银根 额济纳旗盆地苏红图坳陷早白垩世火山岩幔源特征
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国家自然科学基金项目(面上项目,重点项目,重大项目),国家重点基础研究发展计划(973计划)


The Mantle source characteristics of volcanic of Suhogntu Depression in Inggen-Ejin Qi Basin
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    摘要:

    银根-额济纳旗盆地在早白垩世火山喷发强烈,形成了一套中基性火山岩。通过对野外采集样品的地球化学特征进行分析,苏红图火山岩属高钾玄武岩。根据火山岩地球化学特征分析岩浆来源于富集岩石圈地幔,在岩浆上升过程中没有经历明显的地壳物质混染。最后,通过将研究区与位于华北板块北缘的四子王旗及辽西义县组火山岩的地化特征对比研究认为,地跨四个性质不同的大地构造单元的银-额盆地地块岩浆源区特征是亲华北型的,或是在它下方有一独立的和华北板块相似的富集地幔源区。

    Abstract:

    Inggen-Ejin Qi Basin in the Early Cretaceous volcanic eruptions strongly, forming a set of basic volcanic rocks. Samples collected in the field by the geochemical analysis of volcanic rocks belong to high-K basalt Suhongtu. According to the study area volcanic geochemistry of volcanic rocks derived from enriched mantle in the formation process has not experienced significant crustal contamination. Finally, the northern margin of the North China craton, volcanic regions were compared by study area and is located in the northern margin of North China plate Yixian Formation in western Liaoning Siziwangqi and geochemical characteristics of volcanic rocks of comparative study that across four different nature of the earth structural units of silver - the amount of land is a pro-North China Basin by, or under that have a similar independent and North China plates enriched mantle source.

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钟福平,钟建华,由伟丰.2011.银根 额济纳旗盆地苏红图坳陷早白垩世火山岩幔源特征[J].地质学报,85(12):2003-2013.
ZHONG Fuping, ZHONG Jianhua, YOU Weifeng.2011. The Mantle source characteristics of volcanic of Suhogntu Depression in Inggen-Ejin Qi Basin[J]. Acta Geologica Sinica,85(12):2003-2013.

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  • 收稿日期:2010-05-19
  • 最后修改日期:2011-10-14
  • 录用日期:2011-10-17
  • 在线发布日期: 2011-12-09
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