黑龙江科技学院学报
黑龍江科技學院學報
흑룡강과기학원학보
JOURNAL OF HEILONGJIANG INSTITUTE OF SCIENCE & TECHNOLOGY
2012年
2期
148-153,167
,共7页
周莉%于亨达%杨海涛%韩朝龙
週莉%于亨達%楊海濤%韓朝龍
주리%우형체%양해도%한조룡
深部软岩%扫描电镜-X射线能谱%矿物成分%微观结构
深部軟巖%掃描電鏡-X射線能譜%礦物成分%微觀結構
심부연암%소묘전경-X사선능보%광물성분%미관결구
deep soft rock%SEM - EDS%mineral ingredient%microstructure
为了探讨鹤岗兴安矿深部软岩水理特性和塑性变形原因,分别在埋深500和740 m的不同岩性特征处,选取5个试样,采用扫描电镜-X射线能谱仪,对该矿深部软岩矿物成分与微观结构进行实验分析。结果表明:兴安矿深部软岩中主要矿物成分为石英、长石、方解石及黏土矿物,各别试样中含有菱铁矿和金红石。黏土矿物的主要成分为伊/蒙(I/S)混层、伊利石、高岭石、绿泥石等。I/S混层中蒙脱石的类型有钠蒙脱石和钙蒙脱石。碎屑矿物中有石英加大、方解石溶蚀、长石淋滤、菱铁矿解理发育等现象。黏土矿物I/S混层主要呈片架结构、蜂窝结构和絮状结构,高岭石呈书本状结构,伊利石与绿泥石呈片架结构。
為瞭探討鶴崗興安礦深部軟巖水理特性和塑性變形原因,分彆在埋深500和740 m的不同巖性特徵處,選取5箇試樣,採用掃描電鏡-X射線能譜儀,對該礦深部軟巖礦物成分與微觀結構進行實驗分析。結果錶明:興安礦深部軟巖中主要礦物成分為石英、長石、方解石及黏土礦物,各彆試樣中含有蔆鐵礦和金紅石。黏土礦物的主要成分為伊/矇(I/S)混層、伊利石、高嶺石、綠泥石等。I/S混層中矇脫石的類型有鈉矇脫石和鈣矇脫石。碎屑礦物中有石英加大、方解石溶蝕、長石淋濾、蔆鐵礦解理髮育等現象。黏土礦物I/S混層主要呈片架結構、蜂窩結構和絮狀結構,高嶺石呈書本狀結構,伊利石與綠泥石呈片架結構。
위료탐토학강흥안광심부연암수리특성화소성변형원인,분별재매심500화740 m적불동암성특정처,선취5개시양,채용소묘전경-X사선능보의,대해광심부연암광물성분여미관결구진행실험분석。결과표명:흥안광심부연암중주요광물성분위석영、장석、방해석급점토광물,각별시양중함유릉철광화금홍석。점토광물적주요성분위이/몽(I/S)혼층、이리석、고령석、록니석등。I/S혼층중몽탈석적류형유납몽탈석화개몽탈석。쇄설광물중유석영가대、방해석용식、장석림려、릉철광해리발육등현상。점토광물I/S혼층주요정편가결구、봉와결구화서상결구,고령석정서본상결구,이리석여록니석정편가결구。
Aimed at investigating the hydrological characteristics and the plastic deformation of the deep soft rock for Xing’an mine in Hegang,this paper describes the study of mineral composition and the microstructure,based on five samples selected from the 500 m and the 740 m in buried depth,and using SEM-EDS techniques.The results show that the deep soft rocks occurring in Xing’an mine consist mainly of the Quartz,Feldspar,Calcite and some other clay mineral,except some specimen containing Siderite and Rutile.The primary mineral ingredients of clay mineral are Illite mixed layer(I/S),Illite,Kaolinite,Chlorite and so on.The Illite mixed layer is composed mainly of sodium-montmorillonite and Ca montmorillonite.Quartz overgrowth,Calcite dissolution,Feldspar leaching,cleavage-growth of Siderite are all found in the test of detrital minerals.Illite mixed layer shows laminated,honeycomb and flocculated structure.Kaolinite shows booked structure.Illite and Chlorite are of laminated structure.