胶莱盆地晚白垩世不同地幔源区的两种基性岩浆——诸城玄武岩和胶州玄武岩的对比

孟繁聪 李天福 薛怀民 刘福来 许志琴. 胶莱盆地晚白垩世不同地幔源区的两种基性岩浆——诸城玄武岩和胶州玄武岩的对比[J]. 岩石学报, 2006, 22(6): 1644-1656.
引用本文: 孟繁聪 李天福 薛怀民 刘福来 许志琴. 胶莱盆地晚白垩世不同地幔源区的两种基性岩浆——诸城玄武岩和胶州玄武岩的对比[J]. 岩石学报, 2006, 22(6): 1644-1656.
MENG FanCong, LI TianFu, XUE HuaiMin, LIU FuLai , XU ZhiQin. Two serials of basic magmas from different mantle sources of Late Cretaceous in east Shandong province,China:A comparative study on basalts from Zhucheng and Jiaozhou.[J]. Acta Petrologica Sinica, 2006, 22(6): 1644-1656.
Citation: MENG FanCong, LI TianFu, XUE HuaiMin, LIU FuLai , XU ZhiQin. Two serials of basic magmas from different mantle sources of Late Cretaceous in east Shandong province,China:A comparative study on basalts from Zhucheng and Jiaozhou.[J]. Acta Petrologica Sinica, 2006, 22(6): 1644-1656.

胶莱盆地晚白垩世不同地幔源区的两种基性岩浆——诸城玄武岩和胶州玄武岩的对比

  • 基金项目:

    本文受国家重点基础研究发展规划项目(批准号:2003CB716502)和国家自然科学基金重大项目(批准号:40399143)及中国地质科学院重点开放实验室专项资金(KL05-2)的瓷助.

Two serials of basic magmas from different mantle sources of Late Cretaceous in east Shandong province,China:A comparative study on basalts from Zhucheng and Jiaozhou.

  • 采用全岩K-Ar法获得山东省胶莱盆地诸城玄武岩的形成年龄为76M,胶州玄武岩的形成年龄为72Ma,代表了发生在晚白垩世的地幔岩浆事件,但两地岩浆产物具有不同的地球化学性质。诸城玄武岩主要为粗面玄武岩,富集轻稀土元素(LREE),微量元素组成类似于洋岛玄武岩(OIB),(^87Sr/^86Sr)t=0.7060-0.7080,εNd(t)=-3.0--5.1,介于洋岛玄武岩和中生代富集的岩石圈地幔之间,表明软流圈来源的岩浆中混入了富集岩石圈地幔来源的岩浆,是软流圈地幔与岩石圈地幔相互作用的结果。胶州玄武岩主要为碱性玄武岩,比诸城玄武岩更富集轻稀土元素,微量元素组成类似于诸城玄武岩,但Nb、Ta、Ti等高场强元素不显示亏损,Sr-Nd同位素组成也存在明显差别,(^87Sr/^86Sr)t=0、70350-0.70355,εNd(t)=5.4-5.8,与山东省新生代火山岩的地球化学特征类似,类似于洋岛玄武岩(OIB),表明岩浆起源于亏损的软流圈地幔。研究显示出晚白垩世以来胶莱盆地软流圈地幔不均匀上涌和逐渐成为玄武岩浆主要源区的趋势。
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收稿日期:  2004-07-23
修回日期:  2006-01-09
刊出日期:  2006-06-30

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