青海祁漫塔格地区虎头崖矿床Ⅵ矿带花岗岩的成岩时代、地球化学特征和成因

doi:10.13278/j.cnki.jjuese.201503109

吉林大学学报(地球科学版) ›› 2015, Vol. 45 ›› Issue (3): 743-758.doi: 10.13278/j.cnki.jjuese.201503109

青海祁漫塔格地区虎头崖矿床Ⅵ矿带花岗岩的成岩时代、地球化学特征和成因

姚磊^1,2, 吕志成^2,3, 于晓飞^2,3, 庞振山^2,3, 蔡煜琦⁴, 刘鹏⁵, 刘长城⁶, 王凤兰⁷

1. 中国地质大学(北京)地球科学与资源学院, 北京 100083;
2. 国土资源部矿产勘查技术指导中心, 北京 100034;
3. 中国地质调查局发展研究中心, 北京 100037;
4. 核工业北京地质研究院, 北京 100029;
5. 成都理工大学地球科学学院, 成都 610059;
6. 云南铜业矿产资源勘查开发有限公司, 昆明 650001;
7. 河北省地矿局第五地质大队, 河北唐山 063000

收稿日期:2014-10-14 发布日期:2015-05-26
通讯作者: 吕志成(1966),男,研究员,博士,主要从事矿床学及地球化学方面的研究工作,E-mail:zhichenglv@163.com。 E-mail:zhichenglv@163.com
作者简介:姚磊(1986),男,博士研究生,主要从事矿床学及矿床地球化学研究,E-mail:lemmon20054255@aliyun.com
基金资助:
国土资源公益性行业科研专项项目(201411024);中国地质调查局老矿山找矿技术创新与示范项目(1212011220737);中国地质调查局地质调查项目(12120113090000)

Petrogenesis, Geochemistry and Zircon U-Pb Age of the Granite from No.Ⅵ Section of Hutouya Deposit, Qimantag Area, Qinghai Province, and Its Geological Significance

Yao Lei^1,2, Lü Zhicheng^2,3, Yu Xiaofei^2,3, Pang Zhenshan^2,3, Cai Yuqi⁴, Liu Peng⁵, Liu Changcheng⁶, Wang Fenglan⁷

1. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;
2. Mineral Exploration Technical Guidance Center, Ministry of Land and Resources, Beijing 100034, China;
3. Development and Research Centre, China Geological Survey, Beijing 100037, China;
4. Beijing Research Institute of Uranium Geology, Beijing 100029, China;
5. College of Earth Sciences, Chengdu University of Technology, Chengdu 610059, China;
6. Yunnan Company (Ltd) of Exploration & Development of Cu Mineral Resources, Kunming 650001, China;
7. The Fifth Geology Company of Hebei Geology and Minerals Bureau, Tangshan 063000, Hebei, China

Received:2014-10-14 Published:2015-05-26

摘要/Abstract

摘要：

利用LA-ICP-MS锆石U-Pb法,测得与成矿有关的青海祁漫塔格地区虎头崖矿床Ⅵ矿带花岗岩的成岩年龄为(233.6±1.8) Ma(MSWD=1.2,n=17)。地球化学特征显示:花岗岩属高钾钙碱性、弱过铝质花岗岩;样品的稀土元素组成以总体右倾,轻、重稀土分异明显和具明显的负铕异常为特征;微量元素具有富集Rb、Th、U、La、Nd等大离子亲石元素,亏损Ba、Sr、Nb、P、Ti等元素的特点。Sr-Nd同位素组成特征显示,花岗岩的源区可能是富集岩石圈地幔。初步研究认为,虎头崖矿床Ⅵ矿带花岗岩可能形成于中、晚三叠世碰撞后碰撞的构造背景下。

关键词: 花岗岩, 锆石U-Pb年龄, Sr-Nd同位素, 虎头崖矿床, 祁漫塔格, 青海

Abstract:

Zircon LA-ICP-MS dating of the granite from the No.Ⅵ section of Hutouya deposit yields an emplacement age of (233.6±1.8) Ma (MSWD=1.2, n=17). The geochemical analysis indicates that the granite belongs to the weakly peraluminous granitic rocks, showing the nature of high-K calc-alkalic series. The rock has high REE content, and the chondrite-normalized REE distribution patterns show the characteristics of LREE enrichment, obvious LREE and HREE fractionation, and significant negative Eu anomaly. The trace element composition of the granite is enriched in Rb, Th, U, La, Nd and poor in Ba, Sr, Nb, P, Ti. The Sr-Nd isotope composition and geochemical characteristics indicate that the magma source of the granite mainly derived from enriched lithospheric mantle. The data of this study indicate that the granite from the No.Ⅵ section of Hutouya deposit formed under a collision, and post-collision setting.

Key words: granite, zircon U-Pb dating, Sr-Nd isotope composition, Hutouya deposit, Qimantag, Qinghai

中图分类号:

姚磊, 吕志成, 于晓飞, 庞振山, 蔡煜琦, 刘鹏, 刘长城, 王凤兰. 青海祁漫塔格地区虎头崖矿床Ⅵ矿带花岗岩的成岩时代、地球化学特征和成因[J]. 吉林大学学报(地球科学版), 2015, 45(3): 743-758.

Yao Lei, Lü Zhicheng, Yu Xiaofei, Pang Zhenshan, Cai Yuqi, Liu Peng, Liu Changcheng, Wang Fenglan. Petrogenesis, Geochemistry and Zircon U-Pb Age of the Granite from No.Ⅵ Section of Hutouya Deposit, Qimantag Area, Qinghai Province, and Its Geological Significance[J]. Journal of Jilin University(Earth Science Edition), 2015, 45(3): 743-758.

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青海祁漫塔格地区虎头崖矿床Ⅵ矿带花岗岩的成岩时代、地球化学特征和成因

Petrogenesis, Geochemistry and Zircon U-Pb Age of the Granite from No.Ⅵ Section of Hutouya Deposit, Qimantag Area, Qinghai Province, and Its Geological Significance

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