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1.
H2O-和D2O-NaAlSi3O2玻璃的红外光谱与无水钠长石玻璃的红外光谱之间有两大差别:一量有许多由数个O-H伸缩振动引起的高于3000cm^-1的谱带出现,二是在含水玻璃红外光谱中的900cm^-1附近出现一个谱肩。未发现因D-H置换而引起的900cm^-1谱肩的频率偏移。根据我们的红外光谱和分子轨道计算结果,以及以前的NMR和喇曼光谱,我们得出结论:H2O-钠长石玻璃的振动光谱中900cm  相似文献   

2.
石英和碳酸钙表面位的FDIR谱学研究   总被引:1,自引:0,他引:1  
本文采用漫反射红外光谱(FDIR)方法对石英、方解石、合成碳酸钙和孔雀石等矿物表面位(基团)作了研究。随着溶液pH值的升高,由于表面基团间氢键的影响,石英表面位〉Si-O和〉Si-O-Si的吸收峰向高频方向漂移,即〉Si-O非对称伸缩振动吸收峰由1036cm^-1→1045cm^-1→1047cm^-1,〉Si-O-Si对称伸缩振动吸收峰由777cm^-1→782cm^-1→788cm^-1,而〈  相似文献   

3.
谷湘平 《矿产与地质》1995,9(4):275-279
研究了不同程度变生褐帘石及其热处理样品的红外光谱变化特征,提出其变生的红外光谱定量标志-变生度M=1/5(6-N)(N为750-200Cm^-1范围的谱带数)。分析了变生作用中褐帘石晶格内离子基团的变化,结合晶体结构分析,提出褐帘石红外光谱中450、510cm^-1附近的两个谱带分别系结构内孤立硅氧四面体SiO4及群体硅氧四面体Si2O7的弯曲振动谱带。  相似文献   

4.
林传易  田淑贵 《矿物学报》1994,14(2):134-141
本文采用U-B力场在位置群近似时对锆石中SiO^4-4离子的内振动进行了简正坐标分析,振动频率的计算值与观察值吻合很好。根据简正坐标分析确定的力常数值为Kr=400,H1=44,H2=60,F=25N.m^-1。  相似文献   

5.
热液体系中Si的络合作用   总被引:1,自引:0,他引:1  
在不同温度、PH和硅浓度条件下,实验标定了Au-SiO以及Sn-SiO2之间的络合反应:Au^++H3SiO4^-之间的络合反应:Au^++H4SiO=AuH3SiO4 lgK=-1.65436+9611.21/T;Sn^4++4H3SiO4^-=Sn(H3SiO4)4;lgK200c=42.73。通过与Au-Cl、Au-HS以及Sn-OH络合物迁移能力的比较,表明在具地质意义的P睡EH条件下,A  相似文献   

6.
黄铁矿的中远红外谱及其对含金性的评价   总被引:4,自引:0,他引:4  
贾建业 《西北地质》1996,17(3):59-65
针对黄铁矿的具体情况,笔者采用中─远红外幅射以及透射吸收谱与反射吸收谱相比较的方法,对其红外光谱特征和含金性评价进行了系统全面的研究,确定了黄铁矿含金性的红外光谱评价准则是:v1、v2、v3吸收带的频率分别低于415cm-1、347cm-1、287cm-1,Tov1-Tv1值低于30,Tov2—Tv2值低于5时为富金;相反的情况为贫金或无金。在样品物质浓度(C)相同的条件下,黄铁矿特征吸收带的光密度(D)值随其含金性提高而变小。  相似文献   

7.
海泡石粘土矿的应用史玉芳姜燕冬(中国地质大学测试中心,武汉430074)关键词海泡石结构性质用途海泡石属于海泡石-坡缕石粘土矿物族,是一种纤维状含水镁硅酸盐矿物,其典型的化学式为:Mg8Si12O30(OH)4(OH2)48H2O,但其化学成分变化较...  相似文献   

8.
云南乐红铅锌矿床氧化带中异极矿的矿物学特征及其意义   总被引:7,自引:0,他引:7  
云南乐红铅锌矿床氧化带十分发育,呈细脉或葡萄状产于氧化矿石中的白色矿物曾被认为是菱锌矿,笔者对该矿物作了物理、光学性质,化学发,X射线衍射,红外光谱及失重和差热分析研究,确定其为异极矿。其晶体化学式为Zn3.98(Si2.01Al0.01)2.02O7(OH)2.03.0.88H2O晶胞参数a=0.8380(4)nm,b=1.0718(7)nm,c=0.5125(6)nm。对异极矿矿物学特征的全面  相似文献   

9.
彭明生  王后裕 《矿物学报》1995,15(4):372-377
利用偏振喇曼光谱(PRS)和傅里叶变换红外光谱(FTIR)研究了三种不同成因电气石单晶的振动谱学特征。PRS研究表明电气石结构中三个阴离子团(即[Si6O18]^12-、[BO3]^3-、[OH]^-)的喇曼谱在平行c轴方向(//NE)比垂直c轴方向(//NO)敏锐,而且[OH]^-喇曼光谱只在平行c轴的PRS中才观察到。不同成因电气石中[OH]^-占位不同。结合FTIR研究发现在伟晶型和热液型的  相似文献   

10.
本文采用合成溶胶凝胶中间体的技术方法,降低了硅酸盐熔体的熔化温度,并在1750~1850℃和2.0~4.0GPa条件下合面出9个SiO2-Al2O3-Na2O(K2O)系列淬火硅权盐熔体,淬火熔体中Na(K)/A1≤1属过铝质硅酸盐熔体,其激光拉曼微探针(LRM)研究表明,随压力增大,T-Onb在高频区(900~1200cm^-1)的对称和反对称伸缩振动频率明显减小,过铝质熔体中存在六配位铝,且随  相似文献   

11.
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.  相似文献   

12.
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14.
正1 Introduction Geological studies established on several sections in Lanping-Simao basin have shown that the salt-bearing strata of Mengyejing formation(Yunlong Fm.in Lanping basin)are constituted by an alternation of salt layers and interbedded facies.The latter consists mainly of mudstones,and mudstone-rich conglomerate.The mineralogy and geochemistry of salt-bearing beds and  相似文献   

15.
正On 22nd April 2014,with the approach of the 45th World Earth Day,China’s Ministry of Land and resources issued the status of China’s mineral resources in 2013.The first task of the prospecting breakthrough strategy action implemented in the last five years has been completed,and China’s security capacity for mineral resources has been significantly improved.In the  相似文献   

16.
正There are more than 700 salt lakes with area of more than 1km2 on the Qinghai-Tibet Plateau of China.In recent years,an oilfield brine was also found in the Nanyishan Section of Qaidam Basin in the Qinghai-Tibet  相似文献   

17.
正1 Introduction Physical and numerical models are constructed to investigate the evolution and mechanism of salt migration driven by tectonic processes.In recent years,we have designed and ran series of models to simulate salt  相似文献   

18.
正The study of Cretaceous-Palaeogene salt-bearing strata of the Khorat Basin Laos and the Lanping-Simao Basin in Yunnan,China has an great significance not only in explaining the basin evolution and the genesis of potash  相似文献   

19.
正Potash is one of the long-term scare deposits in China,and potash prospecting has long been listed as a key brainstorm project for our nation and geological prospecting units.There have been considerable studies in search for potash deposits in the Kuqa depression of the Tarim basin(Jackson et al.,1991;Gemmer et al.,2004;Vendeville,2005;Vendeville and Jackson,1992a,1992b),  相似文献   

20.
正1 Introduction Qaidam Basin in Qinghai,including 43 salt lakes with multiple dominant mineral such as potassium,magnesium,lithium etc.,is the most intensive distribution of Saline  相似文献   

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