[1]杨东光,聂逢君,夏 菲.2022.钱家店凹陷辉绿岩的时代、成因及对砂岩型铀成矿的制约.大地构造与成矿学,46(2):334-355.doi:10.16539/j.ddgzyckx.2022.02.010
　YANG Dongguang,NIE Fengjun,XIA Fei.2022.Age and Petrogenesis of Early Cenozoic Dolerites in the Qianjiadian Sag, Southwest Songliao Basin, NE China: Implications for the Genesis of Sandstone-hosted Uranium Deposits.Geotectonica et Metallogenia,46(2):334-355.doi:10.16539/j.ddgzyckx.2022.02.010
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钱家店凹陷辉绿岩的时代、成因及对砂岩型铀成矿的制约
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《大地构造与成矿学》[ISSN:ISSN 1001-1552/CN:CN 44-1595/P]

卷:
期数:
2022年46卷02期
页码:
334-355
栏目:
岩石大地构造与地球化学
出版日期:
2022-04-25

文章信息/Info

Title:
Age and Petrogenesis of Early Cenozoic Dolerites in the Qianjiadian Sag, Southwest Songliao Basin, NE China: Implications for the Genesis of Sandstone-hosted Uranium Deposits
文章编号:
1001-1552(2022)02-0334-022
作者:
杨东光1;  聂逢君1、2*;  夏 菲1、2;  巫建华1、2;  严兆彬1、2;  陈梦雅2;  刘晓博2;  王海涛3;  王常东3
1. 东华理工大学 核资源与环境国家重点实验室, 江西 南昌 330013; 2. 东华理工大学 地球科学学院, 江西 南昌 330013; 3. 核工业243地质大队, 内蒙古 赤峰 024006
Author(s):
YANG Dongguang1;  NIE Fengjun1、2*;  XIA Fei1、2;  WU Jianhua1、2;  YAN Zhaobin1、2;  CHEN Mengya2;  LIU Xiaobo2;  WANG Haitao3;  WANG Changdong3
1. State Key Laboratory of Nuclear Resources and Environment, East China University of Technology, Nanchang 330013, Jiangxi, China; 2. College of Earth Science, East China University of Technology, Nanchang 330013, Jiangxi, China; 3. NO.243 Geological Party, CNNC, Chifeng 024006, Inner Mongolia, China
关键词:
钱家店铀矿床;  松辽盆地;  辉绿岩;  年代学;  构造反转;  铀矿化
Keywords:
Qianjiadian uranium deposit;  Songliao Basin;  diabase;  geochronology;  tectonic inversion;  uranium mineralization
分类号:
P597; P595; P612
DOI:
10.16539/j.ddgzyckx.2022.02.010
文献标志码:
A
摘要:
松辽盆地西南缘近年来铀找矿获得重要突破, 预示着盆地蕴藏丰富的铀资源。而铀的成矿机理有待查明, 尤其是矿床中广泛发育的辉绿岩, 是否对成矿有改造作用, 辉绿岩、反转构造及铀元素聚集之间的关系目前尚不十分清楚, 制约了进一步找矿的思路。本文以钱家店凹陷钻孔辉绿岩为研究对象, 通过对斜锆石和锆石U-Pb年代学、全岩岩石地球化学的研究, 探讨辉绿岩对区域反转构造的制约, 并结合铀矿物EPMA定年研究, 探讨构造反转作用对U的聚集行为的影响。辉绿岩具有低SiO2(44.90%~51.20%), 高Fe2O3T(9.10%~15.50%)含量, MgO含量变化大(1.89%~12.58%), 可以分为碱性系列和拉斑系列两组。稀土元素和微量元素显示OIB特征, 结合岩石具有高Nb/U值(33.0~51.4), 表明它们均为软流圈成因。辉绿岩斜锆石、锆石U-Pb定年及前人Ar-Ar定年表明, 碱性系列岩石形成于51~47 Ma, 早于拉斑系列岩石(42~40 Ma)。碱性系列岩石具有较高的HREE含量和Ta/Yb、Sr/Yb值, 表明其与拉斑系列为不同深度部分熔融的结果, 暗示始新世期间岩石圈发生减薄。铀矿物EPMA化学定年结合前人矿石全岩U-Pb等时线年龄结果表明, 钱家店砂岩型铀矿成矿时代集中在67~53 Ma、43~37 Ma和17~0.7 Ma。结合前人低温热年代学研究, 表明盆地内铀成矿作用具有多期、多阶段特点。以往多强调正反转构造背景下的表生流体成矿作用, 如嫩江末期及中新世以来的构造抬升形成构造斜坡, 造成表生含铀含氧流体渗入氧化作用成矿。钱家店凹陷辉绿岩、断裂与铀矿床密切的空间关系, 以及热流体与目的层砂岩相互作用所形成的热液蚀变矿物与铀矿物共生的特点, 指示始新世存在负反转背景下热液改造型铀成矿作用。
Abstract:
The breakthrough of sandstone-type uranium deposit exploration in the last few years demonstrated that the southern Songliao basin may host abundant uranium resources. However, the genetic mechanism of ore deposit, especially (1) the possible impacts of the widely distributed dolerite on the orebodies, and (2) the relationship among the dolerite, tectonic inversion and accumulation of uranium remains poorly constrained, which influences the prospecting efficacy. In this study, baddeleyite and zircon U-Pb dating, geochronology of uranium minerals (the EMPA chemical dating method), whole-rock geochemistry, and mineral chemical compositions were conducted for the dolerites from the Qianjiadian area. The dolerites display low SiO2 of 44.90% to 51.20%, high Fe2O3T contents of 9.10% to 15.50%, and variable MgO contents (1.89% to 12.58%), and can be subdivided into alkali and tholeiitic dolerites. They are characterized by OIB type rare earth and trace element signatures with Nb/U ratios varying from 33.0 to 51.4, suggesting a common asthenospheric origin that underwent subduction-related enrichment prior to melting. Baddeleyite and zircon U-Pb and previous Ar-Ar dating results show that the alkali dolerites formed earlier (51 - 47 Ma) than the tholeiitic dolerites (42 - 40 Ma). Compared to the tholeiitic dolerites, the alkali dolerites have higher HREE contents and Ta/Yb and Sr/Yb ratios, which may reflect different depth of partial melting. Besides, EMPA chemical dating results and available U-Pb ages of the whole rocks suggest three stages of uranium mineralization, i.e., 67 - 53 Ma, 43 - 37 Ma, and 17 - 0.7 Ma, respectively. Combined with previous research, the uranium mineralization of the basin shows the characteristics of multi-period and multi-phase. Previously, more attention had been paid to the mineralization of supergene fluid under the positive reverse tectonics, such as the tectonic slope formed by tectonic uplift since the end of the Nenjiang period and Miocene, respectively, which resulted in the infiltration and oxidation of supergene uranium-bearing and oxygen-rich fluid. The intimate spatial relationship between the dolerites and uranium ore deposits, and the symbiotic relationship between minerals hydrothermal origin and uranium minerals, reveal the existence of hydrothermal modification type uranium mineralization under negative inversion structure system during Eocene.

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备注/Memo

备注/Memo:
收稿日期: 2020-11-04; 改回日期: 2021-05-08
项目资助: 国家自然科学基金项目(U2067202、41772068、41562006、41862010)和国家重点基础研究发展规划项目(2015CB453002)联合资助。
第一作者简介: 杨东光(1988-), 男, 讲师, 从事岩石地球化学方向研究。E-mail: yangdg@ecit.edu.cn
通信作者: 聂逢君(1962-), 男, 教授, 从事铀矿地质与沉积地质学方向研究。E-mail: niefj@ecit.edu.cn
更新日期/Last Update: 2022-04-10