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银根 额济纳旗盆地苏红图坳陷早白垩世火山岩幔源特征
引用本文:钟福平,钟建华,由伟丰.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,2011,85(12):2003-2013.
作者姓名:钟福平  钟建华  由伟丰
作者单位:1. 河南理工大学安全科学与工程学院瓦斯地质研究所,河南焦作,454003
2. 中国科学院广州地球化学研究所,广州,510640;中国石油大学(华东)地球资源与信息学院,山东东营,257061
3. 中国石油化工股份有限公司石油勘探开发研究院,北京,100083
基金项目: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)
摘    要:银根-额济纳旗盆地位于塔里木、哈萨克斯坦、西伯利亚和华北四个板块的结合部位,在早白垩世发生了强烈的火山喷发,形成了一套中基性火山岩.野外和室内研究表明,该盆地中的苏红图火山岩属高钾玄武岩,岩浆来源于富集软流圈地幔,岩浆上升过程中没有经历明显的地壳物质混染.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球...

关 键 词:银根-额济纳旗盆地  苏红图坳陷  高钾玄武岩
收稿时间:2010/5/19 0:00:00
修稿时间:2011/10/14 0:00:00

The Mantle source characteristics of volcanic of Suhogntu Depression in Inggen-Ejin Qi Basin
ZHONG Fuping,ZHONG Jianhua and YOU Weifeng.The Mantle source characteristics of volcanic of Suhogntu Depression in Inggen-Ejin Qi Basin[J].Acta Geologica Sinica,2011,85(12):2003-2013.
Authors:ZHONG Fuping  ZHONG Jianhua and YOU Weifeng
Institution:Guangzhou Institute of Geochermistry, Chinese Academy of Science, Guangzhou
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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