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中朝准地台北缘岩浆岩型磷矿成矿带东端朔州碱性杂岩及磷矿地质特征 被引量:1

Geologic features of Shuozhou alkali mixtite and phosphate deposits in the eastern end of magmatic phosphate metallogenic belt of China-Korea paraplatform north margin
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摘要 朔州碱性杂岩磷矿位于朝鲜北部平安北道,距鸭绿江约10km,大地构造位于中朝准地台营口-宽甸-狼林隆起东部,是朝鲜重要磷矿基地之一,与我国矾山和马伸桥含磷碱性杂岩处于同一构造岩浆岩带,这三个碱性杂岩型磷矿都是大型矿床。马伸桥和朔州碱性杂岩是塔里木-中朝准地台目前发现的两个典型超基性-碱性-碳酸岩三位一体的杂岩,是最具成矿远景的杂岩,根据“古老地台边缘及内部活动带受深大断裂控制的幔源超基性-碱性-碳酸岩杂岩型磷矿成矿模式”和预测准则,塔里木-中朝准地台该类碱性杂岩型磷矿成矿远景十分可观。朔州碱性杂岩划分为三期侵入岩:第一期为正长辉石岩类;第二期为碱性岩,包括碱性正长岩、霞石正长岩和霞石岩;第三期为碳酸岩,包括方解石碳酸岩和白云石碳酸岩。磷灰石矿有碳酸岩型、碱性岩型和交代型三个类型,矿石品位6.9%~9.5%(P2O5),探明储量1亿t,远景储量数亿t,此外伴生有蛭石矿。 Shuozhou phosphate deposit of alkaline mixtite is one of the important phosphate mine bases in DPRK.It is located in North Pyongan about 10 km from the Yalu River.It is located in the east of Yingkou-Kuandian-Langlin uplift of China-Korea paraplatform and is located in the same tectonic magmatic zone as Fanshan and Mashenqiao Phosphorus-containing mixtite.All three alkali mixtite phosphate mines are large deposits.Mashenqiao and Shuozhou alkaline mixtite are two typical superbasic-alkaline-carbonated Trinity mixtite found in Tarim-China-Korea paraplatform.They are the most metallogenic perspective mixtites.According to“the model of mantle source superbasic-alkaline-carbonated mixtite phosphate deposit which is controlled by deep faults on the edge of ancient platform margin and inner active zone”and the prediction rules,this kind of alkaline mixtite phosphate deposit is very considerable in Tarim-China-Korea paraplatform.Shuozhou alkaline mixtite is divided into three stages of intrusive rocks:the first stage is orthoclase pyroxenite;the second stage is alkaline rock,including alkaline syenite,nepheline syenite and nephelinite;the third stage is carbonatite,including calcite carbonatite and dolomite carbonatite.There are three types of apatite:carbonate,alkaline and metasomatic.The ore grade is 6.9%~9.5%(P2O5),the proven reserves are 100 million tons,the prospective reserves are hundreds of millions of tons,and the vermiculite is accompanied.
作者 东野脉兴 Dongye Maixing(Research Institute of Geology,China Chemical Geology and Mine Bureau,Bejing,100101,China)
出处 《化工矿产地质》 CAS 2020年第1期12-18,共7页 Geology of Chemical Minerals
关键词 中朝准地台 朝鲜朔州 碱性杂岩 磷灰石矿床 China-Korea paraplatform Shuozhou in DPRK Alkaline mixtite Apatite deposit
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  • 1东野脉兴.世界内生磷矿地质及成矿规律[J].化工矿产地质,2004,26(3):134-144. 被引量:9
  • 2白鸽 袁忠信.碳酸岩地质及其矿产[J].中国地质科学院矿床地质研究所所刊,1985,(1):99-140.
  • 3奥尼尔 J R 中国科学院地球化学研究所.稳定同位素在矿物学中的应用.氧同位素地化学[M].北京:科学技术文献出版社,1979.93-122.
  • 4邱家骧,秦巴碱性岩,1993年
  • 5牟保磊,矾山杂岩体磷.铁矿床,1988年
  • 6白鸽,中国地质科学院矿床地质研究所所刊,1985年,1期,1页
  • 7奥尼尔 J R,氧同位素地球化学,1979年,93页
  • 8牟保磊;江培谟;曾贻善.矾山杂岩体磷-铁矿床[M]{H}北京:北京大学出版社,1988.
  • 9东野脉兴,赵玉海,郑文忠,祖恩冬,曹作奇,韦钊.内生磷矿成矿规律及预测准则[J].化工矿产地质,1997,19(1):6-10. 被引量:7
  • 10安永福,东野脉兴.天津蓟县马伸桥含磷硷性杂岩及其地质意义[J].化工矿产地质,2011,33(3):129-136. 被引量:3

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