Geology, Geochemistry and Origin of the Hongshan Porphyry-Cryptoexplosive Breccia Type Copper Deposit in Huichang County, Jiangxi Prvince

The Hongshan porphyry-cryptoexplosive breccia type copper deposit occurs in a metamorphic rock series of the Mesoproterozoic Zhongcun Group. Orebodies are distributed inside and outside porphyry-cryptoexplosive breccia pipes. The deposit involves five ore-forming types, i.e the porphyry type, cryptoexplosive breccia type, contact-zone veinlet-disseminated type, in-pipe fracture-zone filling-replacement type and out-of-pipe fracture-zone filling-replacement type, forming an ore-forming system of “five ore-forming types within a single rock body”. Fluid inclusion and isotope geochemical studies indicate the following: S, Pb, O and Sr were derived from the lower crust, Nd was derived from the continental crust or depleted mantle and rare earth elements (REE) and trace elements have the crustal source characters; fluids consist dominantly of formation water, metamorphic water and ***meteoric water with a part of magmatic mater, heat came from porphyry while the latter originated from partial melting caused by shear heating in the lower crust and upper mantle. According to its origin the deposit is classified as the hypabyssal and near-surface, meso- and hypothermal copper deposit associated with the late Yanshanian porphyry-cryptoexplosive breccia.

Methods and Effects of Hongshan Cock Spermatozoa Cryopreservation

The survival rates, acrosomic integrity rates of frozen semen from Hongshan cock and fertilities of the frozen-thawed spermatozoa in both pellets and straws were studied. The result shows that the average survival rate of spermatozoa in straws was 0, 451±0, 056, and 0. 390±0. 040 in pellets, the former was significantly higher than the later （n=20, p〈0, 01）, The average acrosomic integrity rate of the sperms was 0, 613±0. 049 in straws, and 0. 476±0. 057 in pellets. The former was significantly higher than the later （n= 20, p〈0.05）. The fertility rates （%） of sperms in pellets, straws and freshly colleered semen at the third day after artificial insemination （AI） were 85.32±2. 32, 87. 73±1.00 and 90.77±1.68, respectively. The fertility rate,s of the three types of semen at the fourth and fifth days were lower than the third day＇s. Variance analysts shows that the fertilities of the spermatozoa in pellets and straws were significantly lower than freshly collected semen （n=3, p〈0.01）, and the fertilities of the spermatozoa in straws were significantly higher than those in pellets （n= 3, p〈0.01）.

The significance of lake sediments geochemistry in environmental reconstruction of south Hongshan Lake, northwestern Tibetan Plateau during the past 150 years

A 107cm piston-core (SHC-2) was drilled at the site with water depth of 5m in South Hongshan Lake, northwest Tibet in 1998. Based upon the 0.72cm/a of modern sedimentary rate that was tested by 210Pb method and also calibrated by 137Cs method as well as the 1cm interval sample cutting level, a lake sedimentary record of 150-yr old and with a resolution of 1.4 yrs was obtained. Ratio of geochemistry contents (TOC, TN, CaCO3) and concentrations of trace elements such as B, Sr, Ba, Ca, Mg, K, Na, Al, Ti, Cu, Zn, Fe, Mn, Ni, Cr, V, Pb, etc were analyzed. The values of TOC, TN, C/N, CaCO3, Sr/Ba and Fe/Mn had clear environmental significance and well reflected the environmental changes. Geochemical multi-proxies of lacustrine sediments from SHC-2 core showed that the environmental changes in this area during the past 150 years could be reconstructed as follows: Stage 1 (1850s-1880s) was a cold period; Stage 2 (1880s-1920s) was a warm period. But the variation of lake water volume was stable in the two periods. Stage 3 (1920s-1950s) was a fluctuant and transitional period in temperature, but there were a short cold period in the 1920s and a warm period in the 1930s. Stage 4 (1950s-) showed a warming tendency, though there existed a cold period from the mid 1970s to the end of the 1980s. In the view of general trend in the past 150 years, South Hongshan Lake was shrinking gradually. It showed that, from the comparison with the Guliya ice core and meteorological records of adjacent weather stations, there is difference in the variations of temperature and precipitation among different regions and altitudes in Tibetan Plateau. It is necessary to search multi-scale and high-resolution records for environmental reconstruction and comparison.

Study on the origin of the Hongshan brecciated copper deposit in Huichang County, Jiangxi Province, China

The Hongshan copper deposit is a typical cryptoexplosive breccia-type deposit, which occurs in a metamorphic rock series of the Mesoproterozoic Taoxiyuan Formation. Orebodies are distributed inside and outside porphyry-cryptoexplosive breccia pipes. The isotope geochemistry of the deposit is consistent with the origin of porphyry breccia: the δ18OH2O values ranging from 1.2‰ to 6.1‰ and the δ34S values varying from 0 to 2.5‰. 206Pb/204Pb, 207Pb/204Pb and 208Pb/204Pb ratios of pyrite, which coexists with ore minerals, indicate it was derived from the orogenic belt. Thermodynamic analysis indicates that the main metals were deposited largely as a result of the decreasing of proton concentrations associated with H2S and CO2 exsolution during explosion and temperature dropping. Based on K-Ar dating of quartz coexisting with ore minerals, the age of mineralization was estimated to be 97.1–98.8 Ma, which suggests that mineralization occurred between the Early and Late Cretaceous. According to the relevant information obtained, a diagenetic and metallogenic pattern in the area has been presented in this paper.

红山文化的宣传策略研究

红山文化是华夏文明最古老的痕迹之一,红山文化研究在近些年已取得了长足的进展,但红山文化宣传工作的现状却不容乐观。本文以美国学者H·拉斯维尔的5G模式为理论指导,探索了红山文化的宣传策略。

Environmental changes reflected by the lake sediments of the South Hongshan Lake, Northwest Tibet

The 1.07-m long lake core with 1 cm interval cutting, which was obtained by drilling in the South Hongshan Lake of Northwest Tibet, was dated by the 210Pb and 137Cs methods, and a 150-year consecutive lake sedimentary sequence (1840─1997) with 1.4 year resolution was obtained. Some environmental proxies, such as the total organic carbon (TOC), total nitrogen (TN), ratio of TOC to TN (TOC/TN), trace chemistry elements (TCE), CaCO3, grain size, richness of ostracoda etc. showed that they are of well coincidence. These results implied that the environmental background varied from the cold-wet period in the late 19th century, to the warm-wet period from the end of the 19th century to the 1920s and to the warm-dry period since the 1920s. There were sub-variations since the 1920s: the cold-dry/warm-wet fluctuation from 1922 to 1960, the intensively warm-dry period since 1960 with a short cold-wet period in the mid-1970s to the end of the 1980s. The humid period from the mid-1970s to the end of the 1970s and the dry period beginning from the early 1980s were well documented by climatic data of the nearby weather station records while the grain size was well correlated to the annual precipitation. Compared with the records from Guliya ice core in the same area, the TOC proxy in the lake core indicating warm/cold conditions well corresponded to the ( 18O records representing temperature variations in the ice core. However, the proxies with dry/wet significance in the lake core were different from the variations of snow accumulation reflected by the ice core. It can be concluded that the chosen environmental proxies have clear environmental significance and the lake sediments can reflect climatic and environmental changes at high-resolution.

Property and provenance study of fancy celadon samples excavated from the Noble Burials of the Yue State at Hongshan, China

The Noble Burials of the Yue State at Hongshan in Wuxi City with many fancy burial objects were excavated by Archaeology Institute of Jiangsu Province and Xishan District Committee for Administration of Cultural Relics of China. It was appraised as one of the ten major archaeological excavations in 2004. Some precious ceramic samples excavated from this site are very important for studying the development history of Chinese ceramics, especially for studying the origin of porcelain. With the cooperation of Archaeology Institute of Nanjing Museum, the ceramic samples excavated from the Noble Burials of the Yue State at Hongshan were collected and systematically analyzed. Compared with the celadon samples produced in Yue-kiln site during later Eastern Han Dynasty (25–220 A.D.), some important topics such as the provenance and properties of the ceramic samples excavated from the Noble Burials of the Yue State at Hongshan were deeply studied.

农文旅深度融合助力乡村振兴研究——以内蒙古红山区为例

农文旅是依托农业生产,融合自然与农业、当地人文气息以及现代旅游业的一种高效产业,是一种以领略农村田野风光,体验农事生产劳作,了解风土民俗和回归自然为旅游目的的生活方式。随着游客大量参与乡村旅游,消费需求普遍升级,农文旅融合发展不仅是产业升级的需要,更是乡村振兴的有力手段,不断支持和引导“三农”创新发展。以内蒙古红山区为例,分析其农文旅发展现状及薄弱环节,探讨深化红山区农文旅深度融合的路径。

内蒙古巴林右旗地区兴隆洼、红山玉器的材质利用研究

内蒙古巴林右旗地区出土、采集到的兴隆洼、红山玉器较多,但长期以来缺乏针对当地玉器的系统性材质研究。本研究借助拉曼光谱仪和X射线荧光光谱仪等便携式仪器对当地的74件兴隆洼与红山玉器进行无损测试分析,确定了这批玉器的材质主要为闪石玉。根据X射线荧光光谱的峰值记数进行横向对比,这批玉器可被分为3个组别:兴隆洼时期的用材集中于B、C两组,颜色呈浅黄或浅绿色;红山时期玉器用材集中于A、B两组,颜色呈浅绿或深绿色。此外,这批玉器中也包含少量地开石、方解石、蛇纹石、云母、萤石材质。结合地质学相关信息,对玉器的产源地进行分析和探讨,可以推断闪石玉取材于辽宁岫岩地区,而其他材质多为就近取材,亦有部分取材于辽宁岫岩地区。

“中”“阳”视域下“红山医派”《伤寒论》解经与中医临床教育刍议

2023年6月至10月,北京中医药大学“红山医派”《伤寒论》解经研究课题组、北京扶阳国际中医科学研究院持续开展了“红山医派”《伤寒论》解经暨临床教育相关研讨。综合纳入院校与民间中医学者和北京中医药大学研究生、本科生群体,以求在瞄准临床的经典学习、解读中可集“庙堂之上”与“江湖之远”之长。选定《伤寒论》为主要学习研讨对象,以“红山医派”的重“阳”和重“中”的理念,为相对“中规中矩”的院校经典教育及基于教育的临床实践注入“一剂活水”。在传统院校教育基础上,提升了中医学习者在古今语境差异下从相对碎片化的行文论述中把握经典中心思想的能力。文章将“红山医派”《伤寒论》解经与中医临床教育研讨成果进行整理,以求对于临床经典教学有所借鉴及参考。

城市动物园沉浸式展区设计探索--以南京市红山森林动物园亚洲灵长区为例

沉浸式展区是在动物园展区设计发展过程中形成的新型动物展示模式,能够有效提升动物福利及游客观展体验。以南京市红山森林动物园亚洲灵长区为研究案例,从动物生态友好、游客观感体验和园区管理高效3方面入手,深入探讨21世纪现代动物园沉浸式展区设计的方法和策略,以期在有限的空间中更好地展示野生动物的自然行为,提升科普教育、自然教育效果,为动物园沉浸式展区设计提供借鉴。

浅谈博物馆社会教育活动——以红山文化博物馆为例

社会教育是博物馆的一项重要功能。随着人们对精神文明追求的不断提高,博物馆逐渐成为展示地区历史文化,弘扬民族精神的重要课堂。红山文化博物馆是赤峰地区的专题博物馆,是宣传红山文化的重要场所。红山文化博物馆需要通过各种社教活动,让观众感受红山文化的博大精深,从而充分发挥其社会教育功能。

红山文化元素融入中国古典舞创作的可行性探究

本文聚焦红山文化的历史脉络,以《红山玉龙谣》作品为支撑,探讨红山文化元素融入中国古典舞创作的可行性,旨在为古典舞创作提供新思路。本文认为,红山文化元素能赋予古典舞创作强大生命力,丰富古典舞创作语言冲击力,唤醒古典舞创作文化记忆力。

文化翻译理论视域下红山文化负载词的英译策略研究

作为中国北疆地区比较早的史前文化遗存,红山文化是史前文明的典型标志。它不仅属于中国人民,也属于全世界,因此理应被世界上更多的人了解与关注。然而,通过考察发现,红山文化负载词的英译数量相对稀少,而且存在不同程度的硬译、误译现象。本文以文化翻译理论为基,探析合理应用“归化”“异化”翻译策略,提升红山文化英译质量。

红山水库浮游生物调查及鱼产力估算

参照《内陆水域渔业资源调查手册》,于2021年5月、7月和9月,对内蒙古自治区赤峰市红山水库的浮游生物进行了3次采样调查,共鉴定到浮游植物6门87个种属,浮游植物平均生物量为11.899 mg/L,平均密度为3111.99×10^(4)个/L,Margalef指数平均为1.394,Shannon-Wiener指数平均为2.766,Pielou指数平均为0.597。共鉴定到4门39个种属的浮游动物,浮游动物平均生物量为3.183 mg/L,平均密度为5776.78个/L,Margalef指数平均为2.087,Shannon-Wiener指数平均为2.044,Pielou指数平均为0.548。综合浮游生物种群结构、现存量和生物多样性指数结果,红山水库处于富营养化状态。根据红山水库浮游生物调查结果估算鱼产力为115.611 kg/hm ^(2)。

雅俗共融:红山文化在文创产品设计中的现代转化

本文深入探究了红山文化在现代文创产品设计中的应用,特别是造型提取、纹样提取和色彩提取这3个关键设计方法。通过分析红山陶器和玉器的独特风格与文化内涵,强调了其现代转化的重要性,旨在保留原始韵味的同时赋予新的生命力。在现代转化过程中涉及的根本问题是如何让大众深刻体验红山文化魅力并树立文化自信,设计需忠实于红山文化精神,符合其个性,使文创产品成为有效的文化传播媒介。红山文化与现代设计结合,不仅是传统文化的致敬,也是文化传承与创新的重要途径,红山文化在文创产品设计中的应用,是连接历史与现代、传统与创新的桥梁,展现了红山文化在当代社会的活力和可能性。

高层住宅火灾危险性分析与逃生设计——以赤峰市红山区为例

针对高层住宅火灾形势愈发严峻,住户生命安全难以保障的问题,以赤峰市红山区为例,对区内857处高层住宅及其住户进行调研,指出存在的火灾隐患,获取不同人群在火灾时的行为方式与逃生需求,并结合地区消防安全现状为高层住户的逃生设计提供对应建议。

Hongshan Goddess

The Hongshan cultural relics at Niuheliang, Liaoning Province is a large scale ruin where sacrifices used to be offered to the goddess and ancestors. It is composed of a goddess temple, a sacrificial altar and many stone graves. From the ruins of the goddess temple, a clay sculpture of a goddess head has been unearthed.

交响合唱《女神大合唱》对红山文化音乐元素的挖掘与创作研究——以第三乐章《陶鼓声震八百里》为例

为了弘扬中国传统文化,坚定文化自信的目的,音乐人用交响合唱的形式,对红山文化音乐元素进行挖掘创作和深入研究,研究和宣传红山文化已成为弘扬中国传统文化、坚定文化自信的一个重要的措施。作品《女神大合唱》创作团队紧紧围绕这个重大主题,在考古学家的大力支持下,多次深入实地进行考察、研究和深入生活。研究发现,将最具代表性的红山文化实物,以艺术的形象给予升华和呈现,更具有真实感和说服力。作品《女神大合唱》的内容涉及红山文化的玉龙、女神像等多个重要标志型,该作品体现了对红山文化音乐元素挖掘的重要性和创作研究的可行性,起到了对牛河梁文化及中华民族的赞美和宣传作用。

红山文化旅游文创产品设计

发挥旅游文创产品在文化的传播和发展的过程中,发挥巨大作用的同时也挖掘红山文化文创产品极大的商业价值。运用现代设计手法对红山出土文物进行抽象提取结合红山时期先民的日常生活进行创作。对红山文化文创产品进行创新。红山文化旅游文创产品更是文创产品设计中不可或缺的宝藏资源。本文以红山文化旅游文创产品为主要研究对象,针对目前其文创产品设计存在的问题以及相关策略进行了深刻的探讨。有利于改善目前红山文创产品的状况。