|本期目录/Table of Contents|

[1]杨 阳,柯昌辉*,王晓霞,等.北秦岭蟒岭花岗岩体岩浆演化及源区:来自矿物学和Sr-Nd-Hf同位素证据[J].地球科学与环境学报,2022,44(04):658-674.[doi:10.19814/j.jese.2022.02033]
 YANG Yang,KE Chang-hui*,WANG Xiao-xia,et al.Magmatic Evolution and Origin of Mangling Granitic Pluton in North Qinling, China: Evidence from Mineralogy and Sr-Nd-Hf Isotopes[J].Journal of Earth Sciences and Environment,2022,44(04):658-674.[doi:10.19814/j.jese.2022.02033]
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北秦岭蟒岭花岗岩体岩浆演化及源区:来自矿物学和Sr-Nd-Hf同位素证据(PDF)
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第44卷
期数:
2022年第04期
页码:
658-674
栏目:
基础地质与矿产地质
出版日期:
2022-07-15

文章信息/Info

Title:
Magmatic Evolution and Origin of Mangling Granitic Pluton in North Qinling, China: Evidence from Mineralogy and Sr-Nd-Hf Isotopes
文章编号:
1672-6561(2022)04-0658-17
作者:
杨 阳1柯昌辉2*王晓霞2李金宝1吕星球3聂政融4
(1. 长安大学 地球科学与资源学院,陕西 西安 710054; 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. 湖南省有色地质勘查局二一四队,湖南 株洲 412007; 4. 河南新路桥集团高速公路管理有限公司,河南 郑州 450018)
Author(s):
YANG Yang1 KE Chang-hui2* WANG Xiao-xia2 LI Jin-bao1 LYU Xing-qiu3 NIE Zheng-rong4
(1. School of Earth Science and Resources, Chang'an University, Xi'an 710054, Shaanxi, China; 2. MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China; 3. No.214 Geological Party, Hunan Geological & Mining Organization for Non-ferrous Metals, Zhuzhou 412007, Hunan, China; 4. Henan New Road & Bridge Group Motorway Management Co., Ltd., Zhengzhou 450018, Henan, China)
关键词:
花岗岩 矿物学 黑云母 Sr-Nd-Hf同位素 岩浆演化 源区 北秦岭
Keywords:
granite mineralogy biotite Sr-Nd-Hf isotopes magmatic evolution origin North Qinling
分类号:
P597; P57
DOI:
10.19814/j.jese.2022.02033
文献标志码:
A
摘要:
蟒岭花岗岩体位于北秦岭构造带黑沟—栾川断裂和乔端—瓦穴子断裂之间,是由3期岩浆侵入形成的岩浆杂岩体,其岩石类型从早到晚依次为含辉石黑云母闪长岩、二长花岗岩和黑云母正长花岗岩。在详细的野外调查和岩相学观察基础上,对蟒岭花岗岩体中的前两期岩石进行了系统的矿物学和Sr-Nd-Hf同位素研究。结果表明:蟒岭花岗岩体以I型花岗岩为主,从早到晚(含辉石黑云母闪长岩→二长花岗岩→黑云母正长花岗岩),其岩石成因类型具有从I型向I-A过渡型花岗岩变化的趋势; 含辉石黑云母闪长岩和二长花岗岩中黑云母形成于较高氧逸度环境,其结晶温度分别为675 ℃~740 ℃和550 ℃~675 ℃; 蟒岭花岗岩体是古老地壳物质部分熔融形成的长英质岩浆与可能起源于幔源的基性岩浆混合而成的产物。
Abstract:
Mangling granitic pluton is located between Heigou-Luanchuan fault and Qiaoduan-Waxuezi fault in North Qinling. It is a magmatic complex formed by 3 stages of magmatic intrusion, including pyroxene-bearing biotite diorites, monzogranites and biotite syenogranite from early stage to late stage. Based on detailed field survey and petrographic observation, the mineralogy and Sr-Nd-Hf isotopes of the first two rocks in Mangling granitic pluton were systematically studied. The results show that Mangling granite pluton is mainly I type granite; from early stage to late stage(pyroxene-bearing biotite diorites→monzogranites→biotite syenogranites), the petrogenetic type of granite has a tendency of changing from I type to I-A transitional type; the biotites from the first two rocks are formed in high oxygen fugacity, and their crystallization temperatures are 675 ℃-740 ℃ and 550 ℃-675 ℃, respectively; Mangling granite pluton is a mixture of felsic magma formed by partial melting of ancient crust and mafic magma possibly derived from mantle.

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备注/Memo

备注/Memo:
收稿日期:2022-02-19; 修回日期:2022-04-19投稿网址:http:∥jese.chd.edu.cn/
基金项目:中国地质调查局地质调查项目(1212010012012); 国家自然科学基金项目(41972094,42172065)
作者简介:杨 阳(1988-),女,陕西黄陵人,编辑,理学博士,E-mail:yangm0926@163.com。
*通讯作者:柯昌辉(1987-),男,湖北十堰人,副研究员,理学博士,E-mail:kechanghuicags@126.com。
更新日期/Last Update: 2022-07-30