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闽北角闪辉长岩的地球化学特征及其地球动力学意义
GEOCHEMICAL CHARACTERISTICS OF BOJITE IN NORTHERN FUJIAN PROVINCE AND THEIR GEODYNAMIC SIGNIFICANCE

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张贵山 1   温汉捷 2   李石磊 3   胡瑞忠 2   裘愉卓 2  
文摘 赤门角闪辉长岩是中国东南部晚白垩世末基性岩浆活动的产物,分布在福建省南平市的北部,总体呈近NS向展布.岩石属于低钾(拉斑)岩石系列,富Al、Na_2O>K_2O的特征,岩浆演化过程中经历了以橄榄石、辉石、斜长石和Ti-Fe氧化物的分离结晶作用.赤门角闪辉长岩具相对富集大离子亲石元素(LILE)和轻稀土元素(LREE)、亏损高场强元素(HFSE)的特性, 不相容元素蛛网图显示出消减带岩石的地球化学性质,以Nb、Ta、Ti负异常为特征.微量元素地球化学研究表明,赤门角闪辉长岩浆在上升侵位过程中未发生地壳物质混染,来自不含石榴石的富集岩石圈地幔岩部分熔融的产物,地幔源区的演化与太平洋板块俯冲密切相关.赤门角闪辉长岩形成于大陆拉张带-陆内初始裂谷的过渡环境.综合晚中生代的基性岩类资料,与形成较早的沿海辉长岩对比研究,赤门角闪辉长岩是拉张向裂谷转换体制下形成的过渡岩石类型,标志初始裂谷活动的开始.
其他语种文摘 The Chimen bojite with a nearly NS strike, was a product of mafic magma activity in southeastern China at the end of Late Cretaceous. And it is spreaded in the northern part of Nanping City in Fujian Province. It belongs to low-K ( tholeiite) rock series characterized by high Al contents and Na_2O>K_2O, possibly resultant from fractional crystallization of olivine, clinopyroxene, plagioclase and titanium-iron oxide. These stocks are significantly enriched in LILE (such as K, Rb, Ba, Th , and U ) and LREE, depleted in HFSE (Nb, Ta, Zr, Hf). In the primary mantle-normalized spidergram, they show the geochemical features of subduction-zone rocks and negative Nb, Ta, Ti anomalies . The results of trace element geochemical study indicated that the bojite was not contaminated by crustal material during emplacement it was derived from partial melting of garnet-free enriched lithospheric mantle, and the evolution of the mantle source region is closely related with the subduction of the Pacific plate. The Chimen bojite was formed in the geodynamic setting between the crustal extension belt and the continental initial rift. In combination with the results of geological studies for the Late Mesozoic mafic igneous rocks in SE China, it is suggested that the Chimen bojite belongs to the transitional rock series in the transitional zone from the crustal extension belt to the continental initial rift, which may be used to trace rift start up when compared to the coastal gabbro.
来源 矿物学报 ,2009,29(2):243-252 【核心库】
关键词 角闪辉长岩 ; 地球化学 ; 富集地幔 ; 福建
地址

1. 长安大学,地球科学与资源学院, 陕西, 西安, 710054  

2. 中国科学院地球化学研究所, 矿床地球化学国家重点实验室, 贵州, 贵阳, 550002  

3. 四川省川威集团有限公司, 四川, 内江, 642469

语种 中文
文献类型 研究性论文
ISSN 1000-4734
学科 地质学
基金 国家973计划 ;  中国科学院知识创新工程项目
文献收藏号 CSCD:3597212

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引证文献 13

1 唐立梅 海南岛三叠纪中基性岩的年代学、地球化学及其地质意义 地质科学,2010,45(4):1139-1155
被引 18

2 唐立梅 海南岛中三叠世造山后伸展作用:双峰式侵入岩的年代学及地球化学制约 中国科学. 地球科学,2013,43(3):433-445
被引 10

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论文科学数据集

1. 武当地体奥陶纪和三叠纪镁铁质岩墙锆石年龄和地球化学组成数据

2. 长江中下游成矿带池州铜钼多金属矿床形成的年代学和地球化学制约因素地球化学分析图集

3. 江西南部早侏罗世A型流纹岩和高镁安山岩数据(~190 Ma)

数据来源:
国家青藏高原科学数据中心
PlumX Metrics
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