文章摘要
管育春,杨宗锋,祝新友,邹滔,程细音,唐雷,邓海辉.内蒙古北大山杂岩体成因及其地质意义[J].矿产勘查,2017,8(6):1054-1068
内蒙古北大山杂岩体成因及其地质意义
Petrogenesis and geological significance of the Beidashan complex rockmass, Inner Mongolia
投稿时间:2017-09-13  
DOI:
中文关键词: 北大山杂岩体  A型花岗岩  年代学  地球化学  内蒙古
英文关键词: Beidashan complex rockmass, A-type granite, geochronology, geochemistry, Inner Mongolia
基金项目:中国地质调查局国家二级项目内蒙古赤峰有色金属基地综合地质调查(编号:DD20160072)及自然科学基金(编号:4602098)联合资助。
作者单位
管育春 中国地质大学北京,北京 100083
北京矿产地质研究院,北京 100012 
杨宗锋 中国地质大学北京,北京 100083 
祝新友 北京矿产地质研究院,北京 100012 
邹滔 北京矿产地质研究院,北京 100012 
程细音 北京矿产地质研究院,北京 100012 
唐雷 中国地质大学北京,北京 100083
北京矿产地质研究院,北京 100012 
邓海辉 北京矿产地质研究院,北京 100012 
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中文摘要:
      内蒙古北大山岩体是大兴安岭南段成矿带中的一个重要杂岩体。LA-ICP-MS锆石U-Pb测年结果表明,北大山岩体中的斑状石英二长闪长岩、石英二长斑岩和二长花岗岩分别形成于(142.6±1.8)Ma、(141.1±1.9)Ma、(140.4±1.6)Ma,属早白垩世早期的产物。北大山杂岩体由早至晚,岩石地球化学特征有规律的演化,主要表现为:SiO2含量逐渐增高,碱度也增高,而钙镁和铝质渐趋降低;稀土元素中弱铕亏损演变为强铕亏损;微量元素中Rb、Nb、Ta含量升高,而Ba、Sr、P、Ti逐渐降低。主、微量元素地球化学特征总体显示该杂岩体为钙碱性—碱性、准铝质—弱过铝质A型花岗岩,其成因可能为在岩石圈伸展环境下,幔源岩浆的底侵促使上覆的先存地壳发生部分熔融形成花岗质岩浆,岩浆源区与壳幔混熔作用有关,并且该作用形成杂岩体中早期含幔源包体的石英二长闪长岩和晚期富挥发分的二长花岗岩。
英文摘要:
      The Beidashan granite, located in Chifeng area, Inner Mongolia, is an important complex rockmass in the southern of the Da Hinggan Mountains metallogenic belt. The U-Pb dating results of zircon by LA-ICP-MS method show that the porphyritic quartz monzodiorite, quartz-monzonite porphyry and monzogranite in the Beidashan complex rockmass were formed at(142.6±1.8)Ma,(141.1±1.9)Ma and(140.4±1.6)Ma respectively. The geochemical characteristics of Beidashan complex rockmass have a regular evolution from early to late stage as followings:the content of SiO2 increased gradually as well as that of alkalinity, while contents of calcium-magnesium and aluminum gradually reduced. Weak δEu depletion evolved into strong δEu depletion in the chondrite normalized REE patterns. The contents of Rb, Nb, Ta increased , but Ba, Sr, P and Ti decreased gradually. The rocks belong to calc alkaline-alkaline and quasi aluminous-weakly peraluminous A-type granites. Its genesis might be ascribed to the underplating of the mantle-derived magma which caused younger crust partial melting to form granitic magma within the lithosphere extension environment, and its magma source are related to the crust-mantle mixed re-melting. In addition, the quartz monzodiorite which contain mantle enclave in the early time and the rich volatile monzogranite in the late stage was also formed.
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