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western slope     
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  西部斜坡
     Analyzing action of slope break zone in western slope area, south of Songliao basin
     松辽盆地南部西部斜坡区坡折带作用分析
短句来源
     ANALYSIS OF THE CONTROLLING FACTORS ON SEQUENCE STRATIGRAPHY DEVELOPMENT IN DEPRESSION PERIOD IN WESTERN SLOPE OF SONGLIAO BASIN
     松辽盆地西部斜坡区坳陷期层序地层发育控制因素分析
短句来源
     Study on Slope Breaks of the Late Cretaceous Depression Basin Around the Western Slope in the Southern Songliao Basin
     松辽盆地南部西部斜坡区晚白垩世坳陷盆地坡折带研究
短句来源
     The amount of gas released from oil increases from east to west,it can be 12.82% of gas in free phase expelled from source rock,it is important part of gas accumulation in Western Slope.
     油溶释放气量可占到源岩游离相天然气排出量的12.82%,应是西部斜坡区天然气成藏的重要组成部分。
短句来源
     Major hydrocarbon migration pathway system in western slope zone of Songliao basin
     松辽盆地西部斜坡带油气运移主输导通道
短句来源
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  西斜坡
     Study on Reservoir Logging Interpretation Model for the Western Slope of West Depression in Liaohe Basin
     辽河盆地西部凹陷西斜坡储层测井解释模型研究
短句来源
     Subtle reservoir exploration practice on south section of western slope in Liaohe Western Sag
     辽河西部凹陷西斜坡南段隐蔽油气藏勘探实践
短句来源
     Analysis on accumulation conditions and characteristics of gas released from oil in Western Slope
     西斜坡地区油溶释放气成藏条件及特征分析
短句来源
     Characteristics and Genesis of the Western Slope Thick Oils in Songliao Basin
     松辽盆地西斜坡稠油特征及成因
短句来源
     Formation of heavy oil and correlation of oil-source in the western slope of the northern Songliao Basin
     松辽盆地北部西斜坡区稠油成因与油源关系
短句来源
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  西部斜坡区
     Analyzing action of slope break zone in western slope area, south of Songliao basin
     松辽盆地南部西部斜坡区坡折带作用分析
短句来源
     ANALYSIS OF THE CONTROLLING FACTORS ON SEQUENCE STRATIGRAPHY DEVELOPMENT IN DEPRESSION PERIOD IN WESTERN SLOPE OF SONGLIAO BASIN
     松辽盆地西部斜坡区坳陷期层序地层发育控制因素分析
短句来源
     Study on Slope Breaks of the Late Cretaceous Depression Basin Around the Western Slope in the Southern Songliao Basin
     松辽盆地南部西部斜坡区晚白垩世坳陷盆地坡折带研究
短句来源
     The amount of gas released from oil increases from east to west,it can be 12.82% of gas in free phase expelled from source rock,it is important part of gas accumulation in Western Slope.
     油溶释放气量可占到源岩游离相天然气排出量的12.82%,应是西部斜坡区天然气成藏的重要组成部分。
短句来源
     Calculation results indicate the amount of gas to released from oil is considerable. 1 m3 oil migrating from Qijia-Gulong sag to Western Slope can release 20-30 m3 gas.
     计算结果表明,西部斜坡区的油溶释放气量是可观的,1 m3原油从齐家—古龙凹陷运移至西部斜坡地区可释放出20~30 m3的天然气,且由东向西油溶气释放量逐渐增大。
短句来源
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  西部边坡
     THE CAUSE OF FORMATION AND COMPREHENSIVEADMINISTRATION OF SLIP MASS WITHIN 0~2 LINEAT WESTERN SLOPE OF YONGPING COPPER MINE
     水平铜矿西部边坡0~2~#线滑坡体的成因及综合治理
短句来源
     About 15 ten thouund cubic meters slip slope has occurred between 0-2 prospecting line's 202m and 298m at western slope of Yongping Copper Mine The boundary of slip mass was certained on the basis of serious analysis of slope mass for cause of formation, appropriate measures of comprehensive administer was adopted to prevent slopeMass further falling.
     永平铜矿西部边坡在1~2勘探线的202m标高至298m标高间发发生了约15万m3的滑坡,在分析滑坡体成因的基础上,判定滑体边界,采取相应的综合治理措施,制止了滑坡体的进一步下滑。
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  western slope
In this study an attempt is made to examine and analyse the mean characteristics of the katabatic flows at the western slope foot of a 1024?m high knife edge mountain using a meteorological tower and three surface meteorological stations.
      
Five sites were located on the western slope, each in a different vegetation zone, and three sites were selected on the eastern slope, each corresponding in elevation and vegetation type as closely as possible to three of the western sites.
      
Precipitation and surface waters in a high-elevation watershed on the western slope of the Colorado Rockies were studied over a three-year period.
      
Acid precipitation and surface-water vulnerability on the western slope of the high colorado rockies
      
vaseyana (Asteraceae), a widely distributed evergreen species of the Great Basin and the western slope of the Rocky Mountains, and Pentaphylloides floribunda (Rosaceae), a deciduous shrub limited in distribution to moist, high-elevation meadows.
      
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The symptom of the root rot of Korean pine is that, in the earlier stage the crown becomes yellow-green, thinned, and the needles slenderized, and later on, the whole crown turns blight yellow,the stump appears resin flow, swollen and rot. The root collar and root of trees produce fan-shaped, veined,white mycelial felts between bark aud wood. There are a lot of rhizomorphs inside and outside the root. The sapwood becomes spongy rot,when the trees are severely injured. From August to October the sporephores occur...

The symptom of the root rot of Korean pine is that, in the earlier stage the crown becomes yellow-green, thinned, and the needles slenderized, and later on, the whole crown turns blight yellow,the stump appears resin flow, swollen and rot. The root collar and root of trees produce fan-shaped, veined,white mycelial felts between bark aud wood. There are a lot of rhizomorphs inside and outside the root. The sapwood becomes spongy rot,when the trees are severely injured. From August to October the sporephores occur on stump, snag and seriously infect trees. The development oF disease on the south-western slopes is more serious than on the north-eastern, and so it is on the middle and the lower part of the mountain than on the upper part, too. Trees on low niches and moist land are subjected to the disease severely.Pathogenic fungi are obtained from the isolated culture of the sick root. Its colony and funiculus grow well on wort agar medium. At the end, the sporecarps occur in the bottle. Sporecarps are produced in abundance on the westage-wheat skin-urea medium. They seem honey yellow, caespitose and annulate. There are brown scales on the cap. Their spore print is white with light yellow, the gills a-e adnoto-decurrent,spore 6.5-9.9×4.3-6.8 micron, this pathogenic fungus is identified as shoestring fungus [Armillariella mellea (Vahl. et Fr.) Katrst]. The basidiospore from carpophore can infect Stub and weak wounded trees.The rhizomorphs grow actively and extend in the soil, and infect healthy plants.The bavistin has the better fungistatic action in the experiment of chemotherapy. The bavistin mixed with humuic acid-ammoniate, and lime,zineb,thiophanate and dry limes-sulphur give certain result.

红松根朽病的症状是初期冠希、色淡、针叶变细,后期全冠枯黄、干基肿大、流脂、溃烂,形成层有白色扇形菌膜,根部内外有大量菌素。树木严重受害时木质部边材呈海绵状腐朽。在伐根、枯死木及重病衰弱木上,8~10月可产生子实体。病害的发生阳坡重于阴坡,山中、下腹重于上腹。低凹潮湿的林地病重。由病根分离培养获得病原菌,其菌落、菌索在麦芽培养基上生长良好,后期在三角瓶内产生典型子实体,在木屑麦麸脲素培养基上产生大量子实体。子实体蜜黄色、丛生、具菌环,菌盖上有褐色鳞片,孢子印黄白色,菌褶贴生、延生,孢子6.5~9.6×4.3~6.8微米,经鉴定为蜜环菌[Armilla-riella mellea(Vahl.ex Fr.)Karst.]子实体上产生的担孢子侵染伐根和带伤的衰弱木,菌索在地下伸延侵染健康植株。药剂防治试验,多菌灵抑菌效果较好,多菌灵加腐植酸铵、熟石灰、代森锌、托布津、熟石灰加硫黄粉也有一定效果。

This work was made on the basis of data on the interpretation of false color den-site slicer, the fracture profiles, tectonite, fault gouge obtained from the investigations along the middle and southern segments of Tancheng-Lujiang fault zone as well as the studies of Quaternary active faults. Part of data cited here came from previous works on regional geology and geophysics. Some topics, such as the extension, deep geological features, tectonic movement, evolution history and current activity of these segments...

This work was made on the basis of data on the interpretation of false color den-site slicer, the fracture profiles, tectonite, fault gouge obtained from the investigations along the middle and southern segments of Tancheng-Lujiang fault zone as well as the studies of Quaternary active faults. Part of data cited here came from previous works on regional geology and geophysics. Some topics, such as the extension, deep geological features, tectonic movement, evolution history and current activity of these segments of the fault zone concerned in which the interest is growing, are dealt with in this paper.From our research results we come to a preliminary idea that the Tancheng-Lujiang fault zone in East China is a complex fault zone which has been undergoing a long tectonic activity and following intense reformation and that it is one of the main fault zones controlling the occurrence of strong earthquakes in East China. The constitution and deformation characteristics of both bottom and cover of this fault zone are sharply different each other on its opposing sides.The oldest trace showing the activity of this fault zone can be found in the Archaean Taishan Group being occurred in the host whithin this zone.The schitosity of Taishan complex along this zone shows an obvious local left-lateral drag which is also found in the Dabie Group (metamorphic series of rocks) along the SE foothills of Mt. Dabieshan. This explains the significant horizontal displacement along this fault zone during the Pre-Sinian period.From the Sinian period up to the Late Triassic period, in the Yangtse block fault running on the eastern side of this fault zone deposited marine sediments, while the north Jiangsu-east Shandong region was uplifting for a long time. From Late Protero-zoic to Early Cenozoic in the vast area west of this fault zone were developed North China type of marine sediments which were followed by the continental sedimentation.In the Mesozoic time the activity of this fault zone only occurred from the Indo-Chinese to the Yanshanian ages with the dominance of the latter. Judging by the met- amorphic series of rocks found on the northern foothills of Dabieshan and Jiaonan County, we can eatimate that the amount of displacement here is 520km in total. In fact it can be regarded as a resultant amount of displacements from lots of tectonic movements in the geological history, partly belonging to the Proterozoic, partly to the Hercy-nian and Indo-Chinese left-lateral strike-slip.The Himalayan movement probably caused the change of Tancheng-Lujiang fault zone activities in nature, from left-lateral displacement into right-lateral with thrusting movement. There ia an evidence that this fault zone was active in Cenozoic and shows a clear lineament on the satellite images with contrast shade. The other evidences are .as follows: the development of fault gouge with new stria and schistose texture and clastic materials. In addition, the geomorphological features and gravity anomaly also .show its tectonic activity during the Cenozoic period.The Cenozoic right-lateral strike-slip along this fault can be followed obviously, particularly on the Malingshan western slope, Tancheng County. And the right-lateral reversed phenomenan along this fault can be observed in the place where the small co-ombes run through the fault with the offset reaching 25m. As a result, the diabase vein formed in the Late Tertiary was offsetted and dragged by this fault. The solution of mechanism of earthquake also reveals the fact that the fault is still subjected to the right-lateral strike slip.The left-lateral, right-lateral as well as tensile and compressive displacements along the fault imply that throughout the long history of the Tanlu fault, the fault has had larger displacement. This may explain why the fault is such a prominent feature. This change of displacement as a function of time along major faults may de characteristic of intraplate deformation.

本文根据卫星影像、断层泥的分布和特征、重力资料、地震分布和震源机制资料以及其他某些地质资料,讨论了郯庐断裂带前震旦亚代以来的活动情况和现代活动性,并认为沿此断裂带现存达几百公里的左旋走滑位移量,应是地史上历次断裂运动的最终结果。指出了值得继续研究的课题。

The red pine bast scale, Matsucocous koraiensis Young et Hu, is a pest of Korean pine (Pinus koraiensis) widely distributed over the virgin forests in the eastern mountains of the Heilongjiang and Jilin provinces. In Fenlin district the Korean pine bast scale has one generation a year and overwinters in the 1st instar. After overwintering the 2nd inster larval stage is a chiefly injuring period. The adult emerges in early June and become abundant in mid-June. Reproduction is sexual, but we observed that one...

The red pine bast scale, Matsucocous koraiensis Young et Hu, is a pest of Korean pine (Pinus koraiensis) widely distributed over the virgin forests in the eastern mountains of the Heilongjiang and Jilin provinces. In Fenlin district the Korean pine bast scale has one generation a year and overwinters in the 1st instar. After overwintering the 2nd inster larval stage is a chiefly injuring period. The adult emerges in early June and become abundant in mid-June. Reproduction is sexual, but we observed that one of the females produced eggs before copulation. On an average, each female oviosits about 96 eggs. The young larva hatches in the later part of June and becomes abundant in mid-July. The Korean pine bast scale insects mainly in the virgin forest of the Korean pine distributed on the southern or south-western slope. Eight blocks of the younger pine plantation were recently investigated, but no bast scale was found. Some scale insects have been inoculated against the plantation, but whether they could overwinter or not must be determined by further observation. Aphislions and ants are the important natural enemies which considerably control the population density of this pest.

海松干蚧(Matsucocous koraiensis Young et Hu)是红松原始林的干部害虫,广泛分布在黑龙江省的小兴安岭、张广才岭和东部山区,以及吉林省的长白山区。海松干蚧在黑龙江省丰林林区1年1代,以1龄若虫越冬。越冬后,2龄若虫期是主要危害期。成虫出现在6月初,盛期为6月中旬,行两性生殖,但观察到一头雌虫在交尾前产卵。雌成虫平均产卵量为98拉。新若虫在6月下旬孵化,7月上旬未达盛期,随后选择细皮结构的寄主危害。海松干蚧主要发生在南坡、西南坡的红松原始林。作者调查了8块红松人工幼林,未发现此害虫。已将害虫接种到人工林,是否可以越冬需进一步调查。草蛉和蚁类是显著控制害虫虫口密度的重要天敌。

 
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