中国矿业
中國礦業
중국광업
CHINA MINING MAGAZINE
2015年
6期
76-80
,共5页
叶枫%董国臣%郭红党%孟兆国%赵增杰%韩怀亮
葉楓%董國臣%郭紅黨%孟兆國%趙增傑%韓懷亮
협풍%동국신%곽홍당%맹조국%조증걸%한부량
铝土矿%稀土元素%王润-西崖底%矿床成因
鋁土礦%稀土元素%王潤-西崖底%礦床成因
려토광%희토원소%왕윤-서애저%광상성인
bauxite deposits%rare-earth elements%Wangrun-Xiyadi region%genesis of deposit
山西交口‐汾西地区王润‐西崖底铝土矿床是山西省地质调查院近年来发现的大型铝土矿床。本文通过对王润‐西崖底铝土矿的研究,分析铝土矿样品的稀土元素含量特征,研究铝土矿床稀土元素分布特征以及与铝土矿床的关系,探讨稀土元素对于本区铝土矿成因和环境的指示意义。研究表明:该区铝土矿体的ΣREE总量较大,轻稀土元素相对富集,具有明显的Eu负异常;利用稀土元素图解大致反映出铝土矿成矿物质的来源于上地壳,底板碳酸盐岩为铝土矿床源岩,铝土矿形成于海相或海陆过渡相弱氧化环境。铝土矿床ΣREE与Al2 O3含量存在正相关性。
山西交口‐汾西地區王潤‐西崖底鋁土礦床是山西省地質調查院近年來髮現的大型鋁土礦床。本文通過對王潤‐西崖底鋁土礦的研究,分析鋁土礦樣品的稀土元素含量特徵,研究鋁土礦床稀土元素分佈特徵以及與鋁土礦床的關繫,探討稀土元素對于本區鋁土礦成因和環境的指示意義。研究錶明:該區鋁土礦體的ΣREE總量較大,輕稀土元素相對富集,具有明顯的Eu負異常;利用稀土元素圖解大緻反映齣鋁土礦成礦物質的來源于上地殼,底闆碳痠鹽巖為鋁土礦床源巖,鋁土礦形成于海相或海陸過渡相弱氧化環境。鋁土礦床ΣREE與Al2 O3含量存在正相關性。
산서교구‐분서지구왕윤‐서애저려토광상시산서성지질조사원근년래발현적대형려토광상。본문통과대왕윤‐서애저려토광적연구,분석려토광양품적희토원소함량특정,연구려토광상희토원소분포특정이급여려토광상적관계,탐토희토원소대우본구려토광성인화배경적지시의의。연구표명:해구려토광체적ΣREE총량교대,경희토원소상대부집,구유명현적Eu부이상;이용희토원소도해대치반영출려토광성광물질적래원우상지각,저판탄산염암위려토광상원암,려토광형성우해상혹해륙과도상약양화배경。려토광상ΣREE여Al2 O3함량존재정상관성。
The bauxite deposits in Shanxi Wangrun‐Xiyadi region ,which was found by Shanxi Institute of Geological Survey in recent years ,it is a large‐size deposits .Through the research of bauxite deposits , analyze the content of the rare‐earth elements in samples of deposits ,and research the relationship between the characteristics of rare‐earth elements and the deposits ,discuss the significance of the genesis and environment of bauxite deposits from the rare‐earth elements .This study shows that the ΣREE of bauxite deposits is large in this region ,light REE relative enriched ,with Eu negative abnormality ;using the diagram of REE ,we know that the metallogenic source material comes from the upper crust .The carbonate rock of bottom plates is source bed .The bauxite deposits occur on the weak oxidation environment of Marine or Transitional facies ,there was positive correlation between the ΣREE and Al2 O3 in deposits .