首页|粤东北和平地区1∶5万区域地质调查主要成果与进展

粤东北和平地区1∶5万区域地质调查主要成果与进展

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在粤东北地区完成的"广东和平地区1∶5万区域地质调查"项目,以国际年代地层表(2021)为指南,重新厘定了研究区的地层序列,建立了多重地层划分与对比系统.将贝岭镇一带的混合岩解体为变质地层和变形变质花岗岩.根据岩性特征、野外接触关系及同位素年龄将区内侵入岩划分为59个侵入体,15个填图单位,获得了一批高精度锆石U-Pb测年数据,确定了侵入岩成岩时代及活动期次,并结合岩石地球化学特征探讨了岩石成因及大地构造背景.采用三重填图法,查明了火山岩岩性、岩相、火山机构分布特征,划分了火山活动旋回,系统总结了各喷发期火山岩的岩石学、年代学和地球化学特征,并初步探讨了火山岩的成因.在枫树坝一带新发现一套早志留世火山岩,并获得440.5±6.0 Ma的锆石206Pb/238U加权平均年龄,将这套火山岩置于茶园山组.建立了区域构造格架,阐明了构造形成演化历史,划分了构造变形阶段,查明了河源断裂带在区内的表现特征.新发现矿(化)点多处,特别是在区内晚白垩世沉积盆地中首次发现火山黏土型锂矿,为后续矿产勘查工作提供了重要的指导作用.
New Progresses in 150 000 Regional Geological Survey in the Heping Area,Northeastern Guangdong Province
Based on the International Chronostratigraphic Chart(2021),the project called"1∶50 000 regional geological survey of Heping area in northeast Guangdong province"project is completed.The project revised the sequence stratigraphy of the study area;and developed the multi-stratigraphic comparison and correlation system.The migmatite zone defined by previous geologists around the Beiling Town is now divided into metamorphic sedimentary rocks and metamorphic granites.The igneous rocks are been divided into 59 intrusive bodies or 15 mapping units according to lithological feature,field contacting relation and isotope age.A large amount of precise U-Pb zircon dating data were obtained to conclude the ages and history of the igneous rocks.The geochemical features of igneous rocks were considered to build the regional structural frame and explain the structural evolution history of the area.The triple mapping method was applied to determine the facies of volcanic rocks,the distribution of the volcanic edifices,and the different cycles of volcanic activities across the area.This project systematically concluded the lithology,geochemical characteristics and the formation mechanism of the volcanic rocks.A new volcanic formation,named as Chayuanshan Formation,has been discovered near the Fengshuba area,and the zircon age of 440.5±6.0 Ma suggested that this volcanic rocks was formed in Early Silurian.We also identified the different deformation stages in the geological history,and examined the characteristics of Heyuan Fault Zone in the study area.We reported multiple newly discovered mineral occurrences and mineralized occurrences.Last but not least,volcanic clay-type lithium deposit in a late Cretaceous sedimentary basin in the study area is reported,which will contribute to mineral exploration in the future.

stratigraphic division and correlationthe Chayuanshan FormationHeyuan Fault Zonevolcanic clay-type lithium depositregional geologic surveyNortheastern Guangdong Province

邵小阳、邓飞、黄继春、江云川、梁豪、张忠进

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广东省佛山地质局,佛山 528000

同济大学土木工程学院,上海 200092

地层划分对比 茶园山组 河源断裂带 火山黏土型锂矿 区域地质调查 粤东北

2024

华南地质
武汉地质矿产研究所

华南地质

影响因子:0.516
ISSN:1007-3701
年,卷(期):2024.40(4)