瓷器热释光高温峰测年的初步研究

对陕西耀州窑4个古瓷器碎片的热释光高温峰测量的结果表明,瓷器样品具有天然热释光信号,而且,其信号增长呈良好的线性,高温峰可以用于瓷器的年龄测定和真假鉴定之中,瓷器热释光高温峰技术有望成为热释光测定瓷器年龄的一个方法。     

城市土地利用结构的熵值定律

根据对郑州、广州等城市的土地结构分析,总结出关于城市土地利用的信息熵值规律:大城市用地结构的信息熵一般大于小城市的信息熵,综合性城市的信息熵严格大于专业化城市的信息熵,城市化地区的信息熵必须大于各功能区的信息熵。基于信息熵值规律,提出了关于城市空间形态的分维包容原理:城市化地区土地形态的分形维数必须大于各类型土地空间分布的分形维数。     

体验经济时代下旅游项目设计与实证研究

体验性旅游项目设计包括纵向深度设计和横向整合设计。旅游项目纵向设计是深度挖掘单项旅游资源(或吸引物)潜力,实现单项旅游项目经济价值最大化。并就感官指数,时间指数,复杂指数,环节指数,互动指数,交叉指数,遗憾指数,惯性指数8个因子和23个指标提出其定量评价指标体系。旅游项目横向设计,即旅游线路设计,是在纵向设计基础上,对旅游项目在空间上、类型上进行全方位横向整合设计。并以贡嘎山海螺沟风景名胜区为例,在纵向与横向两度空间进行旅游项目体验性设计,为景区体验性旅游项目设计提供理论、方法和范例。     

LUTI模型原理、实现及应用综述

经济全球化背景下可持续发展已成为当今世界发展的主题。快速城镇化下的中国,城市空间的可持续性发展提上日程。为此,期待有力的、可操作的工具用于定量模拟城市空间演化过程、预测不同政策下城市空间的发展趋势,为城市化持续健康发展提供决策支持。本文分析了LUTI模型的基本原理、构建思路、实现框架和建立中国城市LUTI模型面临的问题,并回顾了国内外利用LUTI模型模拟城市空间演化过程,以辅助表明城市空间决策的研究现状,希望能为中国的城市空间可持续发展模拟分析研究提供参考。     

说"国必依山川"

古人认为山为神灵傧居之所,川则通达于山之涂,大邑国都是承天命之处,而天子则以事神祭祀恪谨天命为主任,为本职,“国必依山川”说的正是大邑国都依山傍水,以便于君主上通于神明,以神道政教天下。学者们以经济原因解之,以今度古之论也。     

《周易·大畜》考释

《周易·大畜》向来被解为“大为畜聚” ,这是非常浅显的。本文从文字、易象、易理等方面考释论证 ,认为有三层涵义 :一、指大人死后神灵畜居于山中 ;二、记载的是大人前往山中祭祀先王的过程 ;三、指大人必须顺承先王之德、之道 ,自畜人君之德。     

“清江四案”“白银案”之前后

锦屏本地苗族木商向政府状告外省木商使用冲铅银两假币的诉讼案件。收集到的两件状词,一是道光七年（1827）由李荣魁带头起诉到贵州布政使司批转黎平府的公文,又由黎平府作出处理公告;另件是光绪十三年（1887）姜名卿等向黎平府递交的状纸。两起案件相隔60年,因为假银泛滥、受害深重后才产生诉讼,政府行文禁止后,仍禁而不止,所以少数民族的木商、林农和从事木材运输的农民工,受假银之害至少在80年以上。但从外省木商之滥用假币,折射出清水江木业之兴旺。     

图书馆开架借阅工作浅议

开架借阅是图书馆工作的发展方向,它使图书馆在服务社会方面发挥了积极的作用,但是开架借阅所带来的诸多问题是图书馆管理工作的一大难题。本文通过对存在问题的分析,提出了一些具体的对策。     

Geospatial modeling of pedestrian transportation networks: a case study from precolumbian Oaxaca,Mexico

Using accumulated cost surfaces and various pathfinding techniques within Geographic Information Systems (GIS) software, archaeologists and other spatial scientists have developed increasingly sophisticated models of human movement. Despite their utility, these approaches can be limited because standard GIS software cannot model movement (1) from many origins to many destinations or (2) without specific origins and destinations. Absent these capabilities, it is particularly difficult to model networks of movement over a given tract of land if you are interested in obtaining a more general sense of movement dynamics, not specific site-to-site patterns. In this paper, we present an innovative way of modeling past movement that generates both natural-looking networks and also indicates the degree of traffic that may have existed on any particular segment of those networks. The “From Everywhere to Everywhere” (FETE) model generates networks based on topography and landcover without requiring that origin and destination points be supplied in advance. We apply the FETE model to a case from the southern Mexican state of Oaxaca, a region that has extensive archaeological and ethnohistoric data sets that serve as a test of the efficacy of our technique. A comparison of the FETE output with known late precolumbian and early colonial movement corridors indicates that the method is effective and should be useful for modeling networks in other areas.     

High‐temperature magmatic fluid exsolved from magma at the Duobuza porphyry copper–gold deposit,Northern Tibet

The Duobuza porphyry copper–gold deposit (proven Cu resources of 2.7 Mt, 0.94% Cu and 13 t gold, 0.21 g t^?1 Au) is located at the northern margin of the Bangong‐Nujiang suture zone separating the Qiangtang and Lhasa Terranes. The major ore‐bearing porphyry consists of granodiorite. The alteration zone extends from silicification and potassic alteration close to the porphyry stock to moderate argillic alteration and propylitization further out. Phyllic alteration is not well developed. Sericite‐quartz veins only occur locally. High‐temperature, high‐salinity fluid inclusions were observed in quartz phenocrysts and various quartz veins. These fluid inclusions are characterized by sylvite dissolution between 180 and 360°C and halite dissolution between 240 and 540°C, followed by homogenization through vapor disappearance between 620 and 960°C. Daughter minerals were identified by SEM as chalcopyrite, halite, sylvite, rutile, K–feldspar, and Fe–Mn‐chloride. They indicate that the fluid is rich in ore‐forming elements and of high oxidation state. The fluid belongs to a complex hydrothermal system containing H₂O – NaCl – KCl ± FeCl₂ ± CaCl₂ ± MnCl₂. With decreasing homogenization temperature, the fluid salinity tends to increase from 34 to 82 wt% NaCl equiv., possibly suggesting a pressure or Cl/H₂O increase in the original magma. No coexisting vapor‐rich fluid inclusions with similar homogenization temperatures were found, so the brines are interpreted to have formed by direct exsolution from magma rather than trough boiling off of a low‐salinity vapor. Estimated minimum pressure of 160 MPa imply approximately 7‐km depth. This indicates that the deposit represents an orthomagmatic end member of the porphyry copper deposit continuum. Two key factors are proposed for the fluid evolution responsible for the large size of the gold‐rich porphyry copper deposit of Duobuza: (i) ore‐forming fluids separated early from the magma, and (ii) the hydrothermal fluid system was of magmatic origin and highly oxidized.