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The Liushuigou intermediate-basic meta-igneous complex at Guanzizhen, Tianshui, is composed mainly of metagabbro-metagabbro diorite-metadiorite, and the Baihua basic meta-igneous complex consists mainly of pyroxenite-gabbro-diorite-quartz diorite. They form a relatively complete comagmatic evolutionary series.

提要:天水地区关子镇流水沟变质中基性岩浆杂岩主要由变质辉岩—辉岩—闪岩组成,百花变质岩浆杂岩主要由辉石岩—辉岩—闪岩—石英闪岩组成,构成较完整的同源岩浆演化序列。

Spikelets oblong to gaping, shining, laterally compressed, florets 2–3(–5), disarticulating below each floret; rachilla pilose, extended beyond uppermost floret; glumes lanceolate to oblong, subequal,± equaling spikelet, membranous, shining, keeled, lower glume 1-veined, upper glume 1–3-veined; floret callus small, pubescent to conspicuously bearded; lemmas lanceolate to oblong, hyaline to shiny cartilaginous, back rounded, finely 4-veined (5th midvein extended into awn), glabrous, awned from near base or in lower half, apex membranous, broad, 4-toothed or denticulately truncate; awn straight or weakly geniculate, usually not exserted from spikelet; palea hyaline, subequal to lemma.

小穗圆形为了张口,发亮,侧面压扁,小花2-3(-5),在每小花下面脱节;小穗轴具柔毛,在最重要的小花以外延;披针形的颖片到圆形,近等,多少等,膜质,发亮,龙骨状,下部颖片1脉,上面颖片1-3-脉;小花结茧小,青春期对显著公然反对;外稃披针形的到圆形,对发亮软骨透明,背面圆形,好4脉(中脉第5 延伸进芒),从小穗直或者身体虚弱膝曲,通常不外露的芒;透明的内稃,近等于外稃。

So the meta-granitoids can he recognized and separated from the metamorphic sequences. They are grouped as the Meoproterozoic-Neoproterozoic gneissoid granite-monzogranite-granodiorite, with their isotope ages of 953.4 Ma to 1450 Ma, and the Sinian schistostose quartz monzogranite diorite.

主要成岩期及代表性岩类有:晚元古代为片麻状正花岗岩-二花岗岩-花岗闪岩,同位素年龄为953.4~1450Ma;震旦纪为片理化石英二岩-石英闪岩,同位素年龄为547Ma。

But the value of H angle is smaller than class I malocclusion . Campared with the data of class II malocclusion , for class III malocclusion there are significant differences in LsL , LiL , lower lip angle of inclination , mentolabial sulcus angle , H angle , upper lower lip angle , Ns-Sn-Ls . For class III malocclusion the value of LsL is shoter than class II malocclusion , but the value of LiL is longer than class II malocclusion . The value of lower lip angle of inclination , mentolabial sulcus angle , upper lower lip angle is bigger than class II malocclusion .

安氏Ⅱ类错合患者与安氏Ⅲ类错合患者相比,在上唇、下唇、上唇倾角、下唇倾角、颏唇沟角、H角、上下唇角和软组织轮廓这些指标有显著性差异;安氏Ⅱ类错合患者的上唇比安氏Ⅲ类错合患者的、安氏Ⅱ类错合患者的下唇比安氏Ⅲ类错合患者的短;安氏Ⅱ类错合患者的上唇倾角和H角比安氏Ⅲ类错合患者的大,安氏Ⅱ类错合患者的下唇倾角、颏唇沟角和上下唇角比安氏Ⅲ类错合患者的小。

We found out one kind of new orange-red long afterglow material La2O2S: Eu3+, Mg, Zr.2 In the phosphor Gd2O2S, Mg, Ti which was prepared by high-temperature solid-state method, the orange afterglow phenomenon can be seen after illuminated with UV light.3 Using the high-temperature solid-state method, Gadolinium oxysulfide phosphors doped with rare earth ions were synthesized. We can observe the red or orange phosphorescence in Gd2O2S doped with Eu3+, Sm3+, Tm3+, Yb3+, Dy3+, Er3+, Nd3+or Ho3+. This is a new result of the long afterglow phosphors research.4 Using the microwave radiation method, the new Sm3+ doped gadolinium oxysulfide phosphor, which has the orange-red long afterglow emission after illuminated with UV light or visible light, was synthesized for the first time.5 In fluorescent materials YOX doped with europium ions, the long afterglow phenomenon wasnt observed but the blue luminescence of Eu2+ and red luminescence of Eu3+ are simultaneously examined. This is a new result of the valence stability and change of Eu2+ in yttrium oxyhalide .We systematically studied the effects of the host, addition agents and reaction atmosphere on the valence change and fluorescence property of europium ions.

经过系统的研究总结得到以下的结论与成果: 1采用高温固相反应法合成了一系列稀土离子掺杂的硫氧化镧发光粉,发现了该体系中Eu~(3+)的余辉发光,从而得到一种迄今未见文献报道的红色余辉发光材料:La_2O_2S:Eu~(3+),Mg,Zr; 2在Gd_2O_2S,Mg,Ti磷光粉中观察到橙色的余辉发光现象; 3采用高温固相反应法合成了一系列稀土离子掺杂的硫氧化钆磷光粉,在掺杂Eu~(3+)、Sm~(3+)、Tm~(3+)、Yb~(3+)、Dy~(3+)、Er~(3+)、Nd~(3+)、Ho~(3+)的Gd_2O_2S中观察到红色和橙色余辉发光; 4首次采用微波法合成了Gd_2O_2S:Sm~(3+),Mg,Ti磷光粉,该磷光粉经紫外或可见光激发后呈现明显的橙红色余辉发光; 5在YOX中同时观察到Eu~(2+)和Eu~(3+)的发射,系统研究了基质、添加剂及反应气氛对Eu价态和发光的影响。

The data of skull morphology on Manis pentadactyla and Manis javanica were reported in this paper, which involved the measurement and comparison of skull variables of the 2 species.

被测定的指标主要有颅全、基底、腭、眶间宽、后头宽、鼻骨、鼻骨宽、脑颅高、听泡和下颌,并且在这两个物种之间进行了比较。

The original defined adakitesare sodium igneous rocks, they are tonalite, trondhjemite or (plagioclase-rich) granodiorite in whole-rock chemistry; however, the K-rich "C-type" adakite defined by Chinese scholars are potassic igneous rocks, they are granite, quartz monzonite and (alkali feldspar-rich) granodiorite, etc.

最初定义的埃达克岩是钠质火成岩,其全岩化学成分相当于英云闪岩、奥花岗岩和花岗闪岩;而富钾的&C型埃达克岩&全岩化学成分相当于花岗岩、石英二岩和花岗闪岩。

For the problem of the ratio of inner to outer diameter of long tube, according to the "residual core" in the target plays an important role in DOP of long tube penetrator, the analytical model of long tube pentration in semi-infinite homogeneous steel target is established and calculated to devide three kinds of different scopes, the rule of varied by the ratio of inner to outer diameter is analyzed. The patterns of penetration of the yawed tubular against a normal homogeneous semi-infinite target is established, the size and direction of "residual core" is analyzed, under the different impact yawed, the regularity of variations in the yawed of the tube and depth of the penetrateion is described during the penetrateion against the plate.

二是对于管体的不同内外径比,依据管体时形成的中间&靶芯&是其侵彻机理不同于杆体的重要因素,分三种情况建立了管体对半无限均质靶板的简化理论模型,并进行了分析,得出了穿深随内外径比变化的规律;描述了带攻角管体垂直侵彻半无限厚靶的物理图像,分析了&靶芯&力的大小和方向,建立了侵彻简化模型,给出了在不同的初始攻角条件下,管体在侵彻过程中攻角和穿深的变化规律。

Inflorescence profusely branched, umbels numerous, small, 1–2 cm across, lax; bracts 2–4, lanceolate or elliptic, 3–6 × 1–2 mm, unequal, 5–7-nerved; rays 2–5(–7), 0.5–2 cm, unequal, very slender; bracteoles 5, lanceolate or elliptic, 3–4 × 1–1.5 mm, equal, 3-nerved, apex apiculate, equaling or slightly longer than flowers; umbellules 1–1.3 mm across, 5–11-flowered; pedicels 0.5–1.5 mm.

花序大量分枝,伞形花序多数,小,1-2厘米直径,疏松;苞片2-4,披针形的或椭圆形, 3-6 * 1-2 毫米,不等,叶脉;伞辐2-5(-7),0.5-2厘米,不等,非常纤细;小苞片5,披针形或者椭圆, 3-4 * 1-1.5 毫米,等,3脉,先端具细尖,稍或近等花;小伞形花序1-1.3毫米直径,5-11开花;花梗0.5-1.5毫米。

Basal leaves rosulate, persistent; petiole to 6 cm; leaf blade oblong or oblong-spatulate, rarely linear-oblong,(0.3-)0.6-1.7(-1.9) cm × 1.5-4 mm, densely tomentose with 4-6-rayed stellate trichomes 1 or more rays of which forked or with a lateral branch on each side, base attenuate or cuneate, margin entire, apex obtuse. Cauline leaves absent or rarely 1, sessile; leaf blade oblong, tomentose as basal leaves, margin entire, apex obtuse.

基生叶莲座状,宿存;叶柄达6厘米;叶片圆形或圆形匙形,很少线状圆形,(0.3-)0.6-1.7(-1.9)厘米×-4毫米,密被绒毛具4-6伞辐星状毛1或更多伞辐那分叉或具侧枝在每边,茎生叶缺席的或很少1,无柄;叶片圆形,象基生叶一样被绒毛,边缘全缘,先端钝。

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