| 中太平洋CA海山玄武岩中斜长石化学成分特征及地质意义 |
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| 引用本文： | 何欣,孙国胜,初凤友,王春光,晋瑞香,李洋,战乃臣,刘世伟,孙九达. 中太平洋CA海山玄武岩中斜长石化学成分特征及地质意义[J]. 海洋学研究, 2017, 35(2): 23-32. DOI: 10.3969/j.issn.1001-909X.2017.02.003 |
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| 作者姓名： | 何欣 孙国胜 初凤友 王春光 晋瑞香 李洋 战乃臣 刘世伟 孙九达 |
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| 作者单位： | 1.吉林大学 地球科学学院,吉林 长春 130061; 2.国家海洋局 第二海洋研究所,浙江 杭州 310012; 3.吉林省地质勘查基金管理中心,吉林 长春 130061 |
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| 基金项目： | 国家自然科学基金面上项目资助(41176045) |
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| 摘 要： | 在对CA海山玄武岩CAD21样品岩相学研究基础上,运用电子探针和X-荧光光谱法(XRF)对中太平洋CA海山斜长石斑晶中的环带、斜长石微晶和玄武岩中的硅酸盐进行了化学成分研究。CA海山玄武岩为地幔柱成因的板内玄武岩;斜长石斑晶具有环带结构,环带核部与边部为不连续消光,是不连续环带;环带核部为培长石,边部为拉长石,是岩浆演化过程中形成的正环带,其成因受岩浆演化过程中熔体组分及温、压条件的共同制约。斜长石斑晶核部、边部及斜长石微晶估算温度平均值分别为1 281,1 198和1 071 ℃,分别代表了岩浆源区、岩浆房及岩浆喷发温度,三者温度差值较小,这和洋岛玄武质岩浆的形成及喷发特点相吻合。
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| 关 键 词： | CA海山 玄武岩 斜长石 环带 结晶温度 |
| 收稿时间： | 2017-01-20 |
Chemical characteristics and geological implication of plagioclase in CA Seamount basalts from the Middle Pacific |
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| HE Xin,SUN Guo-sheng,CHU Feng-you,WANG Chun-guang,JIN Rui-xiang,LI Yang,ZHAN Nai-chen,LIU Shi-wei,SUN Jiu-da. Chemical characteristics and geological implication of plagioclase in CA Seamount basalts from the Middle Pacific[J]. Journal of Marine Sciences, 2017, 35(2): 23-32. DOI: 10.3969/j.issn.1001-909X.2017.02.003 |
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| Authors: | HE Xin SUN Guo-sheng CHU Feng-you WANG Chun-guang JIN Rui-xiang LI Yang ZHAN Nai-chen LIU Shi-wei SUN Jiu-da |
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| Affiliation: | 1. College of Earth Sciences, Jilin University, Changchun 130061, China; 2. Second Institute of Oceanography, SOA, Hangzhou 310012, China; 3. Geological Exploration Fund Management Center of Jilin Province, Changchun 130061, China |
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| Abstract: | Chemical composition of plagioclase phenocryst zone, plagioclase crystallite and silicate of basalts in CA Seamount (sample CAD21), was examined using EPMA method and X-Ray fluorescence spectrometry (XRF) on basis of petrography. The basalts of CA Seamount are intraplate basalts formed by the activity of mantle plume. The core and the edge of zones of plagioclase phenocrysts show nonsequence optical extinction phenomenon, indicating a discontinuous zoning structure. The sequence of zones is labradorite to bytownite from edge to core, showing a normal zoning in the process of magmatic evolution. Such a phenomenon is constrained by melt composition and temperature-pressure condition. Average temperatures of plagioclase phenocrysts are 1 281 ℃(temperature of magmatic source),1 198℃(temperature of magmatic chamber) and 1 071 ℃(temperature of magmatic exhalation) respectively. The small temperature difference indicates a rapidly eruption process, in accord with the formation and eruption characteristics of oceanic island basalt magma. |
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| Keywords: | CA Seamount basalt plagioclase zoning crystallization temperature |
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