查询词典 algae zone

To facilitate the restoration and recovery of reef ecosystems and to protect the marine resources, the government of Taiwan ROC has designated Dongsha Atoll as a marine national park in March 2004. The area encircled by 100 m isobath has been designated as the protected zone and the area encircled by 12 miles from the edge of the atoll has been declared as the general control zone.

为了保护东沙环礁的生物资源及促进环礁生态系的复原，政府已於2004年3月通过设立东沙国家海洋公园，预定将环礁外围100公尺等深线之内的范围划设为海洋生态保护区，此界限至环礁外围12里为一般管制区。

The deep water deposition means the deposition in the area where the water depth is larger than 30 meters, in which the major sediments are coarse sand and gravel. This kind of deposition is the relic deposition formed by the Pleistocene alluvial-lacustine deposition reworked under modern channel currents actions, and ususally the Holocene acummulation lack in the deep waters. The transitional zone deposition is the deposition between the low tidal level line and the 30 meters isobath, where the sediment types is changeable and the grain sizes are gradually coarsening from the low tidal line to the deep water area. This kind of deposition is developed by the deep water eroded sediments sorting under the transitional zone current action. The different types distributed along the isobath. The tidal flat deposition is the fine sediment deposition on the tidal flat which is flo sedimentation of the silty clay under the tidal flat dynamic action and ususally developed fluid mud on the lower tidal flat. The channel mouth deposition is the deposition in the channel mouth area. According to the sediment types, it includes sand deposition where there are coarse sediments supply and silt deposition where there are only fine sediments surpport.

峡道深水区沉积是指水深大于30米的峡道底部沉积，它以粗颗粒砂砾石沉积为特色，是现代峡道水动力对第四纪海退时发育的冲洪积和坡积物进行改造形成的蚀余沉积，全新世沉积地层往往缺失；峡道过渡带沉积是指水深介于低潮位线至30米水深线之间发育的峡道边坡沉积，该带沉积以沉积物类型多样为特色，自低潮位线至30米水深线，沉积物粒级逐渐变粗，由粉砂质粘土逐渐递变为中粗砂，是峡道深水区沉积物经多次分选沉积而发育的，基本平行于等深线分布的条带状沉积，在岸坡较陡岸段，过渡带下部可发育重力沉积；峡道潮滩沉积是指在低潮线与海岸线之间发育的细颗粒沉积，它是粘性细颗粒泥沙在潮滩动力作用下，发生动水絮凝沉积而形成的粉砂质粘土沉积，在低潮滩可发育浮泥；峡道口门区沉积则是在峡道汇入大海或海湾时，在峡道出口水流影响所及范围的沉积，根据峡道口门区供给泥沙的特性，峡道口门区沉积有粉砂质淤泥沉积和砂质沉积两种类型。

The Kago Zone contains a Start Zone , a Lodge , Checkpoints , a Mountain Pass and Woods .

2.5.2。轿区包括一个出发区，一个旅馆，数个检查区，一个穿山区和林区。

In this zone the following blossoming shrubs are found in addition to those in the higher zone: Azalea Mollis (golden yellow and found on the hills above Tung Lin); Kerria Japonica; Styracacea, a low shrub with white flowers; and Daphne Genkwa, a violet colored flower resembling the lilac.

此外这里高处还生长着金黄色杜鹃花、黄色的棣棠花、野茉莉和紫色的瑞香花。

In the present paper, a series of investigation has been developed in principle and application on capillary zone electrophoresis with amperometric detection and the third is capillary zone electrophoresis with amperometric detection for composition analysis of Laminarin.

它具有仪器分析所要求的高效、快速、灵敏度高、进样量少、选择性好、仪器简单等优点。本论文围绕毛细管电泳-安培检测技术的原理及其应用做了一些工作。

Chapter 4 Capillary Zone Electrophoresis with Amperometric Detection forComposition Analysis of LaminarinThe composition of laminarin was firstly determined by analyzing its hydrolysis monosaccharides with capillary zone electrophoresis - amperometric detection.

第四章毛细管电泳一安培检测法测定昆布中多糖成分本论文首次用毛细管电泳一安培检测法测定了昆布多糖水解单糖的成分，实现对(来源：Aa4BC9b2b论文网www.abclunwen.com)昆布多糖的测定。在选定的最佳条件下，昆布多糖水解产物岩藻糖、半乳糖、葡萄糖、甘露糖、木糖在20min内实现完全分离而且在铜电极上有着很好的电流响应。通过对昆布多糖中水解单糖成分含量的计算显示该多糖中岩藻糖、半乳糖、葡萄糖、甘露糖、木糖的摩尔比为

It may be the Binhai fault zone according to former studies. The depth of Moho discontinuity change a little larger landward of DanGan Islands, it maybe relate with HaiFeng fault zone.

在担杆列岛往陆方向香港和深圳之间的研究区域，莫霍面有较大起伏，可能与此处发育的海丰断裂有关。

The ophiolites of east Qinling are mainly distributed within a narrow zone lying along the southern fringe of east Qinling and to the north of ShangnanDanfeng fault zone, winding nearly latitudinally as a discontinuous belt.

东秦岭蛇绿岩主要分布在北秦岭南缘、商丹断裂带以北的狭窄地带，断续逶迤呈带状作近东西向展布。

1:250000 geological mapping has further revealed the mysteries of the tectonics of the Qinghai-Tibet Plateau. The Altun Mountains are not of the Tarim massif, but a part of the Kunlun-Qilian-Qinling orogenic system; the Altun fault is a large transform fault; the Muztag-Maqên suture zone and Jinshajiang suture zone are both Variscan ones; the Songpan-Garzê area in the Triassic was a huge turbidite basin on the southern margin of Laurasia; the Gangdise belt underwent the important Indosinian orogenic movement; an ocean basin that persisted from the Paleozoic to Triassic did not exist, i.e. the so-called Paleo-Tethys or permanent Tethys was not in existence in the Qinghai-Tibet Plateau. In the Paleozoic, most parts of China, including the Sino-Korean, Yangtze and Tarim massifs and the Qinghai-Tibet Plateau, were located in south of the main ocean basin—the Central Asian-Mongolian sea way—of the Paleo-Asia ocean, belonging to the northern margin of Gondwana. The Yarlung Zangbo and Bangong -Nujiang belts were twins in the Tethyan Ocean, which began to develop into two ocean rift belts in the Triassic. The Tethyan Ocean with the Yarlung Zangbo belt as the main ocean basin belt began to be subducted in the Late Triassic and experienced a process of pulsatory plate convergence orogeny including the Indosinian, Yanshanian and Himalayan stages.

1：25万地质填图进一步揭开了青藏高原地区大地构造的奥秘：阿尔金山是昆仑，祁连-秦岭造山系的一部分；阿尔金断裂确是一条大型转换断层；木孜塔格-玛沁缝合带和金沙江缝合带均是华力西缝合带；松潘甘孜三叠系沉积盆地是劳亚大陆南部边缘的浊积岩盆地；冈底斯带曾经历了重要的印支造山运动；不存在从古生代延续到三叠纪的大洋盆地，即不存在所谓古特提斯或永久特提斯；古生代时期，在青藏高原地区亦不存在具古生物，古地理分隔意义的大洋盆地，当时，包括中朝，扬子，塔里木以及青藏高原地区在内的中国大部分均位于古亚洲洋主洋盆——中亚-蒙古带之南，属冈瓦纳大陆结构复杂的北部边缘；雅鲁藏布江和班公湖-怒江带是特提斯洋中的孪生姊妹，它们均是从三叠纪起就发展成大洋裂谷带的；以雅鲁藏布江带为主洋盆带的特提斯洋，从三叠纪晚期开始消减，经历了印支，燕山，喜马拉雅3个阶段脉动式板块汇聚造山过程。

The polynomials, such as the Zernike polynomial, the orthogonal Zernike polynomial in square zone and the Legendre polynomial, are used to describe the phase of the wavefront in the algorithm of the Hartmann Sensor's model reconstruction in square zone.

方形区域上的哈特曼波前传感器的波前模式重构算法中可用Zernike多项式、方域上正交的Zernike多项式以及Legendre多项式来重构波前相位。

There are different types of personal loans available.

有许多不同类型的个人贷款优惠。

The above mentioned teaching model of spiral rising can be used to avoid rigidness in teaching.

上述螺旋式上升的教学模式，可以避免教学形成模式後的僵化现象。