CAJ | 학술논문

对龙源坝地区南西部山间小盆地周围的花岗岩风化壳进行踏勘调查发现，区内山形地势受燕山期 NE向良伞寨断裂带和喜山期新构造的双重影响，盆地周缘多为低缓山丘，风化壳厚度大，壳层结构发育完整，是离子型稀土矿理想的赋存场所。基岩岩性主要为燕山早期粗中粒似斑状黑云母花岗岩，次为燕山晚期细粒二云母花岗岩、煌斑岩，是离子型稀土矿的成矿物质来源。研究区处于赣南粤北(稀土矿)成矿亚区，属亚热带气候，温热多雨，利于离子型稀土矿的形成。认为该区具有探寻中-小型花岗岩风化壳离子吸附型稀土矿的找矿潜力。
대룡원패지구남서부산간소분지주위적화강암풍화각진행답감조사발현，구내산형지세수연산기 NE향량산채단렬대화희산기신구조적쌍중영향，분지주연다위저완산구，풍화각후도대，각층결구발육완정，시리자형희토광이상적부존장소。기암암성주요위연산조기조중립사반상흑운모화강암，차위연산만기세립이운모화강암、황반암，시리자형희토광적성광물질래원。연구구처우공남월북(희토광)성광아구，속아열대기후，온열다우，리우리자형희토광적형성。인위해구구유탐심중-소형화강암풍화각리자흡부형희토광적조광잠력。
Through the reconnaissance survey on granite weathering-crust on the periphery of intermontane basin which locates at the southwest part of Longyuanba area,it is indicated that the orographic and geo-graphic features are under the influence of both Yanshaian NE-trending Xiangliangsanzhai faulted zone and Himalayan neotectonic movement.The periphery of the basin is characterized by rolling hills,and the weathering crust is thick with well-developed shell structure.It is the ideal occurrence place of ion type rare earth minerals.The lithology of basic rocks is early Yanshanian coarse-medium-grained porphyraceous bio-tite granite with minor late Yanshanian fine-grained binarygranite and lamprophyre,which are ore-forming material source of ion type rare earth minerals.This area is a part of South-Jiangxi North-Guangdong (rare earth mineral)metallogenic sub-region which is characterized by subtropical climate of intermediate tempera-ture and abundant precipitation and is favor of development of ion type rare earth minerals.It is believed that the area has favorable prospecting potential of medium-small scale granite weathering-crust ion-absorption type rare earth minerals.