| Three Alkali—Rich Intrusive Rock Belts Bewly Discovered in the Mt.Kunlkun—Mt.Altun Region,Xinjiang,China |
| |
| 引用本文： | 朱笑青 王元龙 等. Three Alkali—Rich Intrusive Rock Belts Bewly Discovered in the Mt.Kunlkun—Mt.Altun Region,Xinjiang,China[J]. 中国地球化学学报, 2002, 21(3): 244-251. DOI: 10.1007/BF02831089 |
| |
| 作者姓名： | 朱笑青 王元龙 等 |
| |
| 作者单位： | [1]OpenLab.ofOreDepositGeochemistry,InstituteofGeochemistry,ChieseAcademyofScinences,Guiyang550002,China [2]InstituteofGeophysicsandGeology,ChineseAcademyofSciences,Beijing100029,China |
| |
| 摘 要： | The newly discovered three alkali-rich intrusive rock belts in the Mt.Kunlun Mt.Altun region of southern Xinjiang are the Lapeiquan-Yitunbulak alkali-rich intrusive fock belt, the Gez-Taxkorgan alkali-rich intrusive rock belt and the Beeilisai-Abulash alkali-rich intrusive rock belt.The former two belts were formed during the Yanshanian period,and the third one was formed during the Himalayan period,which is the youngest alkali-rich intrusive rock belt in China.The discovery of the alkali-rich intrusive rock belts is of great significance in shedding light on the history of tectono-magmatic activities in this region.
|
| 关 键 词： | 昆仑山 碱性花岗岩 碱性岩 新疆 中国 |
Three alkali-rich intrusive rock belts newly discovered in the Mt. Kunlun-Mt. Altun region, Xinjiang, China |
| |
| Zhu Xiaoqing,Wang Yuanlong,Bi Hua,Wang Zhonggang. Three alkali-rich intrusive rock belts newly discovered in the Mt. Kunlun-Mt. Altun region, Xinjiang, China[J]. Chinese Journal of Geochemistry, 2002, 21(3): 244-251. DOI: 10.1007/BF02831089 |
| |
| Authors: | Zhu Xiaoqing Wang Yuanlong Bi Hua Wang Zhonggang |
| |
| Affiliation: | (1) Open Lab. of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, 550002 Guiyang, China;(2) Institute of Geophysics and Geology, Chinese Academy of Sciences, 100029 Beijing, China;(3) Hainan Normal University, 571158 Haikou, China |
| |
| Abstract: | The newly discovered three alkali-rich intrusive rock belts in the Mt. Kunlun Mt. Altun region of southern Xinjiang are the Lapeiquan-Yitunbulak alkali-rich intrusive rock belt, the Gez-Taxkorgan alkali-rich intrusive rock belt and the Beilisai-Abulash alkali-rich intrusive rock belt. The former two belts were formed during the Yanshanian period, and the third one was formed during the Himalayan period, which is the youngest alkali-rich intrusive rock belt in China. The discovery of the alkali-rich intrusive rock belts is of great significance in shedding light on the history of tectono-magmatic activities in this region. Granted jointly by the State 305 Research Program and the National Natural Science Foundation of China (Grant No. 493333030). |
| |
| Keywords: | Kunlun Mountains Altun Mountains alkali granite alkaline rock alkali-rich intrusive rock belt |
| 本文献已被 维普 SpringerLink 等数据库收录！ |
|
