Geochemistry, zircon U–Pb geochronology, and Hf isotopes of S-type granite in the Baoshan block, constraints on the age and evolution of the Proto-Tethys

Geochemistry, zircon U–Pb geochronology, and Hf isotope data for the Early Paleozoic granites in the Baoshan Block reveal the Early Paleozoic tectonic evolution of the Proto-Tethys. The samples are high-K, calcalkaline, strongly peraluminous rocks with A/CNK values of 1.37–1.46, are enriched in SiO2, K2O, and Rb, and are depleted in Nb, P, Ti, Eu, and heavy rare earth elements,which indicates the crystallization fractionation of the granitic magma. Zircon U–Pb dating indicates that they formed in ca. 480 Ma. The Nansa granites have εHf(t) values ranging from-16.04 to 4.36 with corresponding TC DMages of 2.10–0.81 Ga, which suggests the magmas derived from the partial melting of ancient metasedimentary with minor involvement of mantle-derived components. A synthesis of data for the Early Paleozoic igneous rocks in the Baoshan block and adjacent(Tengchong,Qiangtang, Sibumasu, Himalaya, etc.) blocks indicates that these blocks were all aligned along the proto-Tethyan margin of East Gondwana in the Early Paleozoic. The Early Paleozoic S-type granites from Nansa were generated in a high-temperature and low-pressure(HTLP) extensional tectonic setting, which resulted from Andean-type orogeny instead of the final assembly of Gondwana or crustal extension in a non-arc environment. In certain places, an expanding environment may exist in opposition to the tectonic backdrop of the lithosphere’s thickening and shortening, leading the crust to melt and decompress,mantle-derived materials to mix, and a small quantity of peraluminous granite to emerge.

Detecting land subsidence near metro lines in the Baoshan district of Shanghai with multi-temporal interferometric synthetic aperture radar

Land subsidence is a major factor that affects metro line （ML） stability. In this study, an improved multi- temporal interferometric synthetic aperture radar （InSAR） （MTI） method to detect land subsidence near MLs is presented. In particular, our multi-temporal InSAR method provides surface subsidence measurements with high observation density. The MTI method tracks both point-like targets and distributed targets with temporal radar back- scattering steadiness. First, subsidence rates at the point targets with low-amplitude dispersion index （ADI） values are extracted by applying a least-squared estimator on an optimized freely connected network. Second, to reduce error propagation, the pixels with high-ADI values are classified into several groups according to ADI intervals and processed using a Pearson correlation coefficient and hierarchical analysis strategy to obtain the distributed targets. Then, nonlinear subsidence components at all point-like and distributed targets are estimated using phase unwrapping and spatiotemporal filtering on the phase residuals. The proposed MTI method was applied to detect land subsidence near MLs of No. 1 and 3 in the Baoshan district of Shanghai using 18 TerraSAR-X images acquired between April 21, 2008 and October 30, 2010. The results show that the mean subsidence rates of the stations distributed along the two MLs are -12.9 and -14.0 ram/year. Furthermore, three subsidence funnels near the MLs are discovered through the hierarchical analysis. The testing results demonstrate the satisfactory capacity of the proposed MTI method in providing detailed subsidence information near MLs.

The Characteristics of Ore-Controlling Structure in Baoshan Cu-Pb-Zn Polymetallic Deposit,Hunan Province

The Baoshan Cu-Pb-Zn polymetallic deposit is lied in the central Nanling mineralization zone,and belongs to the junction area of the Chenzhou-Linwu fault zone and the Leiyang-Linwu fault zone.It is a significant part of Nanling polymetallic deposit belt.The outcropping stratas consist of upper Devonian Shetianqiao,Xikuangshan Formation,Lower Carboniferous Menggong’ao,Shidengzi,Ceshui,and Zimenqiao Formation.Igneous rocks in the Baoshan ore area mainly comprise granodiorite porphyry.Furthermore,the radio isotopic age ranges from 123 Ma to 183 Ma,belonging to the early to middle Yanshanian.

Metallogenic Prediction of the Peripheral Areas of the Xiyi Concealed Lead-Zinc Deposit in Baoshan City, Yunnan Province

The newly-discovered Xiyi lead-zinc deposit is a large deposit located in the north central Baoshan block of the southern Sanjiang metallogenic belt section, Southwest China.The surface of the deposit is mainly covered by eluvial-deluvial lateritic layer, without any mineralized outcrops. The main concealed orebody V3 is buffed in the depth of 300-500m. The orebodies are controlled by certain stratigraphic horizons, and most are cut by strata with a high angle, while a few occur along the strata. The direct wall rocks are calcisiltite, calclithite, bioclastic calcarenite,

Early Permian Conodonts from the Baoshan Block, Western Yunnan, China

The Rabeignathus bucaramangus fauna was recently found from the limestone beds of the top part of the elastics-dominated Dingjiazhai Formation in the Aluotian section, southern Baoshan Block, western Yunnan. With Rabeignathus bucaramangus as the dominant species, this fauna includes Rabeignathus bucaramangus (Rabe), Homeoiranognathus huecoensis (Ritter), Sweetognathus inomatus Ritter, Sweetognathus whitei (Rhodes), Mesogondolella cf. bisselli (Clark and Behnken) and a few of ramiform elements. The characteristies of the fauna suggest that it can be correlated with the upper part of the Sweetognathus whitei Zone and assigned to the Middle Artinskian.

New Materials of the Shanita-Hemigordius Assemblage (Permian Foraminifers) from the Baoshan Block, Western Yunnan

Fossil materials of Shanita and Hemigordius from a section northeast of the Woniusi (the Woniu Temple) of Baoshan, western Yunnan are described and figured in this paper. Field investigation indicates that fossils of these two foraminifer genera are extremely abundant and form a typical Shanita-Hemigordius assemblage in the so-called 'Cracked Limestone' in the Baoshan area. Preliminary study has revealed that the features of this assemblage, which includes Shanita amosi, S. chagouensis, Hemigordius renzi and H. biconcavus, are similar not only to the Shanita fauna previously reported from the Shazipo Formation in the Zhengkang area, west Yunnan, but also to those from the Permian of Burma, Thailand, Iran and Turkey.

The Early Permian Woniusi Flood Basalts from the Baoshan Terrane, SW China: Petrogenesis and Geodynamic Implications

The Woniusi flood basalts from the Baoshan terrane,SW China,represent a significant eruption of volcanic rocks which were linked to the Late Paleozoic rifting of the Cimmeria from the northern margin of East Gondwana.However,the precise mechanism for the formation and propagation of the rifting is still in debate.Here we report 40 Ar/39 Ar dating,whole-rock geochemistry,and Sr-Nd-Pb isotopes for the Woniusi basalts from the Baoshan terrane of SW China,with the aim of assessing if a mantle plume was related to the formation of the continent Cimmeria.40 Ar/39 Ar dating of the Woniusi basalts yielded ages of 279.3±1.1 Ma and 273.9±1.5 Ma,indicating they were emplaced during the Early Permian.Whole-rock geochemistry shows that these basalts have subalkaline tholeiitic affinity,low Ti O2(1.2-2.2 wt%),and fractionated chondrite-normalized LREE and nearly flat HREE patterns[(La/Yb)N=2.86-5.77;(Dy/Yb)N=1.21-1.49]with noticeable negative Nb and Ta anomalies on the primitive mantle-normalized trace element diagram.Theε(Nd)(t)values(-4.76 to+0.92)and high(206 Pb/204 Pb)i(18.40-18.66)along with partial melt modeling indicates that the basalts were likely derived from a sub-continental lithospheric mantle(SCLM)source metasomatized by subduction-related processes.On the basis of a similar emplacement age to the Panjal basalts and Qiangtang mafic dykes and flood basalts in the Himalayas,combined with a tectonic reconstruction of Gondwana in the Early Permian,we propose that the large-scale eruption of these basalts and dykes was related to an Early Permian mantle plume that possibly initiated the rifting on the northern margin of East Gondwana.

Distribution of Landslides in Baoshan City,Yunnan Province,China

Using Google Earth software as a platform,this study has established an integrated database of both old and new landslides in Baoshan City,Yunnan Province,China,and analyzed their development characteristics together with distribution rules,respectively.Based on the results,a total of 2427 landslides occurred in the study area,including 2144 new landslides and 283 old landslides,with a total area of about104.8 km^2.The new landslides are mostly in small-scales with an area less than 10000 m^2,while the area of individual old landslide is mostly larger than 10000 m^2.By analyzing the relationship between the two types of landslides and eight impact factors(i.e.,elevation,slope angle,slope aspect,slope position,lithology,fault,regional Peak Ground Acceleration(PGA),and average annual rainfall),the different individual influencing factors,distribution regularities and mechanisms of the two types of landslides are revealed.In detail,the main influencing factors of new landslides are elevation,slope angle,slope aspect,slope position,lithology,regional PGA and average annual rainfall,while the influencing factors of old landslides are mainly elevation,slope angle,and lithology.This study provides basic data and support for landslide assessment and further disaster reduction in Baoshan City.Besides,it also provides new constraints in deeply understanding the effect of different topographic and geological conditions,historical earthquakes,rainfall and other factors on the occurrence mechanisms of both new landslides and old landslides.

Rare earth element(REE) geochemistry of different colored fluorites from the Baoshan Cu–Pb–Zn deposit, Southern Hunan,South China

The Baoshan Cu–Pb–Zn deposit, located in the central part of the Qin–Hang belt in South China, is closely related to the granodiorite-porphyry. However, the characteristics and the source of the ore-forming fluid are still ubiquitous. According to the crosscutting relationships between veinlets and their mineral assemblages, three stages of hydrothermal mineralization in this deposit were previously distinguished. In this contribution, two different colored fluorites from the major sulfide mineralization stage are recognized:(1) green fluorites coexisting with Pb–Zn ores;and(2) violet fluorites coexisting with pyrite ores. Y/Ho ratios verify the green fluorites and violet fluorites were co-genetic. The fluorites display elevated(La/Yb)Nratios, which decrease from 1201 to 5710 for green fluorites to 689–1568 for violet fluorites, indicating that they precipitated at the early hydrothermal sulfide stage,and Pb–Zn ores crystallized earlier than pyrite ores. The similar Tb/La ratios of the fluorites also indicate that they precipitated at an early stage within a short time. From the green fluorites to violet fluorites, the total rare earth element(ΣREE)concentrationsdecreasefrom1052–1680 ppm to 148–350 ppm, indicating that the green fluorites precipitated from a more acidic fluid. The Eu/Eu*ratios increase from 0.17 to 0.30 for green fluorites to0.29–0.48 for violet fluorites, and the Ce/Ce* ratios decrease from 1.08–1.13 to 0.93–1.11, suggesting a gradual increase in oxygen fugacity(fO_(2)) and pH value of the mineralization fluid. Though the fluorites display similar REE patterns to the granodiorite-porphyry and limestone,the ΣREE concentrations of the fluorites are significantly higher than those of limestone and the granodiorite-porphyry, suggesting that an important undetected non-magmatic source is involved to provide sufficient REE for fluorites. The most plausible mechanism is fluid mixing between magma fluid and an undetected non-magmatic fluid.

The study of unified needs assessment system of the elderly care in Shanghai -- taking Baoshan District as an example

In2000, the WHO announced the article named ＂establish the long-term care policy ofelderly＂ .It declares the international consensus on long-term care definition, key issues and policy guidelines, and describes the initial action to establish long-term care for the elderly in terms of international consensus on policy, formulated to provide a strategic framework for the long-term care policy for the world. Shanghai city in December 2014 launched the＂ The assessment methods of unified care demand system for elderly in Shanghai city （Trial）＂; firstly,the paper will analyze ＂The assessment methods of unified care demand system for elderly in Shanghai city （Trial）＂ deeply, and secondly investigate how to carry out the policy of unified care elder in Baoshan District, finally summed up the Baoshan District elderly care demand analysis and evaluation of the construction of a unified existence the problem, combined with the problems,we will give the corresponding countermeasures and suggestions.

2018-2023年保山市农村饮用水水质卫生监测结果分析

目的:了解保山市农村饮用水水质卫生状况,为保障农村水资源质量安全提供科学依据。方法:根据云南省城乡饮用水水质监测工作方案的要求,对2018-2023年保山市农村饮用水水质监测数据进行统计学分析。结果:2018-2023年共监测3790个样本,合格率为63.85%,不同年份之间合格率有显著性差异(P<0.05)。监测指标中有16个项目超标,超标率大于10%的项目均属于微生物指标。丰水期和枯水期的合格率无显著性差异(P>0.05),出厂水和末梢水的合格率有显著性差异(P<0.05)。结论:保山市农村饮用水的水质合格率较低,微生物污染是主要因素,水质有待进一步改善提升。

保山市隆阳区观赏种子植物资源多样性研究

通过野外调查与文献查阅,整理得出保山市隆阳区观赏种子植物名录。结果表明,隆阳区观赏种子植物81科185属286种,其中裸子植物6科9属10种,被子植物75科176属276种,优势科为兰科、蔷薇科、木犀科、鸢尾科;按照生活型划分为乔木类33种、灌木类114种、草本类133种、藤本类6种;按观赏类型可分为观花类植物174种、观植株类植物130种、观果类植物32种、观叶类植物19种。旨在掌握隆阳区观赏种子植物资源应用现状,并对观赏种子植物资源保护与开发利用提出建议。

原特提斯洋在滇西南地区的俯冲记录:来自保山地块奥陶纪花岗岩的年代学、地球化学以及Hf-Nd同位素的支持

中国西南地区在早古生代期间位于冈瓦纳大陆北缘,该地区保存有早古生代岩浆岩记录,它们的形成与原特提斯洋的演化密切相关。本文报道了滇西南地区保山地块平达乡附近的早古生代花岗岩的岩石学、全岩主-微量地球化学、LA-ICP-MS锆石U-Pb年龄、锆石Hf同位素和磷灰石Nd同位素组成,以探讨保山地块早古生代花岗岩的岩石成因、岩浆源区性质以及岩体形成的地球动力学机制。通过对保山地块平达花岗岩中岩浆锆石开展LA-ICP-MS U-Pb同位素测试,结果显示花岗岩形成于465.9~454.9Ma,是中-晚奥陶世岩浆作用的产物。平达岩体主体岩性为二长花岗岩,主要矿物组成为斜长石、石英和碱性长石(条纹长石和正长石),次要矿物为黑云母和白云母。本文报道的花岗岩样品显示出高的SiO_(2)(72.16%~76.87%)和Al_(2)O_(3)(12.50%~14.36%)含量,低的MgO(0.12%~0.64%)、Mg#(20.9~35.9)、Cr和Ni含量以及较高的Rb/Sr和Rb/Ba比值;结合花岗岩较高的A/CNK值(1.06~1.45),显示弱过铝质至强过铝质的特征,表明其属于S型花岗岩。此外,平达岩体二长花岗岩样品具有低的Al_(2)O_(3)/TiO_(2)比值和变化的CaO/Na_(2)O、Rb/Sr、Rb/Ba比值,表明其岩浆源区包含泥质岩石和砂质岩石,显示混合源区的特征。结合滇西南早古生代二长花岗岩变化较大的锆石εHf(t)值(-11.10~-4.05)、磷灰石εNd(t)值(-8.76~-6.96)和Hf同位素二阶段模式年龄(2140~1704Ma),表明它们的岩浆源区为古元古代地壳中泥质岩石和砂质岩石混合源区。综合滇西南地区广泛发育的早古生代岩浆岩以及同时期的蛇绿混杂岩记录,本文认为保山地块早古生代S型花岗岩是地壳沉积组分部分熔融的产物,形成于原特提斯洋西向俯冲相关的活动大陆边缘背景。

新疆黑山低阶煤镜质组的分离及其微生物降解研究

利用重液离心法分离出新疆黑山低阶煤中的镜质组,采用土壤水微菌对低阶煤镜质组进行降解实验。通过偏光显微镜分析结果可知,镜质组的最佳分离密度区间为1.15~1.20 kg/m^(3),此区间内镜质组的富集产率达到92.50%。土壤水微菌降解镜质组的最佳工艺条件为:煤浆浓度0.60 g/50 mL培养基,菌液用量8 mL/50 mL培养基,降解时间13 d,此时降解率为24.35%。FTIR分析和XRD分析结果表明,微生物降解后,镜质组的脂肪烃、芳香烃吸收峰减弱,羧基和硝基的吸收峰消失,芳香层间距增加,芳香层数减小,说明镜质组中的有机大分子已被土壤水微菌降解为小分子。GC-MS分析结果表明,镜质组的液相产物中主要含有脂肪烃、芳香烃、酯类和胺类等小分子物质,其中脂肪烃类物质的含量最高。

湘南宝山铜铅锌多金属矿床石榴子石原位成分及其地质意义

宝山铜铅锌多金属矿床位于湘南钨锡多金属矿集区中西部,大地构造位置处于扬子地块与华夏地块两大构造单元的碰撞拼接地带。矿床中主要发育两类石榴子石,Ⅰ类石榴子石(Grt-Ⅰ)呈灰-灰绿色,具明显的韵律环带,Ⅱ类石榴子石(Grt-Ⅱ)呈棕红色或浅红色,环带不发育,较为破碎,呈脉状产出。本文利用激光剥蚀电感耦合等离子体质谱仪(LA-ICP-MS)分析了两类石榴子石成分,结果表明,Grt-Ⅰ主要富Fe,属于钙铁榴石(And_(91-93)Gro_(5-8)Spe+Pyr+Alm_(0.71-0.79));Grt-Ⅱ较Grt-ⅠFe含量降低,Al含量增加,以钙铝榴石组分增加为主要特征,属于钙铁榴石-钙铝榴石固溶体系列(And_(52-66)Gro_(32-47)Spe+Pyr+Alm_(1.10-1.37))。石榴子石稀土元素总量偏低(42.60×10^(-6)~201.50×10^(-6),不包括Y),Grt-ⅠΣREE、LREE/HREE值、δEu值高于Grt-Ⅱ,前者具强烈的Eu正异常、稀土配分曲线向右陡倾,而后者中等Eu负异常、稀土配分曲线向左平缓倾。两类石榴子石亏损Rb、Ba、Sr等大离子亲石元素,富集Nb、Zr和Hf等高场强元素,Grt-Ⅰ富集程度整体低于Grt-Ⅱ。两类石榴子石不同的端员组分、Eu异常等特征,指示Grt-Ⅰ富含Fe,且形成高氧逸度、碱性环境,Grt-Ⅱ形成于弱氧化-弱还原、弱碱性的环境,说明由Grt-Ⅰ至Grt-Ⅱ氧逸度逐渐降低,由氧化转变为弱氧化-弱还原环境。金属成矿元素Cu、Zn、Mo、Pb等在两类石榴子石中的含量较低,Sn含量却高达地壳中Sn平均含量(2.00×10^(-6))的几十甚至上百倍,指示深部石榴子石矽卡岩有利于Sn的富集,具成矿潜力。

滇西保山地块铁厂中新世花岗岩成因与构造意义

滇西保山地块新生代岩浆岩是理解印度-欧亚板块斜向碰撞带新生代构造演化和动力学背景的窗口。本文对保山地块铁厂地区中新世二云母花岗岩和含电气石二云母花岗岩开展了岩石地球化学、锆石U-Pb年代学和Hf同位素组成研究。结果表明二云母花岗岩和含电气石二云母花岗岩的岩浆锆石U-Pb年龄分别为18.1±0.1Ma和16.9±0.2Ma,反映岩浆岩形成于中新世。两类花岗岩具有高硅(SiO 2=73.7%~74.2%),富钾(K 2O=6.3%~6.7%,K 2O/Na 2O>1),且相对高碱(K 2O+Na 2O=8.8%~9.3%)的特征,属钾玄岩系列,为强过铝质S型花岗岩。两类花岗岩的CaO/Na 2O比值介于0.25~0.39,具有低Sr(56×10^(-6)~79×10^(-6))、低Ba(155×10^(-6)~211×10^(-6))、高Rb/Sr比值(4.6~6.2)特征。二云母花岗岩的锆石εHf(t)值为-12.1~-1.5。这些特征表明铁厂中新世花岗岩是变泥质岩脱水部分熔融的产物。结合同时代西南三江地区崇山剪切带淡色花岗岩和喜马拉雅淡色花岗岩的对比分析,表明铁厂中新世花岗岩可能形成于伸展构造环境。

滇西阿面根铅锌矿床成因研究——硫、铅同位素和闪锌矿微量元素证据

保山地块南部的芦子园地区是我国西南重要的铁铜铅锌多金属矿集区之一,阿面根铅锌矿床是该区近年来新发现的铅锌矿床,但目前研究程度低,成矿物质来源、矿床成因不明。本文在详细的野外地质调查和显微观察基础上,通过阿面根矿床的金属硫化物硫同位素、铅同位素探讨矿质来源,利用闪锌矿微量元素特征判定矿床成因。结果显示,阿面根矿床硫化物的δ~(34)SV-CDT值(9.44‰~12.16‰)介于壳源花岗岩硫与围岩地层同期海水硫之间,显示出二者混合特征;铅主要来自上地壳;闪锌矿以富集Fe、Mn、Co、Cu、Cd而贫Ga、Ge、As、Sn、Cr、Ni为特征,其中Fe、Cd、Mn、Co、Ag、Sb、Ga主要以类质同象形式产出,Cu则以类质同象和矿物包裹体的形式同时进入闪锌矿晶格中,可能存在Zn^(2+)↔Fe^(2+)、Zn^(2+)↔Cd^(2+)、2Zn^(2+)↔Ag^(+)+Sb^(3+)等方式的替代关系;闪锌矿微量元素组成特征与VMS型、MVT型、矽卡岩型和浅成低温热液型矿床中的闪锌矿明显不同,其Cd/Fe(0.02~0.04,均值0.03)、Co/Ni(15~1 019,均值1 275)和Ga/In(0.11~1.10,均值0.31)比值特征和较低的Ge元素含量均表明闪锌矿形成与岩浆热液关系密切。综上证据,本文认为阿面根矿床的成矿物质主要来源于深部隐伏中酸性侵入岩,有少量地层围岩物质加入。结合矿床地质特征,认为阿面根矿床属于岩浆热液充填交代型铅锌矿床。

保山烟区降水及其干旱风险性评价区划

以保山各县区2015—2020年11个烤烟气象站点的逐日降水量和气温数据为基础资料,对云南保山烤烟生长发育过程中降雨风险指标及其时空分布特征进行分析,并构建干旱危险性评价模型,旨在为保山烤烟安全生产及风险防范策略制定提供依据。结合地理信息系统软件ArcGis和气候倾向率、趋势系数等相关数理统计方法分析保山烟区降水和干旱风险的时空分布特征。采用层次分析法和干旱危险性评价模型,借助GIS平台实现保山烟区的干旱灾害危险性评价区划。结果表明:洪涝高风险地区主要集中在保山西部的龙陵和腾冲地区,龙陵年降水量在1060~1865.6 mm,腾冲年降水量在804~1348.5 mm,均大于烤烟正常需水量的2倍,其中腾冲猴桥地区气候倾向率最大,通过了0.01显著性检验,逐年上升趋势十分显著。烤烟旺长期干旱风险主要发生在保山中部和东部。施甸旧城和隆阳区附近的干旱风险最高,达到严重风险以上;保山中部和东部大部分地区干旱危险性风险都在中等风险以下,利于烤烟种植。本文研究阐明了保山烟区的水分气候条件对烤烟种植的重要影响,有利于保山地区烤烟优质生产及当地政府气象防灾减灾策略制定。

刘宝山教授运用扶正抑瘤法治疗淋巴瘤经验撷萃

刘宝山教授认为本虚标实为淋巴瘤的基本病机,以脏腑亏虚为本,痰瘀互结为标。汲取历代医家及现代中医大家治疗血液病之经验,提出以扶正抑瘤、攻补兼施为治疗大法,重在调理肝脾肾三脏。从临床中筛选出有效药物,自创扶正抑瘤方(生地黄、白芍、当归、川芎、红芪、黄精、龙眼肉、土贝母、夏枯草、卷柏、四季青、白花蛇舌草、天葵子、龙葵)为基础方,随症加减灵活运用。有效抑制淋巴瘤疾病进展,促进造血改善骨髓粒细胞、红细胞、白细胞三系血减少,使血象趋于稳定,脱离输血依赖。

保山咖啡产业现状及发展对策

保山是云南省重要的咖啡产区之一,其地理、气候条件非常适宜咖啡生长,咖啡种植历史悠久,但目前市场占有率和品牌影响力不高。本文分析了保山市咖啡产业发展现状和存在的问题,从提高生豆精品率、提高精深加工率、提高品牌影响力和市场占有率、培育壮大市场主体、精准的政策供给等方面提出了做强做大咖啡产业的建议,以期为当地咖啡产业高质量发展提供参考。