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Male flowers: pedicels long and slender; sepals 4-7, imbricate, margins entire or serrulate; petals absent; disk of 4-7 segments, these sometimes connivent or fused; stamens 4-7, inserted at base of disk, longer than sepals; filaments free; anthers 2-locular, erect, extrorse, longitudinally dehiscent; pistillode small, 2- or 3-lobed.

雄花:花梗长和纤细;萼片4-7,覆瓦状,边缘全缘或有细锯齿;花瓣无;花盘4-7裂,有时靠合或愈合;雄蕊4-7,着生于花盘基部,长于萼片;花丝离生花药2室,直立,外向,纵向开裂;退化雌蕊小,有叶2或3。

Results 6 patients with PAP presented with ground-glass opacification of the bilateral lungs on HRCT. Typical chest HRCT scan showed "map-like" lesions in 3 cases and "cobble stone-like" lesions in 3 cases. Multifocal consolidative opacities in the lungs were seen on HRCT in 3 cases. Lung biopsies from 6 patients with PAP revealed a prominent positive periodic acid-Schiff intra-alveolar exudates. There were normal alveolar spetasis in 3 patients while interstitial thickening, fibroblast hyperplasia, interstitial fibrosis in the others.

结果 6例患者在不同层面可见磨玻璃影,其中2例可见小结节影;3例表现为两肺斑片状磨玻璃影与周围肺组织分界清楚,呈地图样改变;3例因磨玻璃影与小叶间隔增厚交织成铺路石样改变;3例可见肺泡实变融合成密度较高的斑片状阴影,1例在肺泡实变区可见&空气支气管征&。6例患者活检肺组织在光镜下显示肺泡腔内充满大量块状或颗粒状嗜伊红物质,PAS染色阳性,AB染色阴性,其中3例肺泡间隔正常,3例肺泡间隔增宽,可见慢性炎性细胞浸润、成纤维细胞增生和胶原沉积。

Stem leaves petiolate, petioles ca. 10 cm; sheaths broadly ovate, 2.5–4 cm, purple-red adaxially, densely white-setose abaxially; blades triangular-oblong, 10–15 × 5–7 cm, 3-pinnate; pinnae 5–7 pairs, only basal pinnae short-petiolulate; ultimate segments obovate or oblanceolate, 3–5 × 2–3 mm, setose along nerves abaxially, entire or 2–3 toothed, cuspidate at apex.

茎生叶具叶柄,叶柄约厘米;鞘宽卵形,正面2.5 -4厘米,紫红色,密被白色具刚毛;叶片三角形的长圆形, 10-15 * 5-7 厘米,3回羽状;羽片5-7 对,只是基本的羽片短的小叶柄;末回裂片倒卵形或倒披针形, 3-5 * 2-3 毫米,具刚毛沿着叶脉背面,全缘或齿状,骤尖在先端。

Plants 50–80 cm; bracts usually 4; bracteoles 5, equaling or slightly exceeding the flowers.

植株50-80厘米;通常的苞片4;小苞片5,等于或者稍微地超过花。

Mm, widened at apex. Spikelets 4–8 × 1–1.5 mm, yellowish brown or purplish brown; lower glume absent; upper glume lanceolate-oblong to narrowly oblong with slightly falcate apex, obscurely 7–11-veined, midvein usually shortly excurrent; lemma lanceolate-oblong, 3–4 mm, 1-veined; palea absent.

小穗 4-8 * 1-1.5 毫米,黄棕色或带紫色棕色;更低的颖片无;上面颖片披针形长圆形到狭长圆形具稍镰刀形先端,不明显脉,中脉短通常;外稃披针形长圆形,3-4毫米,1脉;内稃缺席。

Flowers 12–13 mm in diam.; pedicel ca. 1 mm; bract 3- or 4-parted with segments fasciated; bracteoles in 1 pair, ovate, margin 3-serrate.

花12-13毫米直径;花梗约1毫米;苞片3或4与分别裂片;小苞片在1 对内,卵形,边3使成锯齿波。

Perianth segments not connate into a tube, without an acicular appendage; axil of bractlets glabrous or ± hairy, but hairs not fascicular.

花被片并非合生成筒,没有一件针状的附加物;无毛的小苞片腋或者有毛的±,但是头发而不是束状。

The steps are as the following:1、Preparing the cerebrospinal fluid one hour before the experiment,take some of them for cryopreservation;2、Without paralyse,cuting down the rat head quickly and dislodge the hippocamp part which is used in the experment in freezing liquid,and trim the hippocamp distrct.3、Fixing the hippocamp tissue on the vibratome,to cut down a brain slice with 300μm,use the haustorial tube to move the slice to the preincubate dish,cultivanting it for one hour.Then move it to the record incubation chamfer.4、Preparing the glass micloelectrode and fill it with NaCl,the corcentation is 3mol/L.5、adjusting the recorder,after cultivate the brain slice in the incubation chamfer for 2 hours,the expermentize can be gone on.6、In order to ensure the accurate of the experimental result,use only one medicine concentration for one brain slice in every experiment.

本实验研究方法是:1、实验前1小时配制好所需脑脊液并充以95% O2和5% CO2的混合气,取小部分冷冻保存;2、在乙醚麻醉下,快速断头并在冷冻液里取出包含海马的大脑部位,修整出所需海马区;3、将海马组织固定于振动切片机上切出300μm厚的海马脑片,用广口吸管转移至预孵育皿培养一小时,后再转移到记录用孵育槽内;4、拉制好玻璃微电极,并充以3mol/L的NaCl;5、调试好记录仪器,将脑片在孵育槽内培养2小时后进行实验;6、为了保证实验结果的准确性,每一块脑薄片只进行一个浓度的药品实验。

Flowers axillary, 2 or 3 in a cluster, rarely solitary. Pedicel 0.6-1.5 cm, often recurved, densely hirsute; bracteoles caducous. Sepals broadly ovate, 5-14 mm, outside densely ferruginous hirtellous, apex acute.

花梗 0.6-1.5厘米,经常下弯,密被长硬毛;小苞片早落宽卵形的萼片,5-14毫米,外面密被铁锈色具微糙硬毛,先端锐尖的。

According to the variation in the components of intermediateacid igneous rocks coming from the lower crust, it is possible to restrain the depth of the source area and the minimum thickness of the crust, and thus to provide important information for the study of the deep process of the continental intraplate mineralizationGlobally, many world level porphyry copper deposits and metallogenic systems formed by hypabyssal hot liquid have their close relationship with the synchronous adakite in spacetime and genesis; domestically, the adakitelike rocks have been identified to be related to the metallogenesis in the main metallogenic areas in ChinaThe recognition of adakitelike rocks having no relationship with the process of subduction makes it possible to construct a metallogenic model of continental intraplate porphyry metal deposits by combining other geological evidences, and this model is totally different from the metallogenic model of porphyry copper deposits with Bsubduction setting constructed by Sillitoe (1972)The existence of adakitelike rocks may be the necessary condition but not the sufficient one for forming the largescale porphyry deposits and the hypabyssal hotliquid deposits, whose metallogenic elements mainly came from the mantleThe metallogenic potential of adakitelike rocks is achieved by the entering of the mantle material, and the metallogenic specialization of adakitelike rocks is decided by the distribution characteristics of the metallogenic elements in the upper mantleAn important reason for the adakitelike magma related to subduction being advantageous to mineralization is that there were abundant high pressure and high temperature liquid coming from the subducted platepieces and the magma of high fO2 coming from the melting of subducted platepiecesHowever, for those adakitelike rocks, whose occurrence has continental plate background but does not relate to the subduction, their metallogenic mechanism is not clear yetBased on the concept of modern mineral exploration and combined with the analysis of integrated geological information, we may better realize the practical prospecting significance of the adakitelike rocks

根据起源于下地壳的中酸性岩浆岩的成分变化,可以约束其源区深度以及地壳最小厚度,为大陆板内成矿作用的深部过程研究提供重要信息。全球范围内,许多世界级斑岩铜矿和浅成热液矿化系统与同期的埃达克质岩存在密切的时空与成因联系,在国内主要成矿区带也识别出与金属成矿作用有关的埃达克岩。与俯冲过程无关的埃达克质岩的识别,使我们有可能结合其他地质证据构建完全不同于Sillitoe(1972)B型俯冲环境的斑岩铜矿成矿模式的大陆板内斑岩型金属矿床成矿模式。对于规模巨大、矿质主要源自地幔的热液矿床的形成,埃达克岩可能是必要条件,但不是充分条件。埃达克岩的成矿潜力通过地幔物质加入而获取,埃达克岩的成矿专属性由上地幔成矿元素分布特征决定。与俯冲有关的埃达克质岩浆之所以有利于成矿,重要的原因是存在大量来自俯冲板片的高压、高温流体以及俯冲板片熔融形成高氧逸度(fO2)的熔体,但产出在大陆板内背景、与俯冲无关的埃达克岩的成矿机制还不清楚。根据现代资源勘查理念,结合综合地质信息分析,埃达克质岩具有实际找矿意义。

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