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According to the distribution of species and amount, the author makes a PCA analysis to the different habitats. The analysis of hierarchical cluster to different habitat is according to the distribution of species. According to the results of the two ways of analysis and the factual condition of environment, the environment of Daqinggou is divided into 3 types of habitat that are described as the hygric plant community in the bottom of ditch, xerophytic plant community in the top of ditch and single type plant community.

以直翅目昆虫种类和数量的分布为属性对不同生境作PCA分析并以直翅目昆虫种类分布为属性作等级聚类分析,两种分析方法所得结果十分相似,结合分析结果和实际情况将大青7种不同生境分为3类,分别命名为底湿生植物群落,包括水曲柳植物群落、湖边湿地植物群落和稻田植物群落;上干早植物群落,包括沙丘草地和大果榆植物群落;单一型植物群落,包括人工针叶林植物群落和蒙古栋植物群落。

In the soft tissue measurements, the value of soft tissue facial angle and B'-Pos-FH in the first extraction group was less than those in the second extraction group significantly. After treatment all the patients had an increase in S-Ns-Pos angle, soft tissue facial angle, B'-Pos-FH and depth of mentolabial groove. At the same time, soft tissue convexity angle was diminished obviously. But the change was not significant between the two premolar extraction groups.

2在对软组织项目的测量中,治疗前第一前磨牙拔除组的软组织面角、颏倾角均小于第二前磨牙拔除组,治疗后2组均出现软组织面凸角减少,颏凸角、软组织面角、颏倾角、颏唇深度增加;但2组在各项测量项目的变化上无显著组间差别。

Based on isotopic ages and the cycle of magamtism, the ages of Yanbian granites can be subdivided into five periods:①late Permian granites (260-245Ma), the typical plutons are Liukesong and Liangbing plutons, and the main rock type include diorite-monzonitic-K syenogranites;②Triassic granites (225-200Ma), the typical plutons are Sandaogou, Chunyang, Qishiergedingzi, Dahuanggou, Naozhi, and Qinglinzi plutons, the main rock type include quartz dioritesgranodiorites-monzonitic-alkali granites;③early Jurassic granites (190-180Ma), which composed of quartz diorites-granodiorites - monzonitic ,and the typical plutons are Shimen, Miantian, Daxinggou and Yushuchuan rock;④Middle-Late Jurassic (170-150Ma), which composed of granodiorites- monzonitic- garnet-bearing muscovite granites, the typical plutons are Huangniling, Weizigou, Loutuoshan and Dongqing rock;⑤early Cretaceous (about 130Ma), the typical pluton is Zhongping pluton, and its rock type is paulite diorite.

另外,根据同位素年龄和岩石组合并考虑到岩浆的旋回性,将延边显生宙花岗岩进一步划分为五个期次:1。晚二叠世(260-245Ma),代表性岩体为六棵松和亮兵,主体岩性为辉石闪长岩、二长花岗岩和钾长花岗岩;2。三叠世(225-200Ma),代表性岩体为三道、春阳、七十二个顶子、大荒、闹枝、青林子,岩石组合为石英闪长岩—花岗闪长岩—二长花岗岩—碱长花岗岩,以花岗闪长岩和二长花岗岩为主;3。早侏罗世(190-180Ma),石英闪长岩—花岗闪长岩—二长花岗岩组合,主体岩性为花岗闪长岩,代表性岩体有石门、棉田、大兴、榆树川等;4。中侏罗世(170-150Ma),主体岩性为花岗闪长岩和含石榴石花岗岩,代表性岩体有黄泥岭、苇子、骆驼山、东清5。

Early Paleozoic massive sulfide deposits of ophiolitic type in North Qilian Mountains are distributed mainly in areas of Early and Middle Ordovician basic volcanic and volcano_sedimentary rocks.

文章主要论述了北祁连山西段石居里矿田内Ⅵ号、Ⅷ号、九个泉等矿床的基本地质特征,并与北祁连山东段老虎山地区银硐、猪嘴哑吧等矿床对比。

However, relating to investigate the modes, courses and characteristics of the orogenetic process in Paleozoic and after orogenetic process, the cognitive divergence have still occurred.

通过对新疆北东部地区不同构造区带构造作用的方式、过程和特点的研究,确定:①南天山榆树高压麻粒岩地体的正变质原岩是一个基本完整的蛇绿岩套,其经历了俯冲至下地壳的高压麻粒岩相、构造抬升至深地壳麻粒岩相以及快速构造折返至角闪岩相的变质过程,代表了南天山洋壳俯冲、变质、随后折返的过程,并首次确定了变质过程的PTt轨迹;②奥陶纪末期中天山北缘发生洋盆俯冲、地体增生作用,此时萨日达拉地区处于岛弧活动带;中石炭世晚期中天山小型洋盆关闭,准噶尔地块与伊犁—中天山板块斜向对接随后发生脆韧性质近水平高温低速右行走滑剪切;③根据巴音地区不构成蛇绿岩套有效成分的硅质岩具有与活动大陆边缘密切相关的地球化学特征以及洋中脊玄武岩显示其岩浆源区受到消减带流体交代作用的影响,结合区域地质资料,首次提出巴音蛇绿岩带所代表的洋盆古构造环境为弧后盆地,并于早石炭世至中石炭世末期间,经历了扩张、收缩和闭合过程;④首次在克拉麦里蛇绿混杂岩带中分解出具有N-MORB、T-MORB与OIB三种不同类型的火山岩岩石组合,反映了洋盆俯冲

Maturity of Lower Cretaceous source rock, researched by the authors, is closely relative to the deposition thickness of the Tertiary and the Quaternary. It shows that source rock at the depth of 4,000-4,400m is low mature, and 4,400-5,200m is in the peak of oil generating. Correspondingly, the source rock of the Zhonggou Formation is immature; the Upper Xiagou Formation is low mature; and the Lower Xiagou Formation and the Upper Chijinpu Formation are in the peak of oil-generating; and the Lower Chijinpu Formation is at the stage of generation of condensate-wet gas with high maturity. There is no source rock reaching the overmature stage of dry gas at present.

可溶有机质转化率、镜质体反射率、热解、生物标志物特征等参数表明:青南凹陷中部的下白垩统烃源岩生油门限深度为4000m(相应的镜质体反射率为0.65%),埋深4000~4400m为低成熟阶段,埋深4400~5200m为成熟生油高峰阶段,因此中组烃源岩未成熟,下组上部烃源岩低成熟,下组下部和赤金堡组上部烃源岩处于成熟生油高峰阶段,赤金堡组下部烃源岩处于高成熟的凝析油—湿气阶段,目前尚无烃源岩达过成熟干气阶段。

These samples provided us widi data on the ability of the soil to adequately supply the crop with needed nutrients for normal plant growth and the nutritional status of the peai trees themselves.

而 P、K的含量,厢面为 253 ms Ks'、314 ms Ks',厢为143 ms K合'、168 ms K合'。七月份的样品分析结果呈现相似的变化。N的含量厢面、厢分别为 903 mg Kg叫、730 mg Kg叫。P和 K的含量厢面、厢分别为185 mg Kg'、306 mg Kg'和 122 mg Kg-'、295 mg Ks-'。

Precentral gyri thickness more big postcentral gyri in 93 cases.The mean ratio of percentral/postcentral gyri was 1.736 for left hemisphere and 1.652 for right hemisphere.The superior frontal sulci with precentral sulci intersect in 80 cases.At 31 with brain lesion's patients,MR findings with clinical symptom had same location in the brain gyri.

结果 明确判定中央位置98例,中央前回的厚度大于中央后回的93例,中央前回与中央后回厚度之比左侧半球:1.736,右侧半球:1.652;额上与中央前相交的80例,31例患有脑内疾病的磁共振影像病变的位置与临床神经定位是相一致的。

This process put the anaerobic tank and secondary settlings and the recirculation of nitrified wastewater and the recirculation of sludge and Orbal oxidation ditch inyto together at the basement of Orbal oxidation ditch and the secondary settlings which the inlet and outlet were both circumjacent. This process had many advantages such as the small taking-up area and lower investment and consuming of energy and strong adaptability to raw influent.

介绍了一种新型一体化Orbal氧化,该池以Orbal氧化和周进周出辐流二沉池为基础,将厌氧池、二沉池、硝化液回流、污泥回流系统与Orbal氧化组合为一体,具有占地面积小、投资省、能耗低、原水适应能力强、运行管理更方便的突出优点。

From high resolution RS image of study area, gully head locations and land use information can be extracted, by performing overlay analysis on gully head locations map and flow accumulation map, slope gradient map, the slope and upslope drainage area of each gully head can be obtained.

采用的方法是RS技术与GIS技术相结合的方法,利用高分辨率卫星影像提取研究区内所有切头位置和土地利用状况,将头位置与研究区的水流汇流网络图、坡度图作叠加分析,得到切头的坡度和上游汇水面积。

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