|本期目录/Table of Contents|

[1]张博,荆德龙,汪帮耀,等.西天山备战铁矿石炭纪火山岩地球化学特征及岩石成因[J].地球科学与环境学报,2015,37(06):82-100.
 ZHANG Bo,JING De-long,WANG Bang-yao,et al.Geochemical Characteristics and Petrogenesis of Carboniferous Volcanic Rocks from Beizhan Iron Deposit of West Tianshan[J].Journal of Earth Sciences and Environment,2015,37(06):82-100.
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西天山备战铁矿石炭纪火山岩地球化学特征及岩石成因(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第37卷
期数:
2015年第06期
页码:
82-100
栏目:
基础地质与矿产地质
出版日期:
2015-11-15

文章信息/Info

Title:
Geochemical Characteristics and Petrogenesis of Carboniferous Volcanic Rocks from Beizhan Iron Deposit of West Tianshan
文章编号:
1672-6561(2015)06-0082-19
作者:
张博荆德龙汪帮耀姜常义赵振刚
1. 长安大学 地球科学与资源学院,陕西 西安 710054; 2. 长安大学 西部矿产资源与地质工程教育部重点实验室,陕西 西安 710054; 3. 新疆地质矿产勘查开发局第十一地质大队,新疆 昌吉 831100
Author(s):
ZHANG Bo JING De-long WANG Bang-yao JIANG Chang-yi ZHAO Zhen-gang
1. School of Earth Science and Resources, Chang’an University, Xi’an 710054, Shaanxi, China; 2. Key Laboratory of Western Mineral Resources and Geological Engineering of Ministry of Education, Chang’an University, Xi’an 710054, Shaanxi, China; 3. No.11 Geological Party, Xinjiang Bureau of Geology and Mineral Resources, Changji 831100, Xinjiang, China
关键词:
地球化学岩石成因石炭纪火山岩大陆弧西天山新疆
Keywords:
geochemistry petrogenesis Carboniferous volcanic rock continental arc West Tianshan Xinjiang
分类号:
P588.14;P595
DOI:
-
文献标志码:
A
摘要:
选取西天山阿吾拉勒东段备战铁矿区出露的石炭纪火山岩为研究对象。通过对岩相学与主量、微量元素地球化学等方面的研究来约束其构造环境与岩浆源区性质。分析测试显示该地区火山岩多属中高钾钙碱性及橄榄玄粗岩系列,富集轻稀土元素及大离子亲石元素(Rb、Th、K等),亏损高场强元素(Nb、Ta、Ti等)。岩石组合及地球化学特征表明:该地区火山岩形成于活动大陆弧环境,其形成与早石炭世末期北天山洋盆向位于其南部的伊犁地块之下发生B型俯冲作用有关。另外,火山岩εNd(t)值介于0.73~4.33之间,显示岩浆源区具亏损地幔的属性,且母岩浆在演化过程中还经历有结晶分异作用以及陆壳物质混染作用。
Abstract:
Carboniferous volcanic rocks are exposed in Beizhan iron deposit of the eastern Awulale, West Tianshan. The petrology and geochemistry characteristics of major and trace elements of Carboniferous volcanic rocks were studied to discuss the tectonic settings and petrogenesis of magmatic source. The results show that most of volcanic rocks belong to middle high-K calc-alkaline and shoshonite series; the characteristics include rich in LREE and LILE (Rb, Th and K, etc.), and depleted in HFSE (Nb, Ta and Ti, etc.). Rock association and geochemistry show that volcanic rocks form in active continental arc settings, which have a close correlation with the B-type subduction of North Tianshan oceanic basin towards the south beneath Yili plate during the Late Early Carboniferous. εNd(t) of volcanic rock is 0.73-4.33, suggesting that the origin magma comes from the depleted mantle. The parent magma has also experienced fractional crystallization and crustal contamination in the process of evolution.

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备注/Memo

备注/Memo:
收稿日期:2014-12-29
基金项目:中国地质调查局地质大调查项目(12120114007501,12120113044000)
作者简介:张博(1991-),男,安徽宿州人,理学硕士研究生,E-mail:168239693@qq.com。
通讯作者:姜常义(1951-),男,黑龙江富裕人,教授,博士研究生导师,E-mail:jiangchangyi001@163.com。
更新日期/Last Update: 2015-11-27