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shanxi     
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  山西
     Fruits and Seeds from Yunnan in the Age of Miocene and from Shanxi in the Age of Pliocene
     云南中新世和山西上新世果实和种子的研究
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     Study and Application on Animal Blue Tongue Disease in Epidemiology and Prevetment Technology in Shanxi Province
     山西动物蓝舌病流行病学及防控技术的研究与应用
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     The Reservoir Characteristics and Tectonic Influence of High Rank Coalbed Methane in Qinshui Basin, Shanxi Province
     山西沁水盆地高煤阶煤层气成藏特征及构造控制作用
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     Research on development strategy of forestry in Shanxi Province
     山西林业发展战略研究
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     From Shanxi Academy to Shanxi University (1902-1937)
     从山西大学堂到山西大学(1902-1937)
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  山西省
     Study on Agricultural Mechanization Development of Shanxi Province in the New Era
     新时期山西省农机化发展研究
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     Chinese Hawthorn Natural Resources in Shanxi
     山西省山楂资源现状
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     ODONATA (INSECT) Ⅰ.——A Survey of the Natural Enemy Insect Resources in Shanxi (2)
     蜻蜓目(昆虫纲)Ⅰ——山西省天敌昆虫资源调查(二)
短句来源
     STUDY OF DONGHE SAPROPELIC COAL IN PU COUNTY, SHANXI PROVINCE
     山西省蒲县东河腐泥煤研究
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     Odonata (Insect) Ⅱ……A Survey of the Natural Enemy Insect Resourccs in Shanxi (2)
     蜻蜓目(昆虫纲)Ⅱ——山西省天敌昆虫资源调查(二)
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     A Study of Key City and Regional Economy Development in South of Shanxi
     山西省南中心城市与区域经济发展研究──区域要素转换与重心转移分析
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     Seismic gaps-precursor for earthquakes(M_L≥5.0) in Northern Shanxi Province and its adjacent areas
     北及其附近地区M_L≥5.0地震的震兆──地震空区
短句来源
     ③ Relative to the Yanshan Hebei transition zone of differential movement, Yanshan unit shifts westwards 38° by north with a value of 2.4±1.3 mm/a and Shanxi Hebei Shandong unit moves eastward 35° by south with an amount of 2.3±0.9 mm/a.
     3相对于燕—冀差异运动转换带 ,燕山单元向西偏北 38°方向运动 ,量值为 2 .4± 1 .3mm/a,冀鲁单元向东偏南 35°方向运动 ,量值为 2 .3±0 .9mm/a;
短句来源
     Water Level Change and Reflecting Earthquake Ability of Well No.9-1 of Shanxi
     山西_(9—1)井水位变化及映震能力初探
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     ② Shanxi Hebei Shandong unit moves E40°S off the Ordos Yinshan unit and the magnitude is 4.4±1.0 mm/a.
     2冀鲁单元背离鄂尔多斯 -阴山单元向东偏南40°的方向运动 ,量值为 4.4± 1 .0 mm/a;
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  陕西
     ShanxiShanxi、 Liaoning、Jiangsu: B>O>A;
     山西、陕西、辽宁、江苏:B>O>A;
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     The quality parameters of the combined wastewater from the cider processing of Yitian Juice(Shanxi) Co. ,Ltd. are: CODCr≤4 300 mg/L,BOD5≤2 200 mg/L,SS≤1 500 mg/L,pH 4.5-10,temperature 30-40 ℃.
     伊天果汁(陕西)有限公司综合废水水质参数:CODCr≤4300mg/L,BOD5≤2200mg/L,SS≤1500mg/L,pH4.5 ̄10,水温30 ̄40℃。
短句来源
     Screen for IRF6 gene mutation in a Van der Woude syndrome family in Shanxi province
     一个陕西汉族Van der Woude综合征家系IRF6基因的突变筛查
短句来源
     Conclusion: 13 species in Sichuan, 9 species in Hubei, 8 species in Guizhou, 4 species in Hunan, 3 species in Guangxi, 2 species in Chongqing, 2 species in Yunnan, 1 species in Jiangxi, 1 species in Shanxi, 1 species in Jilin, 1 species in Liaoning and 1 species in Heilongjiang.
     结论:四川有13种、湖北有9种、贵州有8种、湖南有4种、广西有3种、重庆有2种、云南有2种,江西、陕西、吉林、辽宁、黑龙江各有1种。
短句来源
     CONCLUSION Distribution is listed as follows:9 species in Guizhou, 8 species in Sichuan, 5 species in Hubei, 4 species in Shanxi, 3 species in Hunan and 3 species in Chongqing.
     结论主要分布于贵州(9种)、四川(8种)、湖北(5种)、陕西(4种)、湖南(3种)、重庆市(3种)。
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      shanxi
    Division of afforestation site type in the watershed of Wangjiagou, West Shanxi through GIS
          
    Morphological variation of Quercus liaotungensis leaves in Lingkong Mountain, Shanxi province
          
    in Lingkong Mountain Nature Reserve of Shanxi region, five populations were included, and 24 morphological traits of leaf and apical bud were investigated.
          
    Water consumption of a single tree from the main afforestation tree species in Western Shanxi Province, a loess area
          
    The four were the main afforestation species in a loess area of western Shanxi based on the principle of water balance.
          
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    This article is in an attempt to demonstrate the“bamboo shoot”fossils at Yung-ninguan of Yenzhou prefecture recorded in“Dream Pool Essays”by Shen Kuo,one progressive politician as well as brilliant scientist in the Sung Dynasty.Actually,the fossils,which Shen Kuo thought to be of bamboo shoots are in paleontologicalsense,those of Neocalamites and the occurrence of fossils is now situated at Yanshui-guan,35 km.southeast of Yenchuan,Shanxi province.Taking into account the to-pographical features,the stratigraphical...

    This article is in an attempt to demonstrate the“bamboo shoot”fossils at Yung-ninguan of Yenzhou prefecture recorded in“Dream Pool Essays”by Shen Kuo,one progressive politician as well as brilliant scientist in the Sung Dynasty.Actually,the fossils,which Shen Kuo thought to be of bamboo shoots are in paleontologicalsense,those of Neocalamites and the occurrence of fossils is now situated at Yanshui-guan,35 km.southeast of Yenchuan,Shanxi province.Taking into account the to-pographical features,the stratigraphical sequences and the aspects of plant fossils inthe above-indicated region,we could not help admiring his round judgement on thefossils in some respects and his significant contribution to the development of paleon-tology.From his writing,we can see the episode of the political and ideologicalstruggle between the Confucian and the Legalist schools in the field of natural historyat that time.

    这是一篇关于宋延州永宁关“竹笋”化石考辨记实。据现在的延水关地形、地层和所采集的植物化石,作者肯定北宋进步的政治家、杰出的科学家沈括论述“竹笋”化石的正确方面,兼谈他在古生物学上的历史贡献,反映了宋朝时期儒法两条政治思想路线在自然科学领域里的斗争。

    The foraminifera described and figured in this paper were collected from theChanghsing formation in Western Guizhou.They were found together with Palaeofu-sulina and Brachiopods in calcareous siltstone and light grey limestone.12 generaand 13 species(including 7 new species)are here listed below:Nodosaria delicatasp.nov.,Lingulina strigata sp.nov.,Frondicularia inflata(K.M.-Maclay),Colaniellanana K.M.-Maclay,Colaniella cylindrica K M.-Maclay,Geinitzina tcherdynzevi K.M.-Maclay,Padangia cf.perforata Lange,Pachyphloia...

    The foraminifera described and figured in this paper were collected from theChanghsing formation in Western Guizhou.They were found together with Palaeofu-sulina and Brachiopods in calcareous siltstone and light grey limestone.12 generaand 13 species(including 7 new species)are here listed below:Nodosaria delicatasp.nov.,Lingulina strigata sp.nov.,Frondicularia inflata(K.M.-Maclay),Colaniellanana K.M.-Maclay,Colaniella cylindrica K M.-Maclay,Geinitzina tcherdynzevi K.M.-Maclay,Padangia cf.perforata Lange,Pachyphloia pigmobesa sp.nov.,Hemigordiusplautus sp.nov.,Agathammina ovata sp.nov.,Multidiscus semiconcavus sp.nov.,Neo-discus qinglongensis sp.nov.and Robuloides acutus Reichel.So far as the faunal featuresis concerned,the genera Colaniella and Robuloides are known to be widely distributedin the Tethyan region.The genus Colaniella may be regarded as one of zonefossils for the Changhsing limestone in Sichuan,Shanxi,Jiangxi and Hunan of China.Frondicularia inflata(K.M.-Maclay),Colaniella nana K.M.-Maclay,Colaniella cylind-rica K.M.-Maclay and Geinitzina tcherdynzevi K.M.-Maclay,etc.have been knowncommonly from the Upper Permian of N.Csucasus,U.S.S.R..Robuloides acutus Rei-chel has been reported from the foraminiferal limestone of Greece.Accordingly,theforaminiferal fauna from the Changhsing formation in Western Guizhou,accepted asbelonging to late Upper Permian in age,may be correlated with that from the Nikitinformation in N.Caucasus.

    本文描述的有孔虫化石计12属、13种,其中包括7新种。多数化石是根据分离出来的完整壳体和做定向切片的观察和研究的。讨论了Angulodiscus 和Multidiscus 两个属的归属,并讨论了含有孔虫化石的地层时代应属晚二叠世。

    The specimens described in this paper were collected at Hongyantou in the Yushedistrict and at Shengzhuang in the Pingyao district of Shanxi Province.FromHongyantou the following fossil plants have been found:Pleuroneia sternbergi(Muenster),Pl.rossica Neuberg,Yuccites? sp.,Voltzia sp.(male cone),Neocalamites sp.and Equisetites sp.,while those from Shangzhuang are:Pleuromeia sternbergi(Muens-ter),cf.Anomopteris mougeoti Schimper,Samaropsis sp.and Neocalamites sp.The plant-bearing beds of the above-mentioned...

    The specimens described in this paper were collected at Hongyantou in the Yushedistrict and at Shengzhuang in the Pingyao district of Shanxi Province.FromHongyantou the following fossil plants have been found:Pleuroneia sternbergi(Muenster),Pl.rossica Neuberg,Yuccites? sp.,Voltzia sp.(male cone),Neocalamites sp.and Equisetites sp.,while those from Shangzhuang are:Pleuromeia sternbergi(Muens-ter),cf.Anomopteris mougeoti Schimper,Samaropsis sp.and Neocalamites sp.The plant-bearing beds of the above-mentioned localities are generally consideredas belonging to the Heshangkou formation,i.e.,the upper part of the so-called“Shi-chienfeng series”or the Shihchienfeng series used in the wide sense of North China.Owing to the scarcity of biota remains the geological age of the Heshangkou formationhas long been a subject of dispute.It seems acceptable,however,to refer to it asearly Triassic,as a result of discovering the most characteristic plant Pleuromeiasternbergi in the formation.The specimens assigned to Pleuromeia are so rich in number and good in preser-vation as to be capable of our accurate determination.At first glance,there is aresemblance between Pleuromeia sternbergi and Pl.rossica in the general habit.Thelatter species differs,however,distinctly from the former in its relatively smaller sizeof the trunk,in its bisexual strobilus with a long pedicel instead of sessile unisexualone,and in its smaller mega-and microspores,etc.Besides,there is a distinction be tween the imprints of sporophyll-scars preserved on the strobolus-axis of the twoforms.The present writers agree with Konno's(1973)view that the genus Pleuromeiarepresents one of the large tribes of the Lycopsida.It is more than probable thatPleuromeia rossica might represent another type of Pleuromeia-like plant which seemsto be generically distinct from Pl.sternbergi.Of great interest is that the most important middle-upper Bunter Sandstone spe-cies.Pl.sternbergi,occurs in the Heshangkou formation from Hongyantou,Yushe,inassociation with Pl.rossica.The latter species has first been described by Neuberg(1960)from early Triassic strata of the Russian platform.The plant-bearing stratahas later been considered by Lozovsky(1973)to be lower-middle Olenekian in agewhich corresponds only slightly earlier to that of the middle-upper Bunter Sandstoneof Germany.The age of the Heshangkou formation is therefore regarded preferablyfor the present as the lower-middle Olenekian stage.

    本文描述了在山西沁水盆地和尚沟段地层新发现的两种肋木化石(Pleuromeia sternbergi,Pl.rossica)及有关的一些茎和根托标本,这在国内尚系首次报道,并据此对华北早三叠世的地层问题进行了讨论。

     
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