Towards automation of palynology 2: the use of texture measures and neural network analysis for automated identification of optical images of pollen grains     

P. LI  W. J. Treloar  J. R. Flenley  L. Empson 《第四纪科学杂志》2004,19(8):755-762

The automation of palynology (the identification and counting of pollen grains and spores) will be a small step for image recognition, but a giant stride for palynology. Here we show the first successful automated identification, with 100% accuracy, of a realistic number of taxa. The technique used involves a neural network classifier applied to surface texture data from light microscope images. A further significance of the technique is that it could be adapted for the identification of a wide range of biological objects, both microscopic and macroscopic. Copyright © 2004 John Wiley & Sons, Ltd.  相似文献   

掌鳞刺属演化及晚泥盆世环境变迁     

王超勇  夏文臣 《南方国土资源》2002,15(2):21-25

牙形石掌鳞刺属Palmatolepis齿台结构和形态随时间演替 ,由近正三角形向长三角形、长菱形演化 ,在F/F界线附近受地质事件的影响而中断 ,使Palmatolepis齿台结构呈二段式发展 ,在Palmatolepis的分子中 ,那些演化速度快 ,结构变化大的分子首先灭绝 ,而那些演化速度慢 ,结构变化小的分子延续时间长 ,分布范围也更加广泛 ,在地质事件中被保留下来并得以延续 ,这种演化规律可能是生物有选择性灭绝与复苏的原因之一。晚泥盆世F/F之交环境的变化可能是由于海退 ,海底毒气喷发 ,超量金属元素的污染造成的  相似文献   

翡翠的结构特征及其对翡翠质量的影响   总被引：2，自引：0，他引：2  

谢星  王崇礼  梁婷 《地球科学与环境学报》2005,27(3):15-18

通过对市面上常见翡翠结构的研究表明．翡翠的结构类型主要为：变晶结构、交代结构和碎裂结构，其中以粒柱状变晶结构最具代表性。不同结构的翡翠质量具有一定差异：变晶结构中以显微纤状变晶结构为最佳．具此结构的翡翠可达半透明至全透明；具交代结构的翡翠中常因含有钠质闪石、钠长石或绿泥石，且使翡翠的粒度不均匀而使其质量变差；具碎裂结构的翡翠硬度将略有降低．因而也会影响翡翠的质量。  相似文献   

一种新的基于Wold分解的纹理分析方法     

王淑晴  臧晓兵  关泽群 《测绘工程》2006,15(1):20-23

针对纹理图像具有结构性和随机性的特点,提出一种新的统一的纹理描述方法。该方法基于Wold分解,在图像为均匀同质随机场的条件下,将纹理图像分解为结构性成份和随机性成份,用少量参数对纹理特征进行描述,为纹理图像的分割、检索、压缩提供了一个统一的纹理模型。  相似文献   

结构光系统结合数码相机的小物体高质量纹理重建   总被引：1，自引：0，他引：1  

郑顺义  周漾 《武汉大学学报(信息科学版)》2012,37(5):529-533,633

针对双鸟饕餮纹夔神鼍鼓等小文物或其他小型物体,提出了基于结构光扫描系统结合普通高分辨率单反数码相机的纹理重建方法。该方法具有自动化程度高、效率和质量高的特点,其中主要解决了单张高分辨率影像与物体几何模型的自动配准,以及配准后从多张影像生成无缝纹理模型的问题。实验证明了本文方法的可行性和有效性。  相似文献   

城市3维模型构建方法研究与实现     

李军锋  胡蕊娟  张春奎  滕大强 《测绘与空间地理信息》2012,35(9):77-79,82

3维模型的构建是城市3维地理信息系统建设的核心。介绍了基于现有数据资料制作城市3维模型的工艺流程,重点研究了利用城市大比例尺3维DLG数据批量获取建筑物高度的新方法和贴图制作过程。按照上述制作工艺和方法较好地解决了大面积城市3维建模这一问题,生成的模型具有很高的精度,完全满足城市3维建模的精度要求。  相似文献   

下垫面对WRF模式模拟黑河流域区域气候精度影响研究   总被引：7，自引：0，他引：7  

潘小多  李新  冉有华  刘超 《高原气象》2012,31(3):657-667

利用高精度的土地覆盖、土壤质地类型和地形高度值替换了天气研究和预报模式Weather Research and Forecasting Model(WRF)中的相关数据,通过数值模式试验检验了下垫面数据对WRF模拟精度的影响。同时,通过与黑河综合遥感联合试验中7个测站观测数据的比较,以平均误差、均方根误差和相关系数为指标,分析了WRF模式下垫面数据改变对近地表气象要素的模拟精度的影响。结果表明:(1)WRF模式本身的地形高度信息在黑河流域上游地区有较大误差,造成了一定的模拟误差。而使用高精度的下垫面数据可以提高WRF模式在黑河流域上游复杂区域的模拟能力;(2)2m气温除了随地形高度递减外,还受土壤质地和土地覆盖小幅度影响,而且进行地形订正后的2m气温与2m湿度的模拟在下垫面为水体的区域对比强烈,因此为模式提供准确的水体分布信息也至关重要;(3)2m气温和湿度等要素的模拟差异值与地形高度资料的差异呈负相关,而降雨量的差异与地形高度差异呈微弱的正相关,与土壤质地差异和土地覆盖差异的相关性也比较弱。  相似文献   

Metamorphic reactions in dry and aluminous granulites: a Perple_X <Emphasis Type="Italic">P–T</Emphasis> pseudosection analysis of the influence of effective reaction volume     

P. Nasipuri  A. Bhattacharya  S. Das 《Contributions to Mineralogy and Petrology》2009,157(3):301-311

In high-Mg, Al metapelites, monophase sapphirine corona occur around spinel–corundum aggregates in monomineralic cordierite layers, and bi-phase orthopyroxene–sillimanite aggregates replace locally warped sapphirine in polygonized cordierite aggregates. P–T phase topologies computed (Perple_X software) using compositions of cordierite-rich layers that host the reaction textures did not match the assemblages for the discontinuous reactions spinel + corundum + cordierite → sapphirine and sapphirine + cordierite → orthopyroxene + sillimanite. Instead, the reaction assemblages were reproduced using P–T pseudosection analysis for micro-domain reaction volumes estimated from compositions of product phases in the volume proportion they occur. The results are consistent with known phase relations deduced using Schreinmakers P–T grids. Apparently, the compositions of cordierite-rich layers that hosted the reaction textures were inadequate chemical proxies for determining P–T–X relations of phase-boundary controlled reactions influenced by compositions of the nearest-neighbor minerals in the proportion they react (effective composition), and not in the proportion they existed in the layer/bulk rock. In other words, P–T–X phase topologies and reconstructed P–T paths in dry and aluminous rocks may be best understood by thermodynamic modeling of reactions using effective reaction volume compositions rather than the bulk composition of the rock or the mineralogical layer that host the reaction textures.  相似文献   

Experimental modelling of corona textures   总被引：1，自引：0，他引：1  

T. L. LARIKOVA  G. P. ZARAISKY 《Journal of Metamorphic Geology》2009,27(2):139-151

Formation of corona textures along olivine–plagioclase and orthopyroxene–plagioclase interfaces has been experimentally reproduced at 670 and 700 °C and 5 kbar with either a pure H₂O fluid phase or 0.1 and 37 m NaCl–H₂O solution fluid. In these experiments, we investigate the interaction of primary olivine and/or orthopyroxene and plagioclase in powders and polished crystals, and in small samples of a natural gabbro. The experiments result in the formation of corona textures with several layers of different assemblages (according to the experimental conditions) consisting of garnet (grossular), clinopyroxene, orthopyroxene, amphibole, chlorite and phlogopite. The experiments show major differences in the number of layers, the mineral assemblages and mineral composition, and in the trends of composition of plagioclase in coronas around olivine and orthopyroxene. The fluid phase composition influences the corona assemblages and the composition of the minerals in the experimental coronas; for example, garnet appears in the coronas in the second experiment where the NaCl–H₂O ratio is low. Experimental modelling of corona textures confirms a model of simultaneous growth of layers by the mechanism of diffusion metasomatism with participation of a fluid phase through which mass is transferred. Zoning in the experimental coronas shows opposing diffusion of Al and Ca from plagioclase and Mg and Fe from olivine/orthopyroxene; difference in the mobility of the components is inferred from observations in the coronas. The experimental corona textures are compared with natural coronas from the Belomorian belt (Baltic shield), developed at 670–690 °C and 7–8 kbar, and the Marun‐Keu complex (Polar Urals), developed at 670–700 °C and 14–16 kbar, where the corona textures correspond to a transitional stage of the gabbro‐to‐eclogite transformation.  相似文献   

Spinifex-like textured metaperidotites from the Higo Metamorphic Rocks,Japan, a possible high-pressure dehydration product of antigorite serpentinite     

Tadao Nishiyama  Hibiki Eguchi  Dai Shiosaki  Akira Yoshiasa  Nobutatsu Mochizuki  Yasushi Mori  Kazumasa Sugiyama  Hiroshi Arima  Kunio Yubuta 《Island Arc》2021,30(1):e12382

Spinifex-like textured metaperidotites from the Higo Metamorphic Rocks (HMR), west-central Kyushu, Japan, may be formed by high-pressure dehydration of antigorite, and may indicate deep subduction of serpentinite reaching a pressure–temperature condition of 1.6 GPa and 740–750 °C. Three rock types have been identified based on mineral assemblage and rock texture: Type I (L) consisting of medium-grained (1–5 cm long) olivine + enstatite + chromite ±tremolite with secondary talc and anthophyllite that occurs in low-grade metamorphic rocks of the biotite zone, Type I (H) of coarse-grained (up to 10 cm long) olivine + enstatite (with clinoenstatite lamella) + chromite ±tremolite with secondary talc that occurs in high-grade metamorphic rocks of the garnet-cordierite zone, and Type II composed of Al-spinel + chlorite + olivine + apatite + ilmenite with minor sodic gedrite in the garnet-cordierite zone together with Type I (H). Olivines in all rock types are mostly serpentinized during exhumation. The chromite-olivine thermometer gives 560–690 °C for Type I (L) rocks, and the spinel-olivine thermometer gives 610–740 °C for Type II rocks. The peak metamorphic pressure will be higher than 1.6 GPa based on the location of the experimentally determined invariant point (P = 1.6 GPa and T = 670 °C) of antigorite + forsterite + enstatite + talc + H₂O. This estimate is consistent with the occurrence of chlorite in Type II rocks, which is stable up to 890 °C at 2.0 GPa. The spinifex-like textured metaperidotites occur as small bodies in the low P/T type gneisses, implying tectonic juxtaposition of them probably during exhumation of the HMR. Recent findings of medium pressure (0.9–1.2 GPa) granulites and gneisses from the HMR may indicate that the HMR has a deep root into the wedge mantle from which the spinifex-like textured metaperidotites have derived.  相似文献