必须声明标量变量 "@Script_ID"。 西昆仑苏纳克早古生代花岗岩锆石U-Pb年龄、地球化学特征及其地质意义-《地球科学与环境学报》
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[1]陈贵民,刘俊辰,王义天*,等.西昆仑苏纳克早古生代花岗岩锆石U-Pb年龄、地球化学特征及其地质意义[J].地球科学与环境学报,2020,42(04):427-441.[doi:10.19814/j.jese.2020.03026]
 CHEN Gui-min,LIU Jun-chen,WANG Yi-tian*,et al.Zircon U-Pb Dating and Geochemical Characteristics of Early Paleozoic Granite in the Southern Sunake of West Kunlun, Northwest China and Their Geological Significances[J].Journal of Earth Sciences and Environment,2020,42(04):427-441.[doi:10.19814/j.jese.2020.03026]
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西昆仑苏纳克早古生代花岗岩锆石U-Pb年龄、地球化学特征及其地质意义(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第42卷
期数:
2020年第04期
页码:
427-441
栏目:
基础地质与矿产地质
出版日期:
2020-07-15

文章信息/Info

Title:
Zircon U-Pb Dating and Geochemical Characteristics of Early Paleozoic Granite in the Southern Sunake of West Kunlun, Northwest China and Their Geological Significances
文章编号:
1672-6561(2020)04-0427-15
作者:
陈贵民1刘俊辰23王义天2*胡乔青2黄诗康2孙政浩3 尼加提·阿布都逊4孔德懿5刘景峰5
(1. 新疆维吾尔自治区地质矿产勘查开发局第六地质大队,新疆 哈密 839000; 2. 中国地质科学院矿产资源研究所 自然资源部成矿作用与资源评价重点实验室,北京 100037; 3. 中国地质大学(北京)地球科学与资源学院,北京 100083; 4. 新疆大学 地质与矿业工程学院,新疆 乌鲁木齐 830046; 5. 新疆维吾尔自治区地质矿产勘查开发局第十地质大队,新疆 和田 848000)
Author(s):
CHEN Gui-min1 LIU Jun-chen23 WANG Yi-tian2* HU Qiao-qing2 HUANG Shi-kang2 SUN Zheng-hao3 Nijiati ABUDUXUN4 KONG De-yi5 LIU Jing-feng5
(1. No.6 Geological Party, Xinjiang Bureau of Geology and Mineral Exploration and Development, Hami 839000, Xinjiang, China; 2. MLR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China; 3. School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China; 4. School of Geology and Mining Engineering, Xinjiang University, Urumqi 830046, Xinjiang, China; 5. No.10 Geological Party, Xinjiang Bureau of Geology and Mineral Exploration and Development, Hotan 848000, Xinjiang, China)
关键词:
花岗岩 锆石U-Pb年龄 地球化学 岩石成因 构造背景 库尔良裂谷带 西昆仑 新疆
Keywords:
granite zircon U-Pb age geochemistry petrogenesis tectonic setting Kuerliang rift zone West Kunlun Xinjiang
分类号:
P588.1; P59
DOI:
10.19814/j.jese.2020.03026
文献标志码:
A
摘要:
苏纳克花岗岩位于西昆仑造山带库尔良裂谷带内,岩体岩性为黑云母二长花岗岩,其中侵入有花岗闪长岩脉。LA-ICP-MS锆石U-Pb定年结果显示,黑云母二长花岗岩和花岗闪长岩脉的结晶年龄分别为(477.0±2.1)Ma和(466.7±2.0)Ma,为早—中奥陶世岩浆活动的产物。苏纳克黑云母二长花岗岩主量元素组成具有高硅(SiO2含量(质量分数,下同)为72.75%~76.44%)、富碱(Na2O+K2O值为8.58%~9.12%)的特征,A/CNK值为1.02~1.11,为弱过铝质、高钾钙碱性系列。球粒陨石标准化稀土元素配分模式表现为平缓的右倾型特征,并呈“V”字型,且具有显著的负Eu异常。微量元素组成明显富集Rb、K等大离子亲石元素及Th、U等高场强元素,强烈亏损Ba、Sr、Eu、P、Ti等。整体上,苏纳克黑云母二长花岗岩具有高分异I型花岗岩的地球化学特征,是西昆仑早古生代原特提斯洋俯冲过程中的产物。
Abstract:
Sunake granite, located in Kuerliang rift zone of West Kunlun orogen, is composed of biotite monzogranite, in which granodiorite dikes are intruded. The LA-ICP-MS dating yields zircon U-Pb ages of(477.0±2.1)Ma and(466.7±2.0)Ma from the biotite monzogranite and granodiorite, respectively, which are the products of tectonic magmatism during Early-Middle Ordovician. The major elements of Sunake biotite monzogranite are characterized by high silica(the contents of SiO2 are 72.75%-76.44%)and alkali(the contents of Na2O+K2O are 8.58%-9.12%)with the A/CNK of 1.02-1.11, showing that they are weakly peraluminous and high-K calc-alkaline series. The chondrite-normalized REE pattern presents a gentle right-leaning and “V” shape with significant negative Eu anomalies. The trace elements are enriched in Rb, K, Th and U, and evidently depleted in Ba, Sr, Eu, P and Ti. Overall, Sunake biotite monzogranite has the geochemical characteristics of high fractionated I-type granite, which is the product of Proto-Tethys Ocean subduction in West Kunlun during Early Paleozoic.

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备注/Memo

备注/Memo:
收稿日期:2020-03-10; 修回日期:2020-06-14; 网络首发日期:2020-07-20投稿网址:http:∥jese.chd.edu.cn/
基金项目:“十二五”国家科技支撑计划项目(2015BAB05B02)
作者简介:陈贵民(1968-),男,陕西蓝田人,高级工程师,E-mail:2549242126@qq.com。
*通讯作者:王义天(1969-),男,辽宁东港人,研究员,理学博士,E-mail:wyt69@263.net。
更新日期/Last Update: 2020-07-27