[1]柯宏飙,王金泉,丁 勇,等.皖南歙县新溪口岩体锆石U-Pb定年、地球化学特征及找矿前景[J].华东地质,2020,41(02):116-127.[doi:10.16788/j.hddz.32-1865/P.2020.02.003]
 KE Hong-biao,WANG Jin-quan,DING Yong,et al.Zircon U-Pb geochronology and geochemistry of the Xinxikou pluton in Shexian County,Southern Anhui Province and its prospecting significance[J].East China Geology,2020,41(02):116-127.[doi:10.16788/j.hddz.32-1865/P.2020.02.003]
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皖南歙县新溪口岩体锆石U-Pb定年、地球化学特征及找矿前景()
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《华东地质》[ISSN:2096-1871/CN:32-1865/P]

卷:
41
期数:
2020年02期
页码:
116-127
栏目:
基础地质
出版日期:
2020-06-20

文章信息/Info

Title:
Zircon U-Pb geochronology and geochemistry of the Xinxikou pluton in Shexian County,Southern Anhui Province and its prospecting significance
文章编号:
2096-1871(2020)02-116-12
作者:
柯宏飙王金泉丁 勇陈 明
(安徽省地质矿产勘查局332地质队,黄山 245000)
Author(s):
KE Hong-biaoWANG Jin-quanDING YongCHEN Ming
(No.332 Geological Team, Bureau of Geology and Mineral Exploration of Anhui Province,Huangshan 245000,China)
关键词:
A型花岗岩 锆石U-Pb定年 燕山晚期 锡石重砂异常 皖南
Keywords:
A-type granite zircon U-Pb dating late Yanshanian heavy mineral anomaly of cassiterite southern Anhui Province
分类号:
P588.121
DOI:
10.16788/j.hddz.32-1865/P.2020.02.003
文献标志码:
A
摘要:
皖南歙县新溪口岩体为中细粒少斑花岗岩,侵位时间为121.31±0.67 Ma; 岩石具有高硅、富钾特征。SiO2含量为75.97%~76.49%,K2O含量为4.84%~5.28%,K2O/Na2O为1.61~2.05,A/CNK为1.05~1.06、A/NK为1.16~1.19,属弱过铝质花岗岩。稀土元素总量为(261.90~329.83)×10-6,具有海鸥型右倾配分模式,(La/Yb)N为3.26~5.15,具有强烈的Eu负异常(δEu=0.018~0.063)。大离子亲石元素Rb富集,Ba、Sr亏损,高场强元素Th、U富集,Nb、Ti具有明显的负异常。岩体形成于燕山晚期早阶段古太平洋板块俯冲后拉张伸展构造环境,是岩石圈减薄引发软流圈地幔上涌,上覆地壳受热部分熔融并发生结晶分离作用形成的A2型花岗岩。岩体出露点较多,剥蚀较浅,富含W、Sn、Bi等金属元素,这些元素通过云英岩化等高温气液蚀变扩散至围岩中,指示良好的找矿前景。
Abstract:
The Xinxikou pluton is mainly consists of medium-to fine-grained granite, was emplaced at 121.31± 0.67 Ma. The granites have high SiO2(75.97%~76.49%)and K2O(4.84%~5.28%)contents with K2O/Na2O ratios from 1.61 to 2.05, and show weakly peraluminous nature with A/CNK values from 1.05 to 1.06. The granites have high total REE contents ranging from 261.90 to 329.83 ppm. On the chondrite-normalized patterns, they all show markedly LREE-enriched patterns with(La/Yb)N ranging from 3.26 to 5.15 and significant troughs of Eu anomalies(δEu=0.018~0.063). Normalized to primitive mantle, the granites are enriched in large ion lithophile elements(e.g. Rb)and high field strength elements(e.g. Th and U)but depleted in Ba and Sr showing affinity to A2 granites. Together with the regional geology, the granites formed in a extensional environment, related to asthenospheric mantle upwelling triggered by roll-back of the Paleo-Pacific oceanic slab. The Xinxikou pluton is widely exposed and have a shallow denudation. These granites are rich in metallic elements(W, Sn, Bi and etc)which diffused into surrounding rocks by high temperature gas-liquid alteration such as greisenization, indicating a good prospect of ore exploration.

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备注/Memo

备注/Memo:
*收稿日期:2019-11-17 修订日期:2020-03-02 责任编辑:叶海敏
基金项目:中国地质调查局南京地质调查中心“钦杭成矿带德兴-歙县地区地质矿产调查(编号:DD20160038)”子项目“安徽1:5万街口幅区域地质矿产调查”项目资助。
第一作者简介:柯宏飙,1969年生,男,高级工程师,主要从事矿产地质勘查和区域地质调查工作。
更新日期/Last Update: 2020-06-23