查询词典 orbicular

Corolla purple-red or pink, subcampanulate, 5-lobed; tube short; lobes spreading, overlapping in bud, oblong to orbicular.

花冠紫红色或粉红色，近钟状，5浅裂；筒部短；裂片平展，在芽中重叠，长圆形到圆形。

Corolla 1.1-1.5 cm when open, tube 1/3 to 1/2 as long as limb, middle lobe of limb largest, rhombic-obovate, subcircular, or obovate-orbicular; petiole ca. 1/5 as long as blade.

花冠1.1-1.5厘米什么时候开阔的，筒部在1/2倍于瓣片，中部裂片大的瓣片，倒卵形，近环形，或倒卵形圆形；约的叶柄1/5的倍于叶片。

Inflorescences capitate; infructescences less than 5 cm; leaf blade orbicular to ovate, margin shallowly cut or subentire.

花序头状；果序少于5厘米；叶片圆形到卵形，边缘减少或近全缘。

Basal petioles 1.5–5 cm, sheaths long, broad; blade oblong, 2–4 × 1–2 cm, pinnate; pinnae sessile,(3–) 4–6 pairs, remote; ultimate segments long-ovate to suborbicular, 5–10 × 3–8 mm, base subtruncate or rounded, entire or apex shallowly 1–3-toothed, sometimes 3–4-crenate; terminal pinnae obovate or orbicular, base cuneate, apex more deeply 3-lobed.

基部的叶柄1.5-5厘米，鞘长，宽；叶片长圆形， 2-4 * 1-2 厘米，羽状；羽片无柄，(3-)4-6 对，遥远；末回裂片长卵形到近圆形， 5-10 * 3-8 毫米，基部近截形或圆形，有时，浅全缘或先端1-3齿状具圆齿；更深的顶生的羽片倒卵形的或圆形，基部楔形，先端3浅裂。

Drupe obliquely ovoid to oblong-ovoid, compressed, 3–4.3 × 2–3 cm, densely pubescent, base mostly subtruncate, apex pointed to somewhat obtuse; mesocarp thin, splitting at maturity; endocarp yellowish white to brown, ovoid, broadly ellipsoid, or shortly oblong, asymmetric on both sides, 2.5–3(–4) cm, hard to fragile, ventral suture curved and ± acutely keeled, dorsal suture generally straight, surface smooth and pitted with or without shallow furrows, base obliquely truncate to orbicular-truncate. Seed sweet or bitter.

花柱长于雄蕊核果的斜卵球形到长圆形卵球形，压扁， 3-4.3 * 2-3 厘米，密被短柔毛，多数基于，顶指向稍钝；中果皮薄，成熟时劈开；内果皮淡黄白色的到棕色，卵圆形，宽椭圆形或者不久长方形，不对称的两面， 2.5-3(-4)厘米，对脆，腹面缝硬弄弯和尖锐龙骨状的多少，种子甜的或难以接受。

Fruit densely tomentose when mature; leaves broadly ovate to orbicular when mature

成熟时的果密被绒毛；成熟时的叶宽卵形到圆形 43

Figs axillary on leafy branchlets, paired, reddish orange to red and with scattered white spots, oblong, pillow-shaped, or conic-ellipsoid, 1.5-2.5 × 1-1.5(-2) cm, glabrous or densely covered with brownish yellow long hairs, inside with few or no bristles, apical pore closed by 3 or 4 umbonate bracts, not forming flat disk, subsessile; involucral bracts orbicular to ovate-lanceolate, margin ciliate.

榕果腋生在生叶的小枝上，配对，带红色橙随着红色并且具星散白点，长圆形，枕头形成，椭圆形的或圆锥形， 1.5-2.5 * 1-1.5(-2)厘米，无毛或者密被带褐色的黄长毛，总苞片圆形到卵形披针形，边缘具缘毛。

For Southwestern Margin of Aqikekule Lake ophiolite, their field geological, petrological, minerological, petrochemical and geochemical characteristics show that:① it outcropped as tectonic slices along the near west-to-east strike Kunzhong fault and is composed of metamorphic perodotties, cumulates and volcanic rocks, in which, chromites are distributed in the upper part of metamorphic peridotites as pods, or in the lower part of cumulates as near-strata;② metamorphic peridotites include serpentinites, chromite-bearing serpentinites, chlorite-epidote schists and chromitites, of which, chromitites have nodular and orbicular structure, and cumulates include pyroxenits, serpentinites, chromite-bearing serpentinites, chromites and metamorphically mafic rocks and only basalts are seen in volcanic rocks;③ Cr# of chromites suggest that they formed in the SSZ and Al〓O〓 and TiO〓 of metamorphic peridotites also suggest SSZ environment;④ metamorphic peridotites have V type and enriched LREE patterns, cumulates have from strongly depleted LREE, flat REE to enriched LREE patterns with universally striking positive Eu anomalies and basalts show flat REE or slight enriched LREE patterns with no Eu anomalies;⑤ trace element and Sm-Nd isotope characteristics of metamorphic peridotites imply their strikingly heterogeneous mantle character ε〓(t+4.39～+26.20 and later Nb, Ta fertilization;⑥ trace element characteristics of basalts and their tectonic diagrams show they probably formed in the rifted island arc or back-arc basin environment.

对阿其克库勒湖西南缘蛇绿岩，野外地质、岩石学、矿物学、岩石化学以及地球化学等特征表明：①该蛇绿岩以近东西向、沿昆中断裂呈构造岩片出露，由变质橄榄岩、堆晶岩和火山岩三个单元组成，其中见铬铁岩呈豆荚状产于变质橄榄岩的上部，或呈似层状产于堆晶岩的下部；②变质橄榄岩包括蛇纹岩、含铬铁矿蛇纹岩、绿帘绿泥片岩和铬铁岩等类型，其中，豆荚状铬铁矿具有结核状构造和球状构造，堆晶岩包括辉石岩、蛇纹岩、含铬铁矿蛇纹岩、铬铁岩和变质基性岩等类型，火山岩仅见玄武岩；③铬铁矿的Cr#表明其形成在俯冲带，变质橄榄岩的Al〓O〓和TiO〓成分也指示了SSZ环境；④变质橄榄岩的稀土配分型式见V型和LREE富集型两种型式，堆晶岩表现出从LREE强烈亏损、REE平坦分布到LREE富集的配分特征，并且普遍具有醒目的正Eu异常，玄武岩的稀土配分型式表现为平坦型或LREE略富集，无Eu异常；⑤变质橄榄岩的微量元素及Sm-Nd同位素特征指示了其地幔的显著不均一性ε〓(t为+4.39～+26.20以及Nb、Ta在后期的富集；⑥玄武岩的微量元素特征及构造图解表明其可能形成在裂谷岛弧或不成熟的弧后盆地环境。

Sepals ovate-orbicular, boat-shaped, ca. 3 mm, glabrous.

萼片卵形圆形，舟状，约3毫米，无毛。

Sepals lanceolate or ovate-orbicular, sometimes shallowly boat-shaped, inner 2 often connate at base.

萼片披针形或卵形圆形，有时舟状，内部2通常在基部合生。

This one mode pays close attention to network credence foundation of the businessman very much.

这一模式非常关注商人的网络信用基础。

Cell morphology of bacterial ghost of Pasteurella multocida was observed by scanning electron microscopy and inactivation ratio was estimated by CFU analysi.

扫描电镜观察多杀性巴氏杆菌细菌幽灵和菌落形成单位评价遗传灭活率。