CAJ | 학술논문

　　姜梨园矿区属于丰-沛隆起位于单县-丰县-沛县一带，总体为东西走向的隆起构造。矿区内由南向北地层渐新，矿体南侧，依次为寒武系、奥陶系三山子组和贾汪组、闪长斑岩岩体；矿体部分为奥陶系肖县组。矿体北侧为石炭系和二叠系。主要为奥陶系灰岩富水，本文主要就矿床开采后水文地质条件变化做简要阐述。
　　강리완광구속우봉-패륭기위우단현-봉현-패현일대，총체위동서주향적륭기구조。광구내유남향북지층점신，광체남측，의차위한무계、오도계삼산자조화가왕조、섬장반암암체；광체부분위오도계초현조。광체북측위석탄계화이첩계。주요위오도계회암부수，본문주요취광상개채후수문지질조건변화주간요천술。
Jiangliyuan mine belongs to Feng and Pei uplift and is located in the Shanxian County. Overall ore is the uplift structure of east-west. In the mine the stratum is new gradually from the south to the north.South of the ore body, followed by the Cambrian, the Ordovician Sanshanzi group and diorite porphyry rock; Ore part is Ordovician Xiao County group in proper sequence. The north of the mine is the carboniferous and permian. Mainly for the Ordovician limestone After mining hydrogeological conditions change are expounded briefly.