天然、优化、处理翡翠玉件常规仪器鉴别(一)     

苏文宁 《云南地质》2003,22(3):229-249

多年系统研究和大量样品检测证明：正确鉴别天然(A)、优化(B)翡翠玉件，比重、荧光是指示，结构是基础，识别充填物是关键，拉曼、红外作验证，综合分析下结论。而在常规仪器检测过程中，特别抓住结构(基础)、充填物(关键)，即：用岩矿显微镜细致观察翡翠玉件结构，辅以针探和微区组分鉴别法区分各种充填物，结合比重、荧光检测结果，可以准确、快捷、经济地鉴别翡翠玉件A货、B货，而不需使用红外、拉曼。借助色源类型鉴别可正确鉴别处理翡翠玉件(C货)。  相似文献   

Crust-Mantle Interaction in Dabie Orogenic Belt, Central China： Geochemical Evidence from Late Cretaceous Basalts     

匡少平  张本仁 《中国地球化学学报》2003,22(3):231-243

It has been suggested that eclogites in the Dabie orogenic belt are exhumation prod-ucts, which had subducted into the deep-seated mantle and undergone ultra-high pressure meta-morphism during the Triassic. But no direct evidence supports this process except the calculated p-T conditions from mineral thermobarometem. The Late Cretaceous basalts studied in the pres-ent paper, however, have provided some geochemical evidence for crust-mantle interaction in the area. These basalts are distributed in Mesozoic faulted basins in central and southern Dabieorogenic belt. Since little obvious contamination from continental crust and differentiation-crys-tallization were observed, it is suggested, based on a study of trace elements, that the basaltsare alkaline and resultant from batch partial melting of the regional mantle rocks, and share thesame or similar geochemical features with respect to their magma source. In the spider diagram normalized by the primitive mantle, trace element geochemistry data show that their mantle sources are enriched in certain elements concentrated in the continental crust, such as Pb, K,Rb and Ba, and slightly depleted in some HFSE such as Hf, P and Nb. Pb-Sr-Nd isotopic com-positions further suggest the mantle is the mixture of depleted mantle (DM) and enriched one(EMI EMII). This interaction can .explain the trace element characteristics of basaltic mag-mas, i.e.,the enrichment of Pb and the depletion of Hf, P and Nb in basalts can be interpre-ted by the blending of the eclogites in DOB (enriched in Pb and depleted in Hf, P and Nd)with the East China depleted mantle (As compared to the primitive mantle, it is neither en-riched in Pb nor depleted in Hf, P and Nb). It is also indicated that the eclogites in the Dahieorogenic belt were surely derived from the exhumation materials, which had delaminated into thedeep-seated mantle. Moreover, the process subsequently resulted in compositional variation of the mantle (especially in trace elements and isotopes) , as revealed by the late mantle-derivedbasalts in the Dabie orogenic belt.  相似文献   

地震活动的三维动画演示系统     

肖立萍 《地震地磁观测与研究》2004,(Z1)

详细介绍了辽宁数字遥测地震台网利用C语言、3DSMAX软件开发的地震活动的三维动画演示系统。  相似文献   

丘陵红壤区决明属牧草品系的适应性筛选   总被引：12，自引：0，他引：12  

黄毅斌  应朝阳  黄金煌  庄绍东  翁伯奇 《山地学报》2004,22(6):742-749

针对占全国总面积22％的南方红壤区有机质含量低、酸性强、水土流失严重等生态问题，及福建省当家豆科草种少等问题。引进40个豆科决明属(Chamaecrista spp．)牧草，在福建省不同气候带的红壤山地进行多年适应性筛选和验证试验。通过聚类分析和建立综合指标评价体系，筛选出适宜荒山荒坡地种植的直立型品种C．nictitans ATF2217、ATF2219，适宜于果园套种的匍匐型品种C．rotundifolia CPI34721、CPI92985和适宜保持水土改良土壤的C．rotundifolia CPI86134、CPI86178等6个品系进行推广利用。其中Chamaecrista nictitans cv．ATF2217已通过全国牧草品种审定，定名为“闽引羽叶决明”。  相似文献   

Charles D. Walcott in England and Wales (1888): A crucial visit in the resolution of Taconic-Cambrian-Ordovician questions     

Michael G. Bassett 《Proceedings of the Geologists' Association. Geologists' Association》2004,115(1):63-75

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Late Holocene climatic changes in Tierra del Fuego based on multiproxy analyses of peat deposits     

Dmitri Mauquoy  Maarten Blaauw  Ana Borromei  Frank M. Chambers 《Quaternary Research》2004,61(2):148-158

A ca. 1400-yr record from a raised bog in Isla Grande, Tierra del Fuego, Argentina, registers climate fluctuations, including a Medieval Warm Period, although evidence for the ‘Little Ice Age’ is less clear. Changes in temperature and/or precipitation were inferred from plant macrofossils, pollen, fungal spores, testate amebae, and peat humification. The chronology was established using a ¹⁴C wiggle-matching technique that provides improved age control for at least part of the record compared to other sites. These new data are presented and compared with other lines of evidence from the Southern and Northern Hemispheres. A period of low local water tables occurred in the bog between A.D. 960-1020, which may correspond to the Medieval Warm Period date range of A.D. 950-1045 generated from Northern Hemisphere tree-ring data. A period of cooler and/or wetter conditions was detected between ca. A.D. 1030 and 1100 and a later period of cooler/wetter conditions estimated at ca. cal A.D. 1800-1930, which may correspond to a cooling episode inferred from Law Dome, Antarctica.  相似文献   

Phytolith evidence for C4-dominated grassland since the early Holocene at Long Pocket, northeast Queensland, Australia   总被引：1，自引：0，他引：1  

Vanessa C. Thorn 《Quaternary Research》2004,61(2):168-180

Preliminary phytolith analysis of ephemeral lake fill sediment at Long Pocket, near Toomba, northeast Queensland, Australia, indicates that a C4-dominated grassland with a minor woody component has been present in the region since ca. 8000 cal yr B.P. Based on the modern distribution of C4 and C3 native grasses in Australia, this suggests that mean summer temperatures of at least 14°C (ca. 10°C cooler than present) were maintained since the early Holocene. This interpretation is comparable with previous studies, which together imply that the establishment of C4-dominated grasses in central and northeast Australia occurred between the last glacial maximum (most likely after ca. 16,000 ¹⁴C yr B.P.) and ca. 7200 ¹⁴C yr B.P. (ca. 8000 cal yr B.P.). Taxonomic composition of the grassland appears relatively consistent since the early Holocene at Long Pocket and includes phytoliths comparable with those from modern Arundinoideae, Panicoideae, and Chloridoideae. Rare non-grass phytoliths are also present. A gradual decrease in abundance of saddle phytolith forms (attributed to Chloridoideae grasses) from the base of the record at ca. 6500-7000 cal yr B.P. suggests decreasing aridity throughout the Holocene. This trend could reflect a locally drawn out effect of the end of the postglacial arid period due to the well-drained basalt flow catchment maintaining a local arid habitat for the Chloridoideae grasses.  相似文献   

卫星导航定位系统中伪随机码的研究   总被引：6，自引：0，他引：6  

卢晓春  陈清刚  胡永辉 《时间频率学报》2004,27(1):23-32

伪随机码在扩频通信中得到广泛应用。目前的卫星导航定位系统大多采用扩频通信技术来传输导航信息 ,常用的伪随机码是平衡Gold码。对平衡Gold码的特性和产生方法作了研究 ,对全球定位系统 (GPS)粗码的平衡性作了分析 ,最后给出了在SystemView平台上相应的仿真结果。此研究对开展相关领域的研究工作具有借鉴意义  相似文献   

小井径双源距碳氧比C/O测井的影响因素及处理   总被引：6，自引：1，他引：6       下载免费PDF全文

吴文圣  付赓  张智  庄人遴 《地球物理学报》2005,48(2):459-464

研究各种地层和井眼环境因素对碳氧比C/O测井长、短源距探测器的影响规律，可以为C/O测井仪器的刻度方法提供指导，为解释模型的建立和数据处理提供依据.本文用Monte Carlo方法，计算了C/O值随井眼直径、水泥环厚度、套管直径、孔隙度、含油饱和度、地层岩性和油密度的变化规律.从中看出，当井内流体为油时，井径或套管直径增大，C/O值增大，井眼影响增大；当井内流体为水时，井径或套管直径的增大，C/O值减小；水泥环厚度增加时C/O值减小；当井眼条件不变时，地层孔隙度越大，含油饱和度越大，C/O值越大，对测井越有利；反之，地层孔隙度越小，含油饱和度越小，C/O值越小，对测井不利；地层岩性对C/O值的影响显著，相同条件下，碳酸盐岩比砂岩的C/O值高；油密度越大，C/O值越大.文中还提出了一种消除这些因素影响的数据处理方法  相似文献   

Simulation of ~(14)C in IAP/LASG L30T63 Ocean Model   总被引：2，自引：0，他引：2       下载免费PDF全文

LI Qingquan  SHI Guangyu 《Acta Meteorologica Sinica》2005,19(4):436-446

1. Introduction14C is a radioactive isotope of carbon, whose halftime is about 5730 yr. Under natural circumstance,14C comes into being in the stratosphere because of thenitrogen explosion of cosmic radial. 14C is mixed inthe atmosphere, absorbed by oceans, and then trans-ported into deep ocean. 14C radioactively reduces asits age increases. The reduction process of 14C canuncover the evolvement process of sea water's age andrenewal time.14 C content is usually described with one in athousan…  相似文献