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However, experts said Tsunehiro seamless iron ore resources through the "digging outside to inside", you can still break a certain extent, China in the world iron ore market in the dilemma has become China's iron and steel enterprises to open up new overseas iron ore supply channels to break the iron ore resource "bottlenecks" an important breakthrough in imports of iron ore so as to gradually establish a "China model" of China to face the world iron ore trade negotiations in the other a window.

但是恒博无缝管专家表示通过对铁矿石资源的&内挖外拓&,仍然可以在一定程度上打破中国在世界铁矿石市场中的窘境,成为我国钢铁企业开辟新的海外铁矿石供应渠道、打破铁矿石资源&瓶颈&制约的一次重要突破,从而逐步建立起进口铁矿石&中国模式&,成为中国面对世界铁矿石贸易谈判中的另外一扇窗。

Hypogene high thermal or deep source epi-mesothermal condition and it is not only stressed the mantle source simply but also the crust-mantle;②in order to guid ore exploration better the artificial classification of uranium deposits should be broken and uranium ore-forming system strengthened;③much attention should be paid to searching the diabase-hosted rich uranium ore in strongly argillized cataclastic zone;④attention should be paid to the influence of basement of volcanic basin on the uranium ore formation that should be undstood both in feeling and theoretically through the ore propect process;⑤relation of red basin with uranium ore formation can be made clear from analyzing tectonics, paleo-climate and time and it is not only theoretically important but also helpful to uranium ore prediction;⑥crypto explosive pipe is an uranium ore, rich uranium ore host structure and it is the next goal for uranium ore exploration in east China.

摘要文章论述了华东火山岩型铀矿找矿值得重视的地质问题:①铀成矿既可形成于浅源浅成低温条件,也可形成于深源深成高温或深源浅成中低温条件,在强调深源时,不是简单地认为是幔源就可以了,还必须强调壳幔作用的地质过程;②打破人为的&类型&划分,加强&铀成矿系统&的研究,更好地指导找矿;③研究基性脉体与铀成矿问题应注意构造、岩石矿物成分、成因、蚀变与成矿3大问题,注意寻找泥岩化作用强烈的破碎辉绿岩脉中的富铀矿;④火山盆地基底对铀成矿的作用主要是提供铀源,将基底对铀成矿的影响从感性认识推向理性认识,有效地指导找矿;⑤红盆与铀成矿关系可以从构造、古气候及时间分析研究中得出结论,它不仅仅是一个理论问题,而且有助于铀成矿预测;⑥隐爆角砾岩筒是铀成矿、成富矿的重要储矿构造,是华东火山岩型铀矿找矿的新领域。

According to model, lead zinc ore bodies of mineral deposit, celestite ore bodies and gypsum ore bodies are distributed by the incomplete dome shape. The sandstone type ore bodies like a curved surface shape, is on the top, wide distribution, which like the top cover of a mushroom. The limestone breccia type ore bodies, under the sandstone type ore bodies, with mostly irregular vein shape, lens body shape, locate at the root of the mushroom. Gypsum and celestite ore bodies, accompanying with limestone breccia type ore bodies with the shape of vein, lens body, distribute under the sandstone type ore bodies.

根据模型显示,金顶矿床铅锌矿体、天青石矿体和石膏矿体呈不完整的穹隆状分布,砂岩型矿体在上,为曲面状,分布广,似一蘑菇的顶盖,而灰岩角砾岩型矿体分布局限,部分产于砂岩型矿体之下,多为不规则的脉状、透镜体状,构成蘑菇的根部;石膏和天青石矿体主要与灰岩角砾型矿体相伴产出,呈脉状、透镜体状,多分布于砂岩型矿体下部。

Following were the main substances of this research: Rules of import-iron oresagglomeration, import-iron ores include Brazil CVRD iron ore、Indias high qualitymine、Brazil iron fine powder、Irani iron fine powder and Mauritania fine powder.Rules of rich iron ores of Tiangang agglomeration, it includes Laiyuan iron ore andQian'an iron ore.

本文主要研究内容包括:进口富矿粉的烧结成矿规律,进口粉主要包括巴西CVRD 粉、印度高品位粉、巴西铁精粉、伊朗粉和毛里塔尼亚粉;地方精粉主要包括涞源精粉和迁安精粉;在上述研究的基础上,进行合理烧结配矿的研究,从而得出合理的配矿方案和工艺参数。

Seven molybdenite samples from greisen ore body and quartz vein tungsten ore body associated with black tungsten ore were chosen for Re-Os isotopic dating and model age of (141.4±2.2) Ma~(158.2±2.2) Ma were obtained. The isochrone age of molybdenites from greisen type tungsten-tin ore body is (156.8±3.9) Ma, which indicates that its mineralogenetic epoch is at the Middle Jurassic, corresponds to the second stage of early Yanshanian period. And the model age for the samples from greisen ore body and from quartz vein ore body are (150.7±2.4) Ma~(158.2±2.2) Ma and (141.4±2.2) Ma~(151.0±2.4) Ma respectively, which indicates that the mineralization time of the quartz vein ore body is slightly earlier than that of greisen ore body.

文章选取云英岩型矿体及上部石英脉型钨矿体中与黑钨矿共生的辉钼矿7件,进行Re-Os等时线年龄测定,得到其模式年龄为(141.4±2.2) Ma~(158.2±2.2)Ma,其中云英型钨锡矿体中辉钼矿等时线年龄为(156.8±3.9)Ma,成矿时代为中侏罗世,对应于燕山早期第二阶段;从云英岩矿体中样品模式年龄为(150.7±2.4)Ma~(158.2±2.2)Ma,石英脉型矿体中样品模式年龄为(141.4±2.2)Ma~(151.0±2.4)Ma。

In the space, along with increased distance from the main ore-controlling structures, the frequency of P type of pyrite and their thermoelectricity also decreased gradually. Within one lode, from the upper to the lower parts of an ore body, the vertical change of pyrite in thermoelectricity as the follows:① when the ore body is stable, that is when the ore body is uniformly and continuously mineralized, the Dp andαvalues keep increased from shallow to deeper parts;② when an ore body is discontinuously mineralized, the Dp andαvalues have a wavy increasing tendency from the shallow to the deeper;③ when the deeper part of an ore body contains abundant, Co and Ni high mafic dykes, the Dp andαvalues of pyrite decreased from the shallow to the deeper parts of an ore body, that is, an reversed zoning of pyrite thermoelectricity occurs for pyrite in this situation contain more Ni and Co and belongs to N type.④ For the deposits hosted in the Archean metamorphic rocks, because all of the pyrite in this case is N-type, the vertical change of pyrite is not featured by the transition of pyrite type, but by the increased values of Vnp and α from the shallow to deeper parts of an ore body.

在空间域上,水平分带规律为:随远离主干断裂,矿脉中P型的出现频率逐渐降低或热电系数值逐渐变小;在同一条矿脉中,这是由于矿化不均匀性及脉岩的影响,由矿体的上部到下部,它的垂向变化特征可以有如下几种变化形式:①由矿体的浅部到深部,黄铁矿的Dp值、或α值呈稳定升高的趋势时,矿体往往表现为矿化均匀,连续性好、延伸稳定;②由浅部到深部,黄铁矿的Dp值、α值呈波状变化,但总体又具有增大的趋势时,所在的矿体连续性差;③当矿脉的下部发育有大量的基性脉岩时,由于基性脉岩中常含有较高的Co、Ni,使其中黄铁矿的Co、Ni含量较高而呈N型导电,由矿体的上部到下部,黄铁矿的Dp值、α值呈减少的趋势,而造成黄铁矿热电性特征的逆向分带,④产于太古代变质岩中的中深脉状金矿,由于其中的黄铁矿均为N型导电,所以垂向变化规律并不表现为导型的改变,只是Vnp值或α值从矿体的上部到下部由小变大。

Rail company's existing six red, four iron yellow, two black iron, an iron green, a total of 13 iron oxide pigment production line, under the holding company of Hangzhou Huayuan Germany, race, equity participation, companies such as Toda sambong an annual output of iron oxide paint 110,000 tons, including blending, roasting, ultra-fine deep processing production lines, annual output reached 10000 tons, the product varieties have iron oxide red, iron yellow, iron oxide black, iron orange, iron brown, green and ultra-fine iron, calcination deep-processing products, such as more than 50, more than 90% of export products, customers across five continents over 40 countries and regions.

公司现有六条铁红、四条铁黄、二条铁黑、一条铁绿,共十三条氧化铁颜料生产线,下属控股公司华源杭德、赛诺康、参股公司户田三峰等,年产氧化铁颜料11万吨,其中拼混、焙烧、超细深加工产品生产线,年产量达 10000余吨,产品品种有氧化铁红、铁黄、铁黑、铁橙、铁棕、铁绿以及超细、焙烧等深加工系列产品五十多个,产品90%以上外销,客户遍及五大洲四十多个国家和地区。

I can provide raw materials for the Division include: tantalum ore, niobium ore, tungsten ore, molybdenum ore, cobalt ore, nickel ore, monazite, zircon ore, chromium carbide, vanadium carbide and so on, the majority of imported raw materials.

我司可提供的原材料包括:钽矿、铌矿、钨矿、钼矿、钴矿、镍矿、独居石、锆矿砂、碳化铬、碳化钒等,大部分为进口原料。

Because the direct roof of the No.92 ore-body is the backfilling of the No.91orebody which is the cementing materials or non-cementing materials, and there are no-filled mined-areas in someplace. So there are large-scale hidden troubles on the top of the No.92 slowly inclined large and thick ore-body, then we must find a new mining technology which aims at the complex mining condition of the No.92 ore-body. The cutting nature of the No.92 ore-body is very poor, so choosing the rational drilling and blasting parameters and enhancing the overall technological economic benefits are also the urgent problems waiting to be solved in the exploitation of the No.92 ore-body. The No.92 ore-body, thin lodes and the exploitation process of the No.91orebody influence each other, the geo-pressure phenomena aggravates obviously in case of the mined-areas increase constantly, and the geo-pressure problem will be more and more serious when the No.92 ore-body be exploited on a large scale in the next step.

由于它的直接顶板就是开采91号矿体时的胶结或者非胶结的空区充填体,部分地段甚至是未充填的采空区,使92号缓倾斜厚大矿体的上部形成大范围的隐患区,因此,必须针对92号矿体复杂的开采技术条件,寻找新的采矿技术与工艺。92号矿体的可凿性极差,选择合理的凿岩爆破参数,提高凿岩爆破工作的总体技术经济效益,也是92号矿体开采急待解决的问题。92号矿体与细脉带、91号矿体开采相互影响,目前在采空区不断增大的情况下地压显现有明显加剧的趋势,在下一步92号矿体大规模开采时,地压问题将越来越严重。

In iron-deficient cells, photosynthetic pigments content decreased, efficiency of photosynthesis was low, With the increase of the concentration of the iron-chelator 2, 2'-Dipyridyl in media, Fv/Fm decreased, indicating photoinhibition increased, the results were consistent with previous research; Heterocyst induction had one delayed time dependent on the status of iron-deficiency, More severe of the iron-deficiency condition, more late of the heterocyst induction, It is possible that certain iron-related genes may directly regulate heterocyst development; under different iron limitation conditions, Protein pattern were different, more serious of the iron-deficiency conditions, less bands of the protein pattern, We could not find the iron-deficiency induced protein; In general the toxic effects of ROS were potentiated by excess iron, But our results revealed that even under iron-deficiency conditions, Oxidative damage existed.

铁限制的细胞光合色素含量下降,光合作用能力下降,随着铁螯合剂2,2'-dipyridyl浓度的增加,叶绿素荧光F〓/F〓逐渐降低,显示光抑制变强。与前人的研究结果相似;依赖铁缺失状态,异形胞诱导有一段推迟的时间,铁缺失越严重,诱导越迟,推断某些铁相关的基因会直接调节异形胞发育;在不同铁营养条件下,蛋白质图谱的变化趋势很明显,缺铁越严重,则蛋白质谱带数愈少,但本文未能找到特异诱导蛋白;一般认为铁过量情况下ROS产生加强,本文结果显示即便在铁缺失条件下,也有氧化胁迫伤害,而且缺铁越严重,活性氧伤害越大。

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