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文摘
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湘东北中生代发育以辉绿岩类和煌斑岩类为代表的基性岩脉，属陆内拉斑玄武岩系，部分煌斑岩属于碱性系列。岩石富集LREE，δEu负异常不明显，其形成主要受软流圈地幔部分熔融作用制约。煌斑岩类微量元素总体上具有洋岛玄武岩（OIB）岩浆源区特征，富集Nd、P、Cs而K、Rb、Sr、U、Th等富集程度不明显，Ta、Nb略有富集。辉绿岩类表现出Ta、Nb、Ti亏损，但LILE并不富集，反映地壳混染程度的增强。基性岩脉形成于陆内拉张带的构造环境，岩浆活动未受到中生代大洋板块俯冲的影响。基性岩脉在时、空及物质组成上与湘东南玄武质岩石基本一致，属于整个湘东南岩石圈拉张-减薄带的一部分。 |
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其他语种文摘
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Mesozoic mafic dikes developed in Northeastern Hunan Province were represented by the diabases and lamprophyres. Most of them belong to tholeiite series, a part of lamprophyres belong to alkali basalt series. The petrological and geochemical characteristics show the nature of tholeiite series within continental plate. The chondrite-normalized REE patterns are characterized by LREE enrichment. The negative Eu anomalies are not observed. The correlation analysis of La/Sm-La shows that the mafic dikes were controlled by partial melting. The lamprophyres are rich in LILE, Nd, P, Cs, but K, Rb, Sr, U, Th and Ta, Nb are not enriched very obviously. The HFSE: Tb, Y, Yb and Lu are depleted, which have the general characteristics of OIB. The diabases show Ta, Nb and Ti depletion, but LILE are not enriched, so that Ta and Nb depletion expresses the continental matters hydridization. The mafic dikes occurred in the tectonic setting of a intracontinental extension belt. The magmatic activity had been not influenced by the Mesozoic subducting oceanic plate. The mafic dikes corresponded with the basaltic rocks at Southeastern Hunan Province in space and time as well as lithogeochemistry. It was the northeastern part of the lithospheric extension-thinning belt of the whole Southeastern Hunan Province and they should have a same magma source. |
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来源
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大地构造与成矿学
,2002,26(2):179-184 【核心库】
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关键词
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基性岩脉
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岩石地球化学
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陆内拉张带
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湘东北
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地址
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1.
吉林大学地球探测科学与技术学院, 吉林, 长春, 130026
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中科院贵阳地球化学所, 矿床地球化学开放研究实验室, 贵州, 贵阳, 550002
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语种
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中文 |
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文献类型
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研究性论文 |
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ISSN
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1001-1552 |
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学科
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地质学 |
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基金
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中国科学院知识创新工程项目
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中国科学院广州地球化学研究所与南海海洋研究所边缘海地质重点实验室基金
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中国科学院贵阳地球化学研究所矿床地球化学中国科学院重点实验室基金
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文献收藏号
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CSCD:964491
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