综合LDA与特征维度的丽江古城意象感知分析

论文通过建立基于LDA(Latent Dirichlet Allocation)模型和包含两级特征维度的旅游地意象感知研究框架,将LDA主题模型用于旅游微博文本分析,以特征维度半定量刻画旅游地意象感知特征,减少LDA主题凝练的主观性,帮助研究者在特定维度框架约束下准确、客观地提取旅游地意象特征。丽江古城案例证明,一级特征维度可以完整勾勒出丽江古城意象感知的基本框架,包括以聚落形态、音乐意境、标志人物、休闲空间和纳西美食为核心的5组空间与景观元素,深度旅游者、城市居民、年轻人、女孩子4类人群的特殊感知体验,及旅游者与环境要素的不同互动特征;二级特征维度进一步精细解读丽江古城的意象感知特征,表现为丽江古城慢活性、夜生活和浪漫之都的文化意象、旅游者对地方文化与现代风情融合的凝视与体验等。结合特征维度的LDA模型,准确构建了意象基本框架,成功刻画了丽江古城的形象及精细特征,并能进一步解析意象的形成机制,为旅游地意象感知研究提供了新视角,有助于深度解读意象形成的地方意义,厘清认知、情感和行为意象间的关系。     

浙江萧山岩山明矾石矿床成矿特征及其成矿演化探讨

笔者对产于元古界双溪坞群古岛弧火山沉积岩系中的岩山明矾石矿床，经矿床地质、成矿作用与成矿时代、构造与成矿演化等方面的分析研究，认为岩山明矾石矿床系元古代古岛弧火山喷发沉积热液交代成矿。     

闽南沿海前湖剖面及其第四纪地质若干问题

前湖剖面第四系出露比较完整，层次清晰，发育有炭质层、铁盘、重矿砂砾石层、“老红砂”层和玄武岩等特殊地层，是一个研究闽南沿海第四纪地质问题的比较有代表性的地表露头剖面。本文通过对前湖剖面中系列样品进行测年、微古、孢粉、矿物、粒度等综合分析研究，探讨了闽南沿海晚更新世晚期以来的古气候变化、海平面变动、“老红砂”的形成年代及成因以及第四纪地层划分等问题。     

东北地区夕阳产业地域划分及其振兴对策研究

夕阳产业地域(Old Industrial Area)是伴随着工业化而出现的一种地域现象。在参考国内外有关研究的基础上,介绍夕阳产业地域形成的背景及其相关机制;根据夕阳产业地域特征,建立划分夕阳产业地域的指标体系并确定划分方法,将东北地区34个城市经济区进行分类,得出抚顺、本溪、阜新、鸡西、鹤岗、双鸭山、大庆、伊春、七台河、辽源等10个夕阳产业地域;并根据夕阳产业地域形成的根本原因,从主导产业选择和产业结构调整两个方面提出夕阳产业地域振兴的对策。     

论《旧约》传记性特征对《新约》的影响

《旧约》是一部具有鲜明传记特征的文化文本,《新约》在继承《旧约》中耶和华一神教信仰的同时,也继承了《旧约》的传记性特征,在以人系事、人物塑造和历史感等方面表现出相应的传记性。因此,《新约》也是一部具有鲜明传记特征的文化文本。     

The significance of stretching lineations in terms of progressive deformation and finite strain

Abstract

For a given increment of deformation, stretching lineations can be defined either by old grains or by new grains.

Progressive strain accumulated in a matrix causes reorientation of old grains. The velocity field acting within a grain depends on the degree of non-coaxiality of the progressive strain in the matrix, and on the competence contrast between grain and matrix (e.g. Lister & Williams, 1983). Deformed populations of old grains do not systematically track the principal directions of finite stretch; this depends on the mechanical behavior of the grains. On the other hand, these populations may be good markers of finite strain magnitude, provided that the initial distribution is known.

In contrast, the statistical shape orientation distribution of population of new grains cannot be related in a simple way to the finite strain magnitude, but their preferred orientation is considered to be the best indicator of the principal directions of finite stretch.

An example is considered from the schistes lustrés near Kenestrelle (Val Chisone, Western Alps), where the observed mineral lineation is attributed to a late E-W stretching event in the alpine orogenic history.     

East Asian Winter Monsoon record from the environmental sensitive grain size component of QF Old Red Sand, Haitan Island, China

The "Old Red Sand" is widely distributed along the coast of Fujian Province, China. Most studies have been carried out from aspects of the origin, age and laterization of the "Old Red Sand", but this paper focused on reconstructing the history of the Asian Winter Monsoon change. On the basis of granulometric analysis of high-resolution samples, we have obtained environmental sensitive grain size component (ESGSC) from the Qingfeng (QF) profile by using the grain size-standard deviation method, which proves that the selected ESGSC is an important climate proxy. The mean grain size of this ESGSC could be used to reconstruct the East Asian Winter Monsoon (EAWM) intensity. As such, the history of the EAWM change since 44.0 ka reconstructed here reveals three main phases based on chronology dates of previous researches: (1) 44.0-25.5 ka B.P., the EAWM is relatively weak but increases gradually with fluctuations; (2) 25.5-15.5 ka B.P., relatively strong with high frequency fluctuations; (3) 15.5-7.1 ka B.P., with a weaker winter monsoon, but during 11-10 ka B.P. is remarkably enhanced. The EAWM recorded by mean grain size of the two neighboring sections have a better repeatability, so the millennial scales oscillation should be a reliable signal of the EAWM intensity. The climate recorded by ESGSC of the QF "Old Red Sand" compared to δ 18 O of Hulu Cave stalagmites and Greenland GISP2 ice cores shows a good consistency, especially in detail, the YD event and four Heinrich events are all recorded, but the signal of D-O cycles was relatively weak.     

福建东部海坛岛老红砂敏感粒度组分对东亚冬季风演变的响应

本文在福建东部海坛岛青峰老红砂剖面年代学框架基础上,通过2.5 cm等间距高密度采样进行粒度分析,采用粒级-标准偏差方法提取敏感粒度组分,并证明敏感粒度组分平均粒径可作为东亚季风的强弱变化的替代指标,据此建立了约44.0 ka以来青峰剖面老红砂记录的冬季风演变序列。结果显示,约44.0 ka以来东亚冬季风经历了3个演变阶段：①44.0~25.5 ka BP东亚冬季风较弱, 呈现在波动中逐步增强趋势;②25.5~15.5 ka BP为东亚冬季风最强盛期,并呈现高频波动特点,东亚冬季风在21.8 ka BP前后达到鼎盛期;③15.5~7.1ka BP为冬季风减弱期,但在11~10 ka BP前后,冬季风突然显著增强。相邻剖面平均粒径记录的冬季风演变阶段也具有较好的重复性。对比发现,青峰剖面老红砂敏感粒度组分的气候记录与长江下游葫芦洞石笋δ18O和格陵兰GISP2冰芯δ18O记录之间有较好的吻合,尤其对新仙女木事件和4次H事件三者都有记录,但青峰剖面对D-O旋回记录信号不明显。     

Ambient noise H/V spectral ratio in site effects estimation in Fateh jang area,Pakistan

Local geology or local site effect is a crucial component while conducting seismic risk assessment studies. Investigations made by utilization of ambient noise are an effective tool for local site estimation. The present study is conducted to perform site response analysis at 13 different sites within urban settlements of Fateh jang area(Pakistan). The aim of this study was achieved by utilizing Nakamura method or H/V spectral ratio method. Some important local site parameters, e.g., the fundamental frequencies f0 of soft sediments, amplitudes A0 of corresponding H/V spectral ratios, and alluvium thicknesses over 13 sites within the study area, were measured and analyzed. The results show that the study area reflects low fundamental frequency f0. The fundamental frequencies of the sediments are highly variable and lie in a range of 0.6–13.0 Hz. Similarly, amplification factors at these sites are in the range of 2.0–4.0.