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Olivine and melt inclusion chemical constraints on the source of intracontinental basalts from the eastern North China Craton: Discrimination of contributions from the subducted Pacific slab

机译：华北克拉通东部大陆内玄武岩来源的橄榄石和熔体夹杂物化学约束：俯冲太平洋板块贡献的区分

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Li Hong-Yan; Xu Yi-Gang; Ryan Jeffrey G.; Huang Xiao-Long; Ren Zhong-Yuan; Guo Hua; Ning Zhen-Guo;
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1. Olivine and melt inclusion chemical constraints on the source of intracontinental basalts from the eastern North China Craton: Discrimination of contributions from the subducted Pacific slab [J] . Li Hong-Yan, Xu Yi-Gang, Ryan Jeffrey G., Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society . 2016,第Null期

机译：华北克拉通东部大陆内玄武岩来源的橄榄石和熔体夹杂物化学约束：俯冲太平洋板块贡献的区分
2. Chemical and Pb isotope composition of olivine-hosted melt inclusions from the Hannuoba basalts, North China Craton: Implications for petrogenesis and mantle source [J] . Qian Sheng-Ping, Ren Zhong-Yuan, Zhang Le, Chemical geology . 2015,第Null期

机译：华北克拉通汉诺巴玄武岩中橄榄石包裹的熔融包裹体的化学和铅同位素组成：对成岩作用和地幔源的影响
3. Constraints from melt inclusions and their host olivines on the petrogenesis of Oligocene-Early- Miocene Xindian basalts, Chifeng area, North China Craton [J] . L.-B. Hong, Y.-H. Zhang, S.-P. Qian Contributions to Mineralogy and Petrology . 2013,第2期

机译：华北克拉通赤峰地区渐新世-早中新世新店玄武岩的熔融包裹体及其宿主橄榄石的成因
4. MELT INCLUSIONS IN CLINOPYROXENE PHENOCRYSTS FROM MAFIC DIKES IN THE EASTERN NORTH CHINA CRATON: CONSTRAINTS ON MELT EVOLUTION [C] . Cai Ya-Chun, Fan Hong-Rui, Santosh M., Asia Current Research on Fluid Inclusion Fifth Meeting . 2014

机译：华北克拉通东部基性岩中次生辉石中的熔体夹杂物：熔体演化的约束
5. Chemical and Pb isotope composition of olivine-hosted melt inclusions from the Hannuoba basalts, North China Craton: Implications for petrogenesis and mantle source [O] . Li GY, Liu XL, An JB, 2015

机译：华北克拉通汉诺巴玄武岩中橄榄石包裹的熔融包裹体的化学和铅同位素组成：对成岩作用和地幔源的影响

Olivine and melt inclusion chemical constraints on the source of intracontinental basalts from the eastern North China Craton: Discrimination of contributions from the subducted Pacific slab

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