotite xenoliths from the West
Hadean to Neoarchean episodic crustal growth: Detrital zircon records in Paleoproterozoic quartzites
Neoarchean recycling of 18O-enriched supracrustal materials into the lower crust: Zircon record from
Water content in the early Cretaceous lithospheric mantle beneath the south-central Taihang Mountain
Water contents of the Cenozoic lithospheric mantle beneath the western part of the North China Crato
Two tales of the continental lithospheric mantle prior to the destruction of the North China Craton:
Multistage melt/fluid-peridotite interactions in the refertilized lithospheric mantle beneath the No
Changing recycled oceanic components in the mantle source of the Shuangliao Cenozoic basalts, NE Chi
Constraints from melt inclusions and their host olivines on the petrogenesis of Oligoence-Early Mioc
Phenocryst He-Ar isotopic and whole-rock geochemical constraints on the origin of crustal components
Abnormal lithium isotope composition from the ancient lithospheric mantle beneath the North China Cr
Episodic widespread magma underplating beneath the North China Craton in the Phanerozoic: Implicatio
Mantle upwelling during Permian to Triassic in the northern margin of the North China Craton: Constr
Recycled oceanic crust in the source of 90-40 Ma basalts in North China Craton: Evidence, provenance
Temporal variation of H2O content in the lithospheric mantle beneath the eastern North China Craton:
The distribution of water in the continental lithospheric mantle and its implications for the stabil
Melt-peridotite interaction in the Pre-Cambrian mantle beneath the western North China Craton: Petro
The hydrous properties of subcontinental lithospheric mantle: Constraints from water content and hyd
Titanite evidence for Triassic thickened lower crust along southeastern margin of North China Craton
Slab-mantle interaction for thinning of cratonic lithospheric mantle in North China: Geochemical evi
Petrology, geochemistry and Re-Os isotopes of peridotite xenoliths from Yantai, Shandong Province: E
Evolution of the Archean and Paleoproterozoic lower crust beneath the Trans-North China Orogen and t
Destruction of ancient lower crust through magma underplating beneath Jiaodong Peninsula, North Chin
Guangtoushan granites and their enclaves: Implications for Triassic mantle upwelling in the northern
Recognizing juvenile and relict lithospheric mantle beneath the North China Craton: Combined analysi
Diverse crustal components in pyroxenite xenoliths from Junan, Suluorogenic belt: Implications for l
Petrology and geochemistry of peridotite xenoliths from the Lianshan region: Nature and evolution of
Coexistence of the moderately refractory and fertile mantle beneath the eastern Central Asian Orogen
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