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阿拉善地块北缘雅干花岗岩体地球化学、地质年代学及其对区域构造演化制约
引用本文:郑荣国,吴泰然,张文,冯继承,徐操,孟庆鹏,张昭昱.阿拉善地块北缘雅干花岗岩体地球化学、地质年代学及其对区域构造演化制约[J].岩石学报,2013,29(8):2665-2675.
作者姓名:郑荣国  吴泰然  张文  冯继承  徐操  孟庆鹏  张昭昱
作者单位:造山带和地壳演化教育部重点实验室,北京大学地球与空间科学学院,北京100871
基金项目:本文受国家自然科学基金项目(41040017)资助.
摘    要:位于阿拉善北部中蒙边境地区的雅干花岗岩体以二长花岗岩为主,岩体的锆石离子探针U-Pb年龄为283.2±2.2Ma (n=14,MSWD=0.016).该花岗岩体具有相对较低的SiO2含量(66.96%~70.71%),和较高的A12O3(15.05%~16.05%)和(Na2O+ K2O)含量(7.24%~9.19%),且岩体钠含量稍高(Na2O/K2O>1).雅干花岗岩体总体上表现为高钾钙碱性及偏铝质-过铝质的特征.岩体稀土元素总合量为101.9×10-6~133.1 ×1O-6,在稀土元素配分模式图中,岩体表现为轻-重稀土元素中等程度-强烈分异,同时具有明显的负Eu异常(δEu =0.59 ~0.77);在微量元素原始地幔标准化蛛网图中,岩体表现为亏损Nb、Ta、P、Ti,富集Ba、Rb、Cs、Th、K等大离子亲石元素;岩体同位素特征则表现为具有高的(87 Sr/86 Sr)i值(0.707654 ~0.710235)以及负εNd(t)值.根据雅干花岗岩体的形成时代、地球化学特征以及相关的沉积建造特征,可推断该岩体形成于后碰撞环境,表明古亚洲洋在阿拉善地块北缘北部地区的分支于早二叠世(283.2 ±2.2Ma)之前已经闭合.

关 键 词:阿拉善地块北缘  锆石SIMS  U-Pb  后碰撞
收稿时间:2011/9/20 0:00:00
修稿时间:2012/10/1 0:00:00

Geochronology and geochemistry of the Yagan granite in the northern margin of the Alxa block: Constraints on the tectonic evolution of the southern Altaids.
ZHENG RongGuo,WU TaiRan,ZHANG Wen,FENG JiCheng,XU Cao,MENG QingPeng and ZHANG ZhaoYu.Geochronology and geochemistry of the Yagan granite in the northern margin of the Alxa block: Constraints on the tectonic evolution of the southern Altaids.[J].Acta Petrologica Sinica,2013,29(8):2665-2675.
Authors:ZHENG RongGuo  WU TaiRan  ZHANG Wen  FENG JiCheng  XU Cao  MENG QingPeng and ZHANG ZhaoYu
Institution:Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China;Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, School of Earth and Space Sciences, Peking University, Beijing 100871, China
Abstract:
Keywords:Northern margin of the Alxa block  Zircon SIMS U-Pb  Post-collision
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