Classification and Development Laws of Karst Landform in Suzhou Area, North Anhui Province of China

Suzhou area in north Anhui Province is a low hilly area on the Huaibei Plain where carbonate rocks and karstification are widely distributed, and karst landscapes form major physical contours of the bedrock outcrops. Through field investigation, karst landscapes of Suzhou area were divided into two categories based on their morphological characteristics: macro-geomorphologic landscapes including normal hills, dry valleys, karst springs and caves, and micro-corrosion landscapes including corrosion pits, dissolved pores, dissolution traces, corrosion cracks, clints and karrens. Distribution, development and scale of karst landscapes in this region are controlled by climate, rock type, structure, topography and other factors. It was suggested that karst landscapes in the study area could be used as a representative of karst landforms in North China.

Lead Isotope Studies of Massive Surphur-Iron-Gold Deposits in the Tongling Area, Anhui Province

Pb isotope ratios and their variation have been measured and explained on ores of massive S-Fe-Au depos-its hosted in the Middle-Upper Carboniferous, on feldspars from diorite bodies closely related tomineralization and on whole rocks from ore-hosting strata (carbonate rocks) in the Tongling area, Anhui Prov-ince. Through a comparison of Pb isotope features of these geological bodies, it has been suggested that oresubstances of the deposits were derived from ore-hosting strata. In the meanwhile, the measurement of ore Pbisotopes of different mineralization types of the same deposit indicates that different mineralization types havedistinct Pb isotope characteristics, showing the potentiality of the Pb isotopic method used in mineral explora-tion.

Discovery of the World's Second Largest Molybdenum Deposit in the Shapinggou Area,Jinzhai County,Anhui Province

In the year of 2011, a superlarge molybdenum deposit was discovered in the Shapinggou area, Jinzhai county, Anhui Province by the Bureau of Geology and Mineral Exploration of Anhui Province, with its reserve more than 2.2 million ton, just next to the Klimax molybdenum deposit （〉3.3 million ton） in Colorado. It has ranged the world＇s second largest molybdenum deposit, with potential economic value up to 100 billion dollars.

The Forming Mechanisms of the Neoproterozoic Molartooth Carbonatites in North Anhui and Jiangsu Provinces

As a characteristic sedimentary type,molartooth carbonatites veins(MCV) can be found in almost all the Neoproterozoic carbonatite strata in the North Anhui and Jiangsu Provinces.But their forming mechanism is still an enigma,and more than four incompatible forming hypotheses have been put forward according to the structures,mineral components and elements of the MCV.Though all the MCV with the similar shape

THE RESEARCH INSTITUTES AFFILIATED TO THE CAS IN HEFE1 AREA, ANHUI PROVINCE

The Hefei Branch of the CAS is an R&D base specializing in basic research and applied developmentof technological physics, established by the CAS in the area of Hefei City,capital of Anhui Province.It is situated beside the Dongpu Reservoir in the western suourb of the City’s downtown area,covering 186.7 hectares in total area. At present, the Branch consists of five subordinate unit.i.e.the Branch organ, the Anhui Institute of Optics & Fine Mechanics, the Institute of Plasma Physics, the Institute of Solid-state Physics and the Institule of Intel-

Child Mortality Patterns in Rural Areas of Anhui and Henan Provinces in China, 1990

County-based IMR and U5MR in Anhui and Henan provinces in China were estimated and analyzed by using the 1990 Census Data. Census was conducted on July 1,1990, the number of deaths only occurred in the first half year of 1990 was collected. In order to obtain the total population and total number of deaths in the same year, the total number of deaths in each eqersex group for the whole 1990 was then estimated by taking the death number in the first half of 1990 as the base and multiplying a coefficient, which varied in different age-sex-region groups. Two major adjustments for some possible underreporting cases in female birth and infant death were made. If the sex ratio at age 0 in some counties was beyond 1. 2, then it was taken as 1. 15 for rural counties and 1.10 for urban cities, which were the estimates of sex ratios for the children at ape 5 in the national 1% Population Sampling Survey in 1995. The adjustment for IMR were made by comparing the segment of the county lift table from age 15 through 59 with that from the same age groups in the international and Chinese Model Life Tables. The IMR in the county life table would be substituted by the one in the closest Model Life Talbe, if it was less than in the latter.The findings of the analysis may be summarized as fol1ows: (i) Total county-based IMR and U5MR were 33. 4 Per 1000 and 41. 4 per 1000 respectively, with great variations between urban cities (25. 4 per 1000 for IMR and 31. 4 per 1 000 for U5MR) and rural counties (35. 1 Per 1000 for IMR and 43. 6 per 1000 for U5MR). There were also sighficant differences in child mortality between nationally identified Poor counties and other counties in rural areas. In the opr counties the total IMR was 40. 7 per 1 000 living births in average while in non-opr counties it was only 33. 2 per 1000 in average (P < 0.05). The U5MR in opr counties was 25 percent higher than in non-opr counties (51. 5 vs 40. 9 Per 1 000 living births).(ii) Statistically significant correlation between child mortality and socio-economic variables was revealed from the data set, among which gross social economic products per capita was found to have the strongest relationship with child mortality. The neqative correlation was found between child mortality and a set of socalled' rich' variables including the gross social products, gr-oss agricultural products, gna industrial products and the proportions of high-educated population at county level, whereas the poSitive correlation was found between child mortality and a set of'poor' variables, such as proportions Of residents with lower 1evel of education and illiteracy rate.(iii) thfferences in child mortality between these two provinces were found, which were identical to the trends of differences in socio-economic indicators between them.tower child mortality proved to be associated with better socio-economic conditions(higher per capita products, higher proPortions of residents with higher level of education, lower proportion of less educated people and illiteracy) in province Henan.

Geochemical Characteristics of Sedimentary Manganese Deposit of Guichi, Anhui Province, China

The sedimentary manganese deposits occurring in Gufeng formation of the Permian in Guichi area, south Anhui Province, include manganese carbonate deposit formed by sedimentation, and manganese oxide deposit made by later oxidation. The total REE contents of these samples are relatively low （ 〈 250 × 10^- 6）, belonging to LREE-enriched type, showing LREE enrichment during the process of formation of Mn deposit, especially during Mn-oxidizing process. Three normalized REE patterns and SCNA-normalized trace elements spider diagrams of the Mn-bearing sequence rocks and ores in this area reflect their same origin of ore sources, which is similar to rock-forming and ore-forming conditions. The Mnforming materials primarily came from the continent with higher mature degree and single material source. The δEu and δCe negative anomaly and Ce anomaly （ 〈 - 0.1） manifest that Mn-bearing sequence of the Permian was mostly formed in marine basin and oxidative environment. The Sr and Ba anomaly, Sr/Ba and Co/Ni values reflect the Mn deposit environment was of deep water and high-salinity of marine facies. Although the Ce/La （mean 1.05）, Y/Ho （25 - 41.5） and trace metals show a variety of correlations with Mn in the ten rock samples, which show multiple sources for the manganese, the analysis of geochemical characteristics indicate that the material sources of Mn deposit have been primarily terrestriallyderived. Another source of the manganese probably comes from the seafloor volcanism in this area. Analysis of sedimentary features and geohistoric evolvement reveals that the maximum transgression of the Qixia Period, ore district is then in deep shelf-basin sedimentary setting and the Mn-bearing sequence is deposited.

Basic Features of the Crustal Structure in the Lower Yangtze and Its Neighboring Area in the Chinese Mainland： Review of Deep Seismic Sounding Research

The Deep Seismic Sounding( DSS) projects carried out from the 1970 s in the lower Yangtze region and its neighboring area were reviewed in this paper,then the basic wave group features of those wide angle reflection / refraction record sections,and of the crustal structure are summarized. It shows that there were in total five clear wave groups on the record sections,which include the first arrival Pg,the reflection P1 from the bottom interface of the upper crust,the reflection P3 from the bottom interface of the middle crust,the strong reflection Pm from the Moho boundary,and the refraction Pn from uppermost mantle. In general,these phases are easily consistently traced and compared,despite some first arrivals being delayed or arriving earlier than normal due to the shallow sedimentary cover or bedrocks. In particular,in the Dabie Mountain region the seismic events of a few gathered shots always have weak reflection energy,are twisted,or exhibit disorganized waveforms, which could be attributed to the disruption variations of reflection depth,the broken Moho,and the discontinuity of the reflection boundary within crust. The regional crustal structures are composed of the upper,middle and lower crust,of which the middle and lower layers can be divided into two weak reflection ones. The crustal thickness of the North China and Yangtze platform are 30km- 36 km,and the Moho exhibits a flat geometry despite some local uplifts. The average pressure velocity in lower crust beneath this two tectonic area is 6. 7 ± 0. 3km / s. Nevertheless,beneath the Dabieshan area the crustal thickness is 32km- 41 km,the Moho bends down sharply andtakes an abrupt 4km- 7km dislocation in the vertical direction. The average pressure velocity in the lower crust beneath the Dabieshan area is 6. 8 ± 0. 2km / s.

安徽铜陵地区晚中生代中基性侵入岩成因与成矿:来自磷灰石矿物学和地球化学证据

辉石闪长岩是安徽铜陵地区晚中生代侵入岩的重要类型,与铜金多金属成矿密切相关。本文以白芒山岩体和舒家店岩体辉石闪长岩为研究对象,着重开展磷灰石矿物学和地球化学研究,探索中基性侵入岩成因及与成矿关系。结果显示:磷灰石强烈富集稀土元素,轻重稀土元素分异明显,弱—中等Eu负异常,富集Th、U等高场强元素,亏损Ta、Nb、Ti、Zr、Hf等高场强元素和Rb、Ba、Sr等大离子亲石元素,稀土—微量元素组成特征指示其寄主岩石成岩物质具有壳幔混源特征。岩相学特征显示磷灰石具有两种不同的晶体形态、产出状态和显微结构,即长柱状、包裹体相、均质结构和短柱状、晶间相、核—边/环带结构,其元素地球化学特征有显著差异,指示其寄主岩石成岩作用经历过壳源长英质岩浆冷凝结晶→高温幔源镁铁质岩浆注入和长英质岩浆早期结晶矿物熔蚀→混合岩浆侵位和结晶的复杂过程。核—边/环带结构磷灰石从核部到边部SO_(3)和Cl含量波动式变化特征,指示镁铁质岩浆幕式注入,并触发混合岩浆上升侵位,有利于流体出溶和热液成矿。磷灰石卤族元素(F、Cl)和SO_(3)高含量则提供板块俯冲环境证据,指示基性端元的镁铁质弧岩浆来自俯冲板片析出流体交代富集岩石圈地幔,镁铁质岩浆幕式注入有利于流体出溶和热液成矿。

冀北上黄旗地区多金属矿成矿规律与矿产预测

冀北上黄旗地区位于华北地台北缘中段成矿带及兴安太行南段成矿带的相交区域,是华北地区著名的(银)多金属成矿区。本文在综合分析区域成矿地质背景、成矿地质条件、地球物理、地球化学、遥感异常特征及成矿规律的基础上,认为该区具有寻找侵入岩型和陆相火山岩型两大类多金属矿床的有利条件,划分出3条Ⅳ级成矿亚带,圈定成矿远景区10个。其中,A类4处,B类4处,C类2处;并优选出多金属矿找矿靶区7个,A类4个,B类2个,C类1个。

安徽枞阳县黄龙桥地区隐爆角砾岩筒特征及其与铀成矿关系

安徽枞阳黄龙桥地区隐爆角砾岩筒地处庐枞盆地黄梅尖A型花岗岩体内,是岩体内发育的规模最大、最为典型的隐爆角砾岩筒。文章在详细的野外地质调查、物化探测量和钻孔岩心地质编录的基础上,通过显微岩石学、元素地球化学特征研究,分析其地质特征并探讨其与铀成矿的关系。分析研究表明:隐爆角砾岩具有角砾成分杂、隐爆作用强度大、“隐爆源”埋藏深特点,其自身并不含有铀矿化现象,铀元素平均含量远远低于石英正长岩;ΣREE为293.16×10^(-6)~453.45×10^(-6),LREE/HREE为6.71~11.00,δCe为0.89~1.02,δEu为0.46~0.57,呈现较明显的负Eu异常,稀土元素配分模式呈右倾斜型,具有轻稀土分馏明显,重稀土分馏不明显的特点;隐爆角砾岩内部发育的大量赤铁矿形成于岩浆“隐爆”作用之前,铀成矿作用发生在隐爆角砾岩筒形成之后,推测隐爆角砾岩爆发时间在124~115 Ma;隐爆角砾岩筒主要为铀成矿提供了重要的导矿通道,外围具有较好的铀矿找矿潜力,而其深部具有寻找铁矿的潜力。

文旅融合视域下皖南国际文化旅游示范区建设路径研究

党的二十大报告中提出要坚持以文塑旅、以旅彰文,推进文化和旅游深度融合发展。国家全域旅游示范区创建工作正持续开展,文旅融合在旅游示范区建设工作中起着至关重要的作用。梳理皖南国际文化旅游示范区建设现状,厘清示范区现有资源优势,分析其所面临的文化传承不力、创新能力欠缺、产业延伸不足、制度框架不全等问题,从保护传承文化资源、凸显文化特色内涵、加快全域旅游发展和提高旅游服务质量4个方面针对性地提出示范区具体建设路径,以期稳步推进示范区建设,助其融入长三角旅游高质量发展,并为文旅融合视域下同类型旅游区建设发展提供参考和指引。

皖南国际文化旅游示范区A级景区空间分布及影响因素

为落实党的二十大报告中区域协调发展的新要求,顺应全域旅游与文旅深度融合新趋势,开展皖南国际文化旅游示范区旅游资源格局的研究,能够为示范区后续开发建设提供思路与导向。借助平均最近邻指数、不平衡指数、核密度、地理探测器等方法,解析示范区内A级景区的空间特征及影响因素。结果表明:示范区A级景区整体分布不均衡,呈现集中分布特征;示范区内A级景区显现“两主、四次”的空间格局,呈现Y字形分布态势;遗产点密度因子驱动力最强,经济发展因素对A级景区空间分布影响程度较大,自然环境因素驱动力较弱;局部自相关分析表明多数因子聚类特征表现明显;交互探测结果表明两种因子共同作用强于单因子作用。

安徽省丘陵山区农业机械化水平研究

现代农业的崛起,极大程度地提升了农业劳动效率、土地生产力和农产品的商品化水平。安徽省在推进农业机械化方面取得进展,但仍面临若干重要挑战,特别是在山丘陵区的机械化推广上。该文通过研究安徽省丘陵山区农业发展概况,重点探讨在新时代限制山丘陵地区农业机械化推广的关键因素,并提出针对性的解决策略。这些策略将为我省新时期山地丘陵农业机械化的推广提供战略支持,有助于促进我省丘陵山区农业机械化的广泛应用。

皖南山区不同类型森林土壤阳离子交换性能差异

为了解皖南山区不同类型森林土壤阳离子交换性能差异,为该区合理营林提供参考,选取皖南山区6种不同类型森林土壤(杉木林、马尾松林、栓皮栎林、外松林、天然阔叶林和杉木-栓皮栎混交林)为研究对象,比较森林土壤阳离子交换性能的差异。结果表明:(1)研究区土壤呈强酸性,土壤有机质含量为33.84~91.50 g·kg^(-1),总氮含量为0.94~3.37 g·kg^(-1),碱解氮含量为131.58~203.62 mg·kg^(-1),总磷含量为0.22~0.77 g·kg^(-1),有效磷含量为0.17~0.32 mg·kg^(-1);土壤主要缺乏速效磷养分。(2)阳离子交换量在8.09~12.57 cmol·kg^(-1)之间,排序为:天然阔叶林>外松林>马尾松林>混交林>杉木林>栓皮栎林,不同森林土壤间阳离子交换量的差异主要由其土壤有机质的差异引起。(3)交换性盐基总量在1.74~2.72 cmol·kg^(-1)g之间,排序为:马尾松林>外松林>杉木林>栓皮栎林>混交林>天然阔叶林,Ca^(2+)和Mg^(2+)是主要的盐基离子,是成土过程中Ca、Mg优先固持形成的。(4)盐基饱和度在13.97%~28.98%之间,排序为:马尾松林>杉木林>栓皮栎林>外松林>混交林>天然阔叶林,该差异是由淋溶作用和树木对盐基离子的吸收共同作用形成的差异。综上,研究区土壤保肥和缓冲性能较低且供肥能力较差,尤其是土壤速效磷供应能力差。其中松林的供肥保肥能力及缓冲性能明显优于其他树种森林,混交林的速效养分含量更高,故可通过营造松类混交林以及施肥来提高森林土壤供肥保肥能力和缓冲性能。

面向经济欠发达地区纺织服装产业高职技术人才培养模式研究--以皖北地区为例

纺织服装产业是经济欠发达地区经济发展的重要支撑,也担负着稳民生促就业的重要使命。文章以皖北地区为例,在梳理皖北地区2019-2022年纺织服装产业发展数据后,认为该地区纺织服装行业目前存在利润下滑、企业发展后劲不足等劣势。企业高质量的发展离不开人才的支撑,而高职院校是人才培养的重要基地。为此,文章基于皖北地区纺织服装人才新需求来探究高职院校“三阶段技能递进式”人才培养模式,以期优化人才培养方法,提高经济欠发达地区纺织服装产业高职技术人才培养质量。

皖南山区洞栖性蝙蝠的本底资源现状调查

2022年6—8月,基于竖琴网、雾网、抄网等工具,对安徽省皖南山区洞栖型翼手目(Chiroptera)多样性进行了调查。调查中共发现翼手目动物4科4属17种,其中,菊头蝠科(Rhinolophidae)1属8种,占比47.05%;蹄蝠科(Hipposideridae)1属2种,占比11.76%;蝙蝠科(Vespertilionidae)1属6种占比35.29%;长翼蝠科(Miniopteridae)1属1种,占比5.88%。从动物区系来看,东洋型共有12种,占比70.59%,南中国型(1种)和季风型(4种)较少。结果显示皖南山区在安徽省洞栖蝙蝠物种丰富度方面,具有较高的多样性水平。此外,在调查的基础上,对皖南山区洞穴型蝙蝠的濒危等级、保护现状、区系特点进行了概述。本次调查能够为安徽省后期开展的翼手目动物资源调查与监测工作提供科学依据。

安徽省宣城地区龙潭组页岩孔隙发育特征及其影响因素

安徽省宣城地区上二叠统龙潭组页岩气资源潜力大,已有钻井揭示其页岩含气性差异大,页岩气赋存富集机理复杂。通过总有机碳含量分析、岩石热解实验、X衍射、低温液氮吸附、二氧化碳吸附和场发射扫描电镜观测等手段,研究宣城地区龙潭组页岩中孔隙的大小、结构及类型,探讨影响其孔隙发育的主要因素。研究表明:(1)宣城地区龙潭组页岩中孔隙主要为半开放型,并且存在一定量的细颈瓶孔。其中,矿物孔较发育,主要为微米孔,孔隙数量多;有机孔发育数量较少,孔径为纳米级—微米级。(2)龙潭组页岩BET比表面积为4.2601~10.3068 m^(2)/g,平均为7.4290 m^(2)/g。介孔+宏孔体积为0.0049~0.0179 cm^(3)/g,平均为0.0089 cm^(3)/g;微孔体积为0.0019~0.0038 cm^(3)/g,平均为0.0026 cm^(3)/g。孔径大于10 nm的孔隙是页岩孔隙体积的主要贡献者。(3)高演化、矿物含量差异大等使得宣城地区龙潭组页岩孔隙发育规律性变得复杂,TOC含量和矿物含量明显影响着宣城地区龙潭组页岩孔隙体积,但与孔隙比表面积没有明显线性相关性。在宣城地区龙潭组页岩气后续勘探开发中,应注重较高TOC含量、较高碳酸盐矿物含量和较低黏土矿物含量的页岩。

抗战与民生:邓子恢与淮北抗日根据地经济建设

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