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学文 《资源导刊(河南)》2007,(9)
这是一个令人振奋的喜讯. 据河南省国土资源厅于2007年9月5日召开的新闻发布会透露,截至8月底,全省已有4个省辖市、53个县(市、区),在经历了一年多的艰苦、细致工作后,终于关闭了辖区内的所有砖瓦窑厂,与"秦砖汉瓦"彻底告别.让我们记住吧,记住这4个省辖市的名字.它们分别是:漯河市、安阳市、鹤壁市、焦作市.让我们记住吧,记住这53个县(市、区)的名字.它们中有:舞阳县、临颍县、召陵区、文峰区、淇滨区、修武县、孟州市、伊川县等. 相似文献
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一边是蒜苗、菠菜、生菜等各种时令蔬菜,一边的猪圈内有五头将要出栏的肥猪.猪圈旁边是沼气池,沼气池为水泥结构,圆锥形,上边留一个直径有半米的圆孔以便向内填充植物垃圾和秸秆,其余的地方用土填好以后还可以种上菜,墙根没有硬化的地方,还零落地留着苦瓜、南瓜的枯藤.这是日前笔者在修武县城关镇河北辛庄村民范庆河家中看到的景象. 相似文献
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浙东大地,河山锦绣,景奇色美.其中许多景区藏而不露,少为世人所知,东海之滨的桃渚便是一例.
桃渚景区是8000万年前火山喷发而形成的独特的火山遗迹地貌,即喀斯特地貌.山上古洞幽壑遍布,奇岩秀石突兀,断崖索桥点缀,处处皆是大自然的神来之笔,令人叹为观止.与天台、雁荡等名山大川相比,亦毫不逊色.怪不得当年文天祥逃出元军的囚禁,落荒从海道经桃渚时,被桃渚雄奇瑰丽的风景所感动,情不自禁赋诗赞美:"海上仙子国,邂逅寄孤蓬.万象图画里,千崖玉界中." 相似文献
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修成国 《资源导刊(河南)》2007,(3)
法国有许多在世界上驰名的标志性建筑或胜地,仅巴黎就有卢浮宫、凡尔赛宫、凯旋门、埃菲尔铁塔、巴黎圣母院等.笔者这里要说的是那条尽人皆知的香榭丽舍大街. 一些历史性的建筑往往标志着一个城市或地区的文化含量.而一条大街则常常标志着这一个城市或地区经济上的繁荣.如美国纽约的华尔街金融大街;日本的银座和日本桥商业街;我国北京的王府井商业大街,都成为这个城市甚至国家的代表.香榭丽舍大街则是巴黎乃至法国的代表. 相似文献
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于文 《资源导刊(河南)》2007,(3)
亲爱的读者朋友,正所谓"春风送佳音,百花迎宾来".当您在办公室里、在田间地头、在行进的火车上捧起本期杂志时,您可能会有一个惊奇的发现:几年来,您一直热情关注和钟爱的《河南国土资源》杂志,经国家新闻出版署批准,已正式更名为《资源导刊》了.我国期刊园林又盛开了一朵鲜艳的花朵. 相似文献
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嵌入式技术以及信息技术的发展使得越来越多的设备接入网络成为可能,这两项技术的融和具有广泛的应用前景.首先分析了嵌入式系统网络化的需求,结合对嵌入式操作系统Vxworks和对ARM芯片的研究,分析了相关网络协议,最后提出构建嵌入式WebServer的软硬件解决方案. 相似文献
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A field monitoring system was established in an active river bank landslide in the Three Gorges area, China, and a consecutive monitoring for about 5 years were conducted to understand the displacement characteristics of flexible piles and the surrounding soil. It was found that piles deformed elastically under reservoir operation, and the soil in front of piles was gradually separated from piles. The movement of the pile heads exceeded that of the soil between and behind piles. This phenomenon was further studied by a large-scale physical model test to gain insights into the pile-soil interaction. The displacement relationship between pile heads and the surrounding soil is in good agreement with the field data. The physical model test shows that the deformation process of pile-reinforced landslides can be divided into two stages: firstly, when the piles head movement exceeds soil movement, the soil arching is mainly affected by the deflection of the piles, the arches between and behind piles bent upwards;but when the soil movement exceeds piles head movement, the arches near the upslope and downslope bent downwards and upwards, respectively. Furthermore, the different deformation of two adjacent piles and the pile stiffness influenced the arch’s shape and formation;the flexible piles exhibit great coordinated deformation with the landslide, and caused the soil arch on the downslope. 相似文献
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在嵌入式产品开发中,除操作系统之外,开发人员关注最多的一个系统软件组件就是图形支持系统.只要是面向人机交互的嵌入式产品,就涉及到文字或者图形的输出.通过比较各种嵌入式Linux平台上的GUI系统的结构和特点,最终选定了MiniGUI作为研究对象.重点研究并实现了MiniGUI在嵌入式Linux上的移植以及Thttpd的GUI控制界面的实现方法及过程,最终在MagicARM2410开发板上成功实现了Thttpd的GUI控制界面.通过GUI界面能够实现对Thttpd的启动、停止、重新启动的功能,实现了GUI控制界面的用户登录限制而且允许用户在登录后更改用户密码. 相似文献
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ZHANG Wenqiang SUN Xiaoxia FAN Dejiang LIU Ming JIA Qi YANG Zuosheng 《中国海洋大学学报(英文版)》2020,19(1):60-68
We used the X-ray diffraction method to determine systematically the mineral phases in bulk sediment samples and acid undissolved residuals of the fine-grained fraction of the surface sediments from the 49.6°E hydrothermal field at the Southwest Indian Ridge(SWIR)and discussed the mineral sources of the surface sediments.The results showed that the surface sediments in this region were composed of calcareous ooze,and calcite was the dominant mineral.The sediments also contained quartz,feldspar,clay minerals,pyroxene,sphalerite,barite,serpentine,and magnetite.The quartz,feldspar,and clay minerals were exogenous minerals that mainly originated from the Namib and Kalahari deserts in southern Africa.The pyroxene,serpentine,magnetite,sphalerite,calcite,and barite were endogenous minerals from weathering of seafloor basement rocks and seafloor hydrothermal activities.The sulfide particles in the sediments were mainly deposited from upwelling plumes. 相似文献
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Geochemical characteristics of stable isotopes from hydrothermal chimneys in the Mariana Trough, West Pacific Ocean 总被引：1，自引：0，他引：1
ＩＮＴＲＯＤＵＣＴＩＯＮＲｅｓｅａｒｃｈｅｓｏｎｓｅａ ｆｌｏｏｒｈｙｄｒｏｔｈｅｒｍａｌａｃｔｉｖｉｔｉｅｓａｎｄｈｙｄｒｏｔｈｅｒｍａｌｓｕｌｆｉｄｅｓｙｉｅｌｄｅｄｔｈｅｎｅｗｅｓｔｋｎｏｗｌｅｄｇｅａｂｏｕｔｍｏｄｅｒｎｍａｒｉｎｅｇｅｏｌｏｇｉｃａｌｅｖｏｌｕｔｉｏｎａｎｄｍｉｎｅｒａｌｉｚａｔｉｏｎｐａｔｔｅｒｎｓ.Ｓｉｎｃｅｔｈｅ 1 980ｓ,ｓｃｉｅｎｔｉｓｔｓｈａｖｅｂｅｅｎａｐｐｌｙｉｎｇｔｈｅｏｘｙｇｅｎｉｓｏｔｏｐｅｍｅｔｈｏｄｔｏｒｅｃｏｖｅｒｔｈｅｎｏｔｄｉｒｅｃｔｌｙｄｅ… 相似文献
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地幔橄榄岩中橄榄石的指示意义 总被引：3，自引：0，他引：3
橄榄石是地幔橄榄岩和辉石岩的主要组成矿物,但也经常以斑晶和捕虏晶的形式出现在玄武质岩石中。结合近年来在地幔橄榄岩的主要元素(如Mg和Fe)组成特征以及Li、Mg和Fe稳定同位素地球化学方面的研究成果,重点对橄榄石的地球化学特征与华北克拉通岩石圈地幔演化过程之间的联系进行了讨论,旨在加深对华北克拉通岩石圈地幔演化过程的理解。现有研究表明:地幔橄榄岩中橄榄石的矿物学特征、元素和同位素地球化学组成能够很好地指示岩石圈地幔的特征及其演化过程,因而具有重要的意义。对于克拉通地区的地幔橄榄岩来说,橄榄石的Mg#通常可以指示岩石圈地幔的属性,古老、难熔的地幔橄榄岩中的橄榄石一般具有较高的Mg#(>92),而新生的岩石圈地幔橄榄岩中的橄榄石则具有较低的Mg#(<91)。因此,地幔橄榄岩中橄榄石的Mg#在一定程度上具有年龄意义。橄榄岩中橄榄石的Li、Mg和Fe同位素组成也可以明确指示岩石圈地幔的属性及其所经历的演化过程,正常地幔的δ7Li、δ26Mg和δ57Fe组成相对均一,如果上述同位素组成偏离正常地幔值,则说明岩石圈地幔经历了熔体/流体的交代作用。华北克拉通地区地幔橄榄岩捕虏体中橄榄石的Li、Mg和Fe同位素组成研究表明:该区的岩石圈地幔经历了多个阶段、不同来源的熔体/流体的改造过程。 相似文献
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Microbial diversity in the abyssal sediments beneath the seafloor of 30, 94, and 151 cm near the southern end of the Mariana Trench was analyzed in the Illumina HiSeq 2500 platform. Results show that the microbial populations were dominated by bacteria but merely no archaea were identified at the three depths. In the bacterial community,Proteobacteria and Firmicutes dominated the total taxon tags, followed by Bacteroidetes, Actinobacteria, Planctomycetes, Cyanobacteria, and Chloroflexi, which together account for over 99% of the total population. Similar to that in the seawater in the trench, the operational taxonomic units(OTUs) belonging to Gammaproteobacteria from the sediment samples showed high abundance.However, common bacterial OTUs in the water of the trench including Nitrospirae and Marinimicrobia were hardly found in the sediments from the southern Mariana Trench or the hadal region. Therefore, this study documented for the first time the compositions of microbial diversity in the trench sediments, revealed the difference in microbial diversity in water and sediment of the trench and will enrich the knowledge on the microbial diversity in the abyssal areas. 相似文献
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南任铁矿床位于莱州-安丘铁成矿带西北部,对其矿床成因认识存在较多争议。矿区内地层广布,构造、岩浆岩不发育。铁矿体呈透镜状产于滹沱纪粉子山群小宋组的底部层位,无穿插或交代围岩现象;围岩蚀变以蛇纹石化、绿泥石化为主,愈近矿体矿化蚀变愈强。矿石矿物以磁铁矿为主,少量黄铁矿、黄铜矿;脉石矿物主要为蛇纹石、绿泥石。矿石的结构构造主要为浸染状构造,半自形—他形粒状结构。岩矿石稀土元素含量表明磁铁矿主要为火山深成岩浆结晶分异形成,部分与火山沉积作用有关;磁铁矿化学成分特征也反映了这一点,综合认为其成因可能属海相火山岩型之火山岩浆-热液和火山沉积复合类型。在此基础上,总结了莱州-安丘铁成矿带上不同成因铁矿床的分布规律,为今后该地区铁矿勘查指明了方向。 相似文献
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Jinqing Liu Ke Cao Ping Yin Fei Gao Xiaoying Chen Yong Zhang Yiyong Yu 《中国海洋大学学报(英文版)》2018,17(6):1352-1360
Clay mineral compositions of 199 offshore surface sediment samples collected from the Hangzhou Bay have been analyzed. The clay minerals in the sediments from the Hangzhou Bay are dominated by illite(58.7%, on average), followed by chlorite(20.3%), kaolinite(16.9%) and smectite(4.1%). Two provinces were classified by Q-mode cluster analysis. Class Ⅰ with relatively low amounts of illite and smectite is widely distributed in the Hangzhou Bay, especially concentrated in the top and mouth of the bay, and the northern and southern nearshore areas. Class Ⅱ with comparatively high amounts of illite and smectite is mainly concentrated in the central part of the bay with the water depth of 8–10 m. By comparing clay mineral compositions with the neighbouring regions, we can find that the sediments in the Hangzhou Bay are mainly influenced by the resuspension and repeated deposition of particles from the Yangtze River due to the strong dynamic environment. In particular, the clay fraction of Class Ⅰ is mainly supplied by the Yangtze River, while the sediments of Class Ⅱ are mixture of the clay minerals carried by the Yangtze River and Qiantang River. In general, the distributions of clay minerals in the northern bay are affected by Yangtze River runoff, coastal current and flood tide together, and in the southern they are mainly affected by the Qiantang River runoff and ebb tide. 相似文献
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根据1:5万水系沉积物地球化学测量工作成果,对采集的3138件样品中Cu,Pb,Zn,Au,Ag,W,Sn,Mo,Bi,As,Sb,Cr,Co,Ni共14种元素进行分析测试。研究结果表明,Au,Ag,Cu,Ni是区内最有找矿潜力的成矿指标元素;聚类分析所划分的4类元素簇群,主要与中低温成矿元素、阿尔金南缘断裂、蛇绿混杂岩相关,通过因子分析得到Ni-Cr-As-Sb-Cu-Bi,W-Bi-As-Cu,Bi-W,As,Ag-Zn-Pb,Cu-Bi-As共6类元素组合。其中Cr,Ni,Sb,Cu,As,Bi组合反映出与低温热液活动和断裂构造活动有关;Cr,Ni元素的富集主要与研究区内叶桑岗蛇绿混杂岩带关系密切;Ag,Pb,Zn组合则与地层低温热液元素局部富集和断裂构造活动密切相关。在综合异常分析和查证的基础上,结合区域成矿地质条件、区内矿产地质特征,圈定、划分出2个找矿远景区,并指出了研究区内以金、铜、银、镍为主要优势矿种,铅、锌为潜力矿种。 相似文献
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胶莱盆地南缘沿五莲青岛深大断裂及其次级断裂,目前已发现大量的金铅锌多金属矿床（点）,除典型的隐爆角砾岩型五莲七宝山金铜矿外,其余各矿床沿断裂发育,以石英脉型矿化为主,均显示热液矿床特征。高家宅科地区已发现的金铅锌多金属矿点,分布在以高岭断裂为主的NNW—近SN向断裂中,但基于成矿规律及成矿作用等认识的不足,该地区找矿工作进展缓慢。本次研究通过短波红外光谱测量,在该地区识别出以伊利石、白云母、绿泥石、高岭石、蒙脱石和菱铁矿为主的蚀变矿物,以面积性绢云母蚀变为主（伊利石+白云母）。绢云母矿物高IC值和低Pos2200吸收峰值分布区域均与区内NNW—近SN向断裂和绢英岩化蚀变带具良好的相关性。结合已有成矿事实,认为区内以高岭断裂为主的NNW—近SN向断裂更靠近热液中心,同时,绢英岩化蚀变带中异常的高IC值和极低的Pos2200吸收峰值分布区域,同样具成矿的可能性。 相似文献