脉金矿体侧伏研究方法及应用

从构造解析，构造地球化学，构造地球物理学，岩石矿物学，地质类比等方面探讨脉金矿体测伏的研究方法，并阐明其在岩金勘查和矿山开采中的应用，以提高脉金深部勘探工程和采矿坑道工程的设计中率。     

新疆若羌县红十井金矿地质特征及深部成矿预测

红十井金矿，产于中，上石炭统基性火山岩和火山碎屑岩中，为受断裂带控制的韧性剪切带型金矿床，原认为主矿体南倾，未查明侧伏方向，在体南侧和中，东段布钻，深部未打到矿体，仅求得0．947t金储量。笔者等经地质构造，矿体空间展布形式，矿物热电性和电磁场测深等研究，预测主体北倾，西挺，南西西侧伏，北东东仰起，在主矿体北侧和中、西段布钻，结果在深部和中、西段均打到了矿体，金储量由0．47t增加至10．1t以上，取得了突破性进展。     

广东云浮金子窝锡多金属矿床控矿条件与矿化分布规律

云浮金子窝锡多金属矿床位于广东四会—吴川构造带与肇庆—海丰纬向构造交汇部位。主要控矿条件包括基底地层、岩浆岩、构造等。主断裂派生的次一级断裂交切部位控制了矿床的定位和空间展布。寒武纪地层的W、Sn等元素含量较高，是重要的矿源层。后期的热事件使成矿元素发生重新分布。混合岩化和花岗岩化作用，使锡等成矿元素在矿液中逐渐富集，并在压力驱使下沿构造裂隙上升，在围岩中有利地段充填交代形成矿床。矿床存在垂直方向变化。根据矿体在空间上的原始展布和变化规律，对矿区边部和深部之隐伏矿体进行了预测。     

Certified Reference Materials of Copper, Lead and Zinc (Silver) Ore Rocks and Their Concentrates (GSO 1-7)

Sulfide mineral certified reference materials GSO 1-7, recently prepared by the Institute of Geophysical and Geochemical Exploration (IGGE), were analysed by twelve laboratories. Various reliable analytical methods based on different principles were adopted and classical chemical methods were taken as the primary analytical methods, by which 5729 determinations were carried out, 1425 average data were obtained, and twenty one to twenty seven elements and components were certified.     

二人沟硼矿床断裂构造与找矿关系探讨

二人沟硼矿床发育有大规模北北东向的逆掩断层,但在以往的工作中对断层的特征了解得不甚清楚,以致于找矿工作未取得满意的效果。通过对原有资料的分析研究,总结出该断层的特征,有效地指导了找矿工作,取得了寻找隐伏矿体的重大进展。     

湖南锡铅锌矿勘查与社会经济可持续发展研究

湖南锡铅锌资源丰富，保有储量列全国第四位，是我国重要的锡铅锌矿工业基地之一，锡铅锌矿业对满足省内外消费需求、促进出口贸易、创造就业机会及发展相关产业起着十分重要的作用．然而，湖南锡铅锌资源保证程度不高，现有锡铅锌保有储量保证年限均在10a以下，很难满足日益增长的国内外需要．作者认为采取“合理部署国土资源大调查工作，加强老矿山周边及深渐找矿工作，建立矿业权市场、加大地勘投入，努力提高资源综合利用水平”等措施可应对社会经济可持续发展对锡铅锌勘查的挑战．     

Determination of Chromium, Nickel, Copper and Zinc in Milligram Samples of Geological Materials Using Isotope Dilution High Resolution Inductively Coupled Plasma-Mass Spectrometry

A simple and accurate method for the determination of Cr, Ni, Cu and Zn at μg g^?1 levels in milligram‐sized bulk silicate materials is reported using isotope dilution high‐resolution inductively coupled plasma‐mass spectrometry (HR‐ICP‐MS) with a flow injection system. Silicate samples with Cr, Ni, Cu and Zn spikes were digested with HF‐HBr and Br₂, and subsequently decomposed at 518 K in a Teflon bomb. In this procedure, all sulfides and chromite, major hosts of these elements, were completely decomposed, thus allowing for isotope equilibration between the sample and spike. Magnesium and Al fluorides formed after the digestion of the sample were removed by centrifugation, and the supernatant was directly aspirated into a HR‐ICP‐MS at a mass resolution of 7500, where interfering oxide ions, ArO⁺, CaO⁺, TiO⁺, CrO⁺ and VO⁺, were separated from Cr⁺, Ni⁺, Cu⁺ and Zn⁺. No matrix effects were observed down to a dilution factor of 50. Detection limits for these elements in silicate samples were < 0.04 μg g^?1. The effectiveness of the technique was demonstrated by the analysis of 13 to 40 mg test portions of USGS and GSJ silicate reference materials with a major element composition ranging from andesite to peridotite, in addition to 8‐23 mg of the Smithsonian reference Allende. Both the reproducibility and the deviation from the reference value for most reference materials of various rock types were < 9%, and thus confirm that the method gives accurate analytical results for small sample sizes over a wide range of Cr, Ni, Cu and Zn contents. This method is, therefore, suitable for analysing small and/or precious bulk samples, such as meteorites, mantle peridotites and mineral separates, and for the characterisation of silicate and sulfide minerals for use as calibration samples in secondary ion mass spectrometry or laser ablation ICP‐MS.     

玲珑金矿田矿物组合与地球化学分带及矿体定位预测意义

详细讨论了玲珑金矿田矿物组合和元素的空间分带，二之间的一致性说明矿物组合的空间分带是宏观的元素地球分带，且具有远程有序和短程无序的特点。同时在矿田水平方向上，由于SE→NW金属矿物的种类和含量呈增加的趋势，由少硫化物蚀变岩型向多金属硫化物石英脉型变化。由于不同矿物组合的矿脉赋矿标高具有较大的差异，这为矿体的定位预测提供了矿物学依据；另外矿物组合的垂向分带，对判定矿体的剥蚀深度和延深也具有重要的参考价值。     

旧店金矿1号脉支脉的勘探及矿床成因分析

分析了旧店矿区的各项地质特征,根据规模、蚀变、细脉标志等特征对1号脉的支脉提出了勘探建议,并对圈定矿体作了详细阐述,认为该支脉与1号脉同期形成并略显张性,上覆1号脉与支脉二者之间的细脉对该支脉的成矿起了重要作用。     

干旱区绿洲土壤共存重金属元素形态变化及生物有效性实验分析

采用盆栽试验,初步研究了干旱区绿洲土壤—胡萝卜系统中镉、锌、镍3种重金属的形态变化特征及其生物有效性问题。结果表明：供试绿洲土壤原状土中,Cd、Zn、Ni均以稳定的残渣态形式存在,而处理土壤中重金属被钝化的量有限,Cd的存在形式主要以碳酸盐态为主,Zn、Ni则主要以铁锰氧化态为主;3种元素的活性大小依次为Cd＞Ni＞Zn。根据回归分析,元素Zn对胡萝卜块茎和茎叶吸收Zn量贡献最大的分别是Zn的碳酸盐结合态和铁锰氧化态;元素Ni对胡萝卜各部位吸收贡献最大的均为Ni的铁锰氧化态。