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| 1 | 东北地区花岗岩地质图(1∶1500000)编图及其说明显示文摘在收集前人资料和最新区调及科研成果文献的基础上,梳理厘定公开发表文献的花岗岩岩体同位素年龄数据1093个,硅酸盐数据772套,微量元素数据627套,稀土元素数据653套.依据这些数据及最新调查成果编制东北地区花岗岩地质图(1∶1 500 000).该图突出了构造-花岗岩区划作用.此次研究将前中生代构造-花岗岩类划分为2个构造花岗岩域、2个构造花岗岩省和7个构造花岗岩区(带),将中新生代构造-花岗岩类划分为2个构造花岗岩域、3个构造花岗岩省和7个构造花岗岩区(带),使得花岗岩类的时空演化特征更加明显. | 陈会军 钱程 庞雪娇 赵春荆 李之彤 刘世伟 崔天日 孙巍 迟效国 葛文春 张彦龙 王利民 于宏斌 唐臣 梁科伟 | 2016 | 地质与资源2016，25，6： | 3 |
| 2 | Petrogenesis and tectonic setting of granite porphyry in Keyouzhongqi area,Inner Mongolia显示文摘The authors studied the geochemistry,zircon U-Pb ages,Hf isotope of the granite porphyry and its petrogenesis and tectonic setting in the studied area. The zircon U-Pb dating indicates the formation of the granite porphyry is in Early Cretaceous( 125. 1 ± 1. 5 Ma). The granite porphyry has high-SiO2and alkali-rich features,which belongs to high-K calc-alkaline series rocks( A / CNK = 0. 95%--1. 25%). The analyses of trace elements show the characteristics of a swallow-shaped REE distribution pattern with enrichment in LREEs and most of LILEs and HFSEs,depletion in Ba,Sr,Nb,P and Ti,and especially strong depletion in Eu,which indicates the granite porphyry belongs to the aluminous A-type granite. Their εHf( t)range from 5. 94 to 8. 80with Hf two-stage model ages( TDM2) of 620 Ma to 803 Ma. Combining with the regional tectonic background,we conclude that the source of the rocks is the new crust materials accreted from depleted mantle in Neoproterozoic and is the product of partial melting of middle and lower crustal rocks,which may be suffered from the dual impact of the subduction of the Palaeo-Pacific Ocean and the closure of the Mongol-Okhotsk Ocean. | WU Qing YANG Weihong HE Zhonghua YANG Deming MA Rui WANG Jianguo | 2014 | Global Geology2014，17，1： | 1 |
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