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| 1 | 祁连造山带玉石沟地幔橄榄岩中挥发分的流体化学和稳定同位素组成及古大洋岩石圈演化意义显示文摘Fluid inclusions in olivine and orthopyroxene of mantle peridotites from the Yushigou ophiolite can be divided into three types based on decrepitation temperature,shape and distribution.Type-1 fluid inclusions are characterized by oval or negative crystal shapes and small size(<5μm across).They occur in the cores and mantles of the host crystals,and decrepitated at>840℃.Type- 2 fluid inclusions have irregular or tabular shapes with relatively large size(10~100μm in length).They occur in irregular or circular healed micro-fractures in the host crystals,and decrepitated at 612~710℃.Type-3 fluid inclusions have size and shape,similar to type-2 fluid inclusions but occur in micro-fractures restricted to the margins of the host crystals,and decrepitated at much lower temperature from 190℃to 340℃.The three different types of fluid inclusions are interpreted to represent primary,metasomatic (pseudo-secondary)and secondary inclusions,respectively.Stepwise heating reveals three concentration peaks of volatiles at 200~400℃,400~800℃and 800~1200℃released from olivine and orthopyroxene in harzburgite and dunite from the Yushigou ophiolite, which are considered to correspond to the decrepitation of secondary,metasomatic and primary fluid inclusions at similar temperature ranges.CO2 is a major constituent in the volatiles released at three different temperature intervals.Trace amounts of H_2 and N_2 are present in the volatiles released at<800℃and trace amounts of H_2O and SO_2 are mainly present in the volatiles at 400~800℃.TheδD(-95.2‰,-306.3‰)of H_2O and theδ^(13)C(-15.5~-12.5‰)andδ^(18)O values(1.4~1.9‰)of CO_2 released at<800℃are lower than normal mantle values and suggest the mixing origin of crustal fluids( sedimentary organic)with ocean water,implying that Yushigou AOLM had undergone an intensive metasomatism by a fluid composed of CO_2.H_2O and SO_2,and followed by degassing. In contrast,the volatiles released at 800~1200℃are characterized by trace amounts of H_2 and CO in dunite and SO_2 in harzburgite, much lighterδ^(13)C(-29.1‰~-19.5‰),heavierδ^(13)O(8.8‰)of CO_2 and positive relationship between these isotopic ratios and the concentration of CO_2.Such features can be best explained by mixing of significant terrestrial crustal(organic)and minor mantle volatiles.We proposed that the Yishigou peridotites are more likely to have derived from a continental lithosphere instead of an oceanic lithosphere comprising the Yishigou gabbros and pillowed basalts.A supra-subduction tectonic setting is thus inferred for the Yushigou ophiolite. | 胡沛青 张铭杰 汤中立 LI Chusi 王记周 | 2007 | 岩石学报2007，23，1： | 8 |
| 2 | Mineralogical, petrological, and geochemical studies of the Limahe mafic–ultramatic intrusion and associated Ni–Cu sulfide ores, SW China显示文摘 | Yan Tao Chusi Li Xie-Yan Song Edward M. Ripley | 2008 | Mineralium Deposita2008，，8： | 1 |
| 3 | Petrogenesis of the Pt–Pd mineralized Jinbaoshan ultramafic intrusion in the Permian Emeishan Large Igneous Province, SW China显示文摘 | Yan Tao Chusi Li Ruizhong Hu Edward M. Ripley Andao Du Hong Zhong | 2007 | Contributions to Mineralogy and Petrology2007，，3： | 1 |
| 4 | Zircon dating, Hf–Sr–Nd–Os isotopes and PGE geochemistry of the Tianyu sulfide-bearing mafic–ultramafic intrusion in the Central Asian Orogenic Belt, NW China显示文摘 | Dongmei Tang Kezhang Qin Chusi Li Liang Qi Benxun Su Wenjun Qu | 2011 | LITHOS2011，，1： | 1 |
| 5 | Critical factors for the formation of a nickel–copper deposit in an evolved magma system: lessons from a comparison of the Pants Lake and Voisey’s Bay sulfide occurrences in Labrador, Canada显示文摘 | Chusi Li Anthony J. Naldrett Edward M. Ripley | 2001 | Mineralium Deposita2001，，1： | 1 |
| 6 | Petrogenesis of the Pt-Pd mineralized Jin- baoshan ultramafic intrusion in the Permian Emeishan Large Igneous Province, SW China 显示文摘 | Tao Yan Li Chusi Hu Ruizhong Ripley E M Du Andao Zhong Hong | 2007 | Contrib Mineral Petrol2007，153，3： | 1 |
| 7 | Critical factors for the formation of a nickel–copper deposit in an evolved magma system: lessons from a comparison of the Pants Lake and Voisey’s Bay sulfide occurrences in Labrador, Canada显示文摘 | Chusi Li Anthony J. Naldrett Edward M. Ripley | 2001 | Mineralium Deposita2001，，1： | 1 |
| 8 | Compositional variations of olivine from the Jinchuan Ni–Cu sulfide deposit, western China: implications for ore genesis显示文摘 | Chusi Li Zhanghua Xu Sybrand A. Waal Edward M. Ripley Wolfgang D. Maier | 2004 | Mineralium Deposita2004，，2： | 1 |
| 9 | Critical factors for the formation of a nickel–copper deposit in an evolved magma system: lessons from a comparison of the Pants Lake and Voisey’s Bay sulfide occurrences in Labrador, Canada显示文摘 | Chusi Li Anthony J. Naldrett Edward M. Ripley | 2001 | Mineralium Deposita2001，，1： | 1 |
| 10 | Compositional variations of olivine from the Jinchuan Ni–Cu sulfide deposit, western China: implications for ore genesis显示文摘 | Chusi Li Zhanghua Xu Sybrand A. Waal Edward M. Ripley Wolfgang D. Maier | 2004 | Mineralium Deposita2004，，2： | 1 |
| 11 | O-Sr-Nd同位素对峨眉山大火成岩省中含钒钛磁铁矿岩体成因的制约显示文摘在我国西南地区的峨眉山大火成岩省内带,发育有一系列含钒钛磁铁矿的基性-超基性层状侵入岩体,例如攀枝花,白马,太和,红格等。虽然前人已经做了大量的研究,这些含矿岩体的成因仍然有争议。例如,地壳混染,特别是岩浆在侵位过程中碳酸岩围岩分解以及富CO2流体的加入是否对Fe-Ti氧化物结晶产生影响尚有不同意见。为解决上述问题,本次研究针对上述四个典型的含矿岩体及其围岩进行了系统的O-Sr-Nd同位素研究。研究结果表明。 | 于宋月 宋谢炎 E.M.Ripley Chusi Li 陈列锰 佘宇伟 栾燕 | 2015 | 矿物学报2015，35，S1： | 1 |
| 12 | Empirical equations to predict the sulfur content of mafic magmas at sulfide saturation and applications to magmatic sulfide deposits显示文摘 | Chusi Li Edward M. Ripley | 2005 | Mineralium Deposita2005，，2： | 1 |
| 13 | Critical factors for the formation of a nickel–copper deposit in an evolved magma system: lessons from a comparison of the Pants Lake and Voisey’s Bay sulfide occurrences in Labrador, Canada显示文摘 | Chusi Li Anthony J. Naldrett Edward M. Ripley | 2001 | Mineralium Deposita2001，，1： | 1 |
| 14 | Stable isotope, fluid inclusion, and mineral chemistry constraints on contamination and hydrothermal alteration in the Uitkomst Complex, South Africa显示文摘 | Arindam Sarkar Edward M. Ripley Chusi Li Wolfgang D. Maier | 2008 | Chemical Geology2008，，1： | 1 |
| 15 | Medicinal plant knowledge and its erosion among the Mien (Yao) in northern Thailand显示文摘 | Kamonnate Srithi Henrik Balslev Prasit Wangpakapattanawong Prachaya Srisanga Chusie Trisonthi | 2009 | Journal of Ethnopharmacology2009，，2： | 1 |
| 16 | Maternalobesityandriskofgestationaldiabetesmellitus显示文摘 | ChuSY CallaghanWM Kim SY etal | 2007 | DiabetesCare2007，30，8： | 1 |
| 17 | Petrogenesis of the Pt–Pd mineralized Jinbaoshan ultramafic intrusion in the Permian Emeishan Large Igneous Province, SW China显示文摘 | Yan Tao Chusi Li Ruizhong Hu Edward M. Ripley Andao Du Hong Zhong | 2007 | Contributions to Mineralogy and Petrology2007，，3： | 1 |
| 18 | Geochronology, petrology and Hf-S isotopes of the newly-discovered, world- class Xiarihamu magmatic Ni-Cu disposit in the Qinghai-Tibet plateau, western China显示文摘 | Li Chusi Zhang Zhaowei Li Wenyuan | 2015 | Lithos2015，21，6217： | 1 |
| 19 | Platinum-group elements in the oxide layers of the Hongge mafic–ultramafic intrusion, Emeishan Large Igneous Province, SW China显示文摘 | Zhong-Jie Bai Hong Zhong Chusi Li Wei-Guang Zhu Gui-Wen Xu | 2012 | Ore Geology Reviews2012，，： | 1 |
| 20 | Exploring the relationships of trust and commitment in supply chain management 显示文摘 | Chusy Fang W C | 2006 | Journal of American Academy of Business2006，，1： | 1 |
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