内蒙古锡盟扎布其铁矿地质特征及成因
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摘要
内蒙古锡盟扎布其铁矿是近三年内新发现的一个规模大、出露浅的超贫钒钛磁铁矿矿床。
矿床位于内蒙古自治区西乌珠穆沁旗巴音高勒苏木，大地构造位置属于华北板块北缘晚古生代陆缘增生带。区内岩浆岩主要为辉长岩和辉石闪长岩，受北东向断裂构造控制，与铁矿化关系密切。区内相对较高的磁异常值主要集中在辉长岩与辉石闪长岩分布处，其走向也呈北东或近东西走向展布。
大量地质研究表明：辉长岩与辉石闪长岩为扎布其铁矿床的含矿矿体。矿体主要以不规则状分布于辉长岩岩体的中下部，受北东向断裂构造控制，产状与辉长岩大致平行，规模较大，延长从几百米到1000m以上，宽度几十米到100m。晚期脉状矿体则明显充填于岩体中的原生构造裂隙中，但规模一般较小。
扎布其铁矿的主要矿石矿物为磁铁矿、赤铁矿、黄铁矿、斜长石、磷灰石、辉石、黑云母、角闪石；次要矿石矿物为钛铁矿、钒磁铁矿、黄铜矿和石英等。矿石构造有浸染状构造、脉状构造、团块状构造和块状构造等，矿石结构具有结晶分异特点，包括胶状结构、海绵陨铁结构、半自形粒状结构等。
其中，磁铁矿主要以稀疏浸染状和海绵陨铁状填隙在造岩矿物粒间，且结晶分异程度弱，富集程度低。磁铁矿是晚于辉石和斜长石形成，这与河北大庙黑山钒钛磁铁矿有一定的相似性。
扎布其矿区矿石品位分析结果为22.8%，已达到超贫磁铁矿的工业要求。同时，矿石中TiO2为1.67%；V2O5为0.1~0.4%，平均为0.25%，可综合回收利用。综合分析显示矿石铁产品为Ⅰ级品。
辉长岩中锆石U-Pb测年结果显示扎布其铁矿的成矿年龄为337±1.5Ma，即晚古生代早石炭世。根据矿石化学全分析结果可知扎布其岩体为富含钒、钛和铁的镁铁质基性岩——即辉长岩与辉石闪长岩，属有利于形成钒钛磁铁矿的岩类。对比攀枝花及河北大庙黑山钒钛磁铁矿，整理分析当前资料可知：扎布其铁矿属于与镁铁质辉石闪长岩——辉长岩有关的非层状晚期岩浆矿床。其中大部分矿体以非层状、不规则状产出于岩体的中下部，为受北东向的断裂控制的岩浆结晶分异型矿体。少量发育在岩浆岩内原生裂隙中的脉状矿体为贯入型矿体，受岩浆岩原生裂隙控制。因此，扎布其铁矿是一个大型的与镁铁质侵入岩有关的非层状超贫钒钛磁铁矿矿床，属贯入——分异型晚期岩浆类型，以分异型为主。
因为扎布其铁矿规模大，埋藏浅，采矿成本低，而选矿工艺要求却相对简单，所以在当前铁矿石市场前提下经济效益还是十分明显的。
The Zhabuqi iron deposit in Xiwuqi of Inner Mongolia is a discoveredultralow-grade vanadium-bearing titanomagnetite deposit which is large scale andshallow occurrence in the last three years.
The mining area belonging to the Bayingaolesumu in Xiwuzhumuqing of theInner of the Mongolia Autonomous Region, the tectonically belongs to the NorthChina plate north of the Late Paleozoic continental margin accretion zone. Magmaticrocks of the region as the gabbro and pyroxene diorite, by NE trending faults controlis closely related to the iron ore of. Region with relatively high magnetic anomalyvalues mainly at the distribution in the gabbro and pyroxene diorite, and the trend alsowas to the north east or near east-west, which reflects the boundaries of theore-bearing rock.
Large number of geological studies have shown that: gabbro and pyroxenediorite the Zarb its iron ore deposits containing ore body. Orebody invasive irregularoutput in the lower part of the gabbro body, by the north-east trending faults control,and occurrence of gabbro is roughly parallel to the larger, extending from a fewhundred m to1000m, width range from tens of meters to300meters. See also latevein-like ore bodies filling in native tectonic fractures of the rock, but the scale isgenerally small.
The Zarb its iron ore, the main ore minerals are magnetite, hematite, pyrite, plagioclase, apatite, pyroxene, biotite and hornblende; secondary ore mineralsilmenite and vanadium magnetite, chalcopyrite and quartz. The ore structures includedisseminated structure, vein-like structure, massive structure and block structure.oretextures have characteristics of crystallization differentiation, including the colloidaltexture, sponge iron meteorite texture, hypidiomorphic-granular texture.
Among them, magnetite is mainly through sparse disseminations and sponge ironmeteorite-like filled in caulking between rock-forming mineral particles, andcrystalline differentiation of low degree, indicating that magnetite is later than theformation of pyroxene and plagioclase, which the Hebei temple Montenegrothere is acertain similarity in the vanadium-titanium magnetite.
Its mine ore grade analysis is22.8%in The Zarb, reaching the industrialrequirements of the ultra-poor magnetite. Ore TiO2is1.67%; of V2O5and0.1~0.4%,an average of0.25%can recycling.Comprehensive analysis show that the ore ironproducts Ⅰ grade.
Gabbro zircon U-Pb dating results show that The Zarb its iron ore mineralizationage of337±1.5Ma,meaning Late Paleozoic Early Carboniferous.According to zheresult of ore chemical analysis, we can know The Zarb its rock is mafic rock (richingin vanadium, titanium and iron)——Gabbro and pyroxene diorite, it is a kind of rocksthat favored the formation of vanadium and titanium magnetite.Contrast Panzhihuaand Hebei temple Montenegro vanadium-titanium magnetite, and analyzed the currentdata shows: the Zarb its iron ore belongs to non-layered late magmatic deposits aboutmafic pyroxene diorite rocks-gabbro. Most of the ore body is a non-layered, irregularoutput in the rock mass in the lower part of special-shaped ore body, which is amagma crystallization and differentiation-type Orebody controled by the NE to thefault-controlled magma crystallization. The development of a small amount of nativevein ore bodies in the fissures of penetration type ore deposits are magmatic rocksexisting fractures control within the magmatic rocks. Therefore,the Zarb its iron oreis the non-layered ultra-poor vanadium titanium magnetite deposit, a large maficintrusive rocks related to the case of penetration-sub-Shaped late magmatic deposits,mainly sub-Shaped.
Because of the large scale of Zarb its iron ore,lying shallow in the earth, lowcost of mining,beneficiation process requirements are relatively simple, the premiseof the current iron ore market is still quite cost-effective.
矿床位于内蒙古自治区西乌珠穆沁旗巴音高勒苏木，大地构造位置属于华北板块北缘晚古生代陆缘增生带。区内岩浆岩主要为辉长岩和辉石闪长岩，受北东向断裂构造控制，与铁矿化关系密切。区内相对较高的磁异常值主要集中在辉长岩与辉石闪长岩分布处，其走向也呈北东或近东西走向展布。
大量地质研究表明：辉长岩与辉石闪长岩为扎布其铁矿床的含矿矿体。矿体主要以不规则状分布于辉长岩岩体的中下部，受北东向断裂构造控制，产状与辉长岩大致平行，规模较大，延长从几百米到1000m以上，宽度几十米到100m。晚期脉状矿体则明显充填于岩体中的原生构造裂隙中，但规模一般较小。
扎布其铁矿的主要矿石矿物为磁铁矿、赤铁矿、黄铁矿、斜长石、磷灰石、辉石、黑云母、角闪石；次要矿石矿物为钛铁矿、钒磁铁矿、黄铜矿和石英等。矿石构造有浸染状构造、脉状构造、团块状构造和块状构造等，矿石结构具有结晶分异特点，包括胶状结构、海绵陨铁结构、半自形粒状结构等。
其中，磁铁矿主要以稀疏浸染状和海绵陨铁状填隙在造岩矿物粒间，且结晶分异程度弱，富集程度低。磁铁矿是晚于辉石和斜长石形成，这与河北大庙黑山钒钛磁铁矿有一定的相似性。
扎布其矿区矿石品位分析结果为22.8%，已达到超贫磁铁矿的工业要求。同时，矿石中TiO2为1.67%；V2O5为0.1~0.4%，平均为0.25%，可综合回收利用。综合分析显示矿石铁产品为Ⅰ级品。
辉长岩中锆石U-Pb测年结果显示扎布其铁矿的成矿年龄为337±1.5Ma，即晚古生代早石炭世。根据矿石化学全分析结果可知扎布其岩体为富含钒、钛和铁的镁铁质基性岩——即辉长岩与辉石闪长岩，属有利于形成钒钛磁铁矿的岩类。对比攀枝花及河北大庙黑山钒钛磁铁矿，整理分析当前资料可知：扎布其铁矿属于与镁铁质辉石闪长岩——辉长岩有关的非层状晚期岩浆矿床。其中大部分矿体以非层状、不规则状产出于岩体的中下部，为受北东向的断裂控制的岩浆结晶分异型矿体。少量发育在岩浆岩内原生裂隙中的脉状矿体为贯入型矿体，受岩浆岩原生裂隙控制。因此，扎布其铁矿是一个大型的与镁铁质侵入岩有关的非层状超贫钒钛磁铁矿矿床，属贯入——分异型晚期岩浆类型，以分异型为主。
因为扎布其铁矿规模大，埋藏浅，采矿成本低，而选矿工艺要求却相对简单，所以在当前铁矿石市场前提下经济效益还是十分明显的。
The Zhabuqi iron deposit in Xiwuqi of Inner Mongolia is a discoveredultralow-grade vanadium-bearing titanomagnetite deposit which is large scale andshallow occurrence in the last three years.
The mining area belonging to the Bayingaolesumu in Xiwuzhumuqing of theInner of the Mongolia Autonomous Region, the tectonically belongs to the NorthChina plate north of the Late Paleozoic continental margin accretion zone. Magmaticrocks of the region as the gabbro and pyroxene diorite, by NE trending faults controlis closely related to the iron ore of. Region with relatively high magnetic anomalyvalues mainly at the distribution in the gabbro and pyroxene diorite, and the trend alsowas to the north east or near east-west, which reflects the boundaries of theore-bearing rock.
Large number of geological studies have shown that: gabbro and pyroxenediorite the Zarb its iron ore deposits containing ore body. Orebody invasive irregularoutput in the lower part of the gabbro body, by the north-east trending faults control,and occurrence of gabbro is roughly parallel to the larger, extending from a fewhundred m to1000m, width range from tens of meters to300meters. See also latevein-like ore bodies filling in native tectonic fractures of the rock, but the scale isgenerally small.
The Zarb its iron ore, the main ore minerals are magnetite, hematite, pyrite, plagioclase, apatite, pyroxene, biotite and hornblende; secondary ore mineralsilmenite and vanadium magnetite, chalcopyrite and quartz. The ore structures includedisseminated structure, vein-like structure, massive structure and block structure.oretextures have characteristics of crystallization differentiation, including the colloidaltexture, sponge iron meteorite texture, hypidiomorphic-granular texture.
Among them, magnetite is mainly through sparse disseminations and sponge ironmeteorite-like filled in caulking between rock-forming mineral particles, andcrystalline differentiation of low degree, indicating that magnetite is later than theformation of pyroxene and plagioclase, which the Hebei temple Montenegrothere is acertain similarity in the vanadium-titanium magnetite.
Its mine ore grade analysis is22.8%in The Zarb, reaching the industrialrequirements of the ultra-poor magnetite. Ore TiO2is1.67%; of V2O5and0.1~0.4%,an average of0.25%can recycling.Comprehensive analysis show that the ore ironproducts Ⅰ grade.
Gabbro zircon U-Pb dating results show that The Zarb its iron ore mineralizationage of337±1.5Ma,meaning Late Paleozoic Early Carboniferous.According to zheresult of ore chemical analysis, we can know The Zarb its rock is mafic rock (richingin vanadium, titanium and iron)——Gabbro and pyroxene diorite, it is a kind of rocksthat favored the formation of vanadium and titanium magnetite.Contrast Panzhihuaand Hebei temple Montenegro vanadium-titanium magnetite, and analyzed the currentdata shows: the Zarb its iron ore belongs to non-layered late magmatic deposits aboutmafic pyroxene diorite rocks-gabbro. Most of the ore body is a non-layered, irregularoutput in the rock mass in the lower part of special-shaped ore body, which is amagma crystallization and differentiation-type Orebody controled by the NE to thefault-controlled magma crystallization. The development of a small amount of nativevein ore bodies in the fissures of penetration type ore deposits are magmatic rocksexisting fractures control within the magmatic rocks. Therefore,the Zarb its iron oreis the non-layered ultra-poor vanadium titanium magnetite deposit, a large maficintrusive rocks related to the case of penetration-sub-Shaped late magmatic deposits,mainly sub-Shaped.
Because of the large scale of Zarb its iron ore,lying shallow in the earth, lowcost of mining,beneficiation process requirements are relatively simple, the premiseof the current iron ore market is still quite cost-effective.
引文
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