由河

Some innovative results are listed below:1、According to the lithologic characters,lithofacies,genetic classification and the geomorphy,the Quaternary system is divided into piedmont-gully\'s and plain\'s. The piedmont-gully\'s Quaternary sediment,which is about 3～20 meters in thick,is in the western hills of the study area.The plain\'s Quaternary sediment is widely distributed in the study area,which is about 30～60meters thick and become thicker from southwest to northeast.2、The Quaternary sediments of plain can be divided into five sedimentary cycles.The Late Pleistocene series Quantan group,at the bottom of the Quaternary System,is constituted by a fluvial facies-river and lake facies sedimentary cycle. The Late Pleistocene series Jiashan group,at the middle of the Quaternary sediment, is constituted by two fluvial facies-neritic facies-river and lake facies sedimentary cycles.The Holocene series Binhai group,at the upper of the Quaternary sediment, is divided into three parts,the under layer and middle layer are constituted by two littoral facies-river and lake facies sedimentary cycles,the upper layer is constituted by paludal facies,which was deposited at the lower-lying land like West Lake, Jiangcun-Gu dang,Xianghu lake,and coastal-estuary facies in other area.3、Folding and fault activities were weak in Quaternary and the tectonic activity had little influence on the Quaternary sedimentation.The ancient landforms,the evolvement of the river system and transgression were the main elements which controlled the Quaternary sedimentation in Hangzhou.The ancient landforms formed the basis of the Quaternary sedimentation.The evolvement of the river system and transgression individually or jointly controlled the Quaternary sedimentation of this area.4、The alternation of the climate was the main reason for the evolvement of the river systems and transgression,and it\'s also the reason why the Quaternary system of Hangzhou has the special sedimentary structure which is called soft interbed with hard layers.

通过研究取得了以下成果：1、根据岩性、岩相、成因类型和地貌特点，将本区第四系划分为山麓沟谷区沉积和平原区沉积：山麓沟谷区第四系主要分布于西部丘陵地区，厚度较薄且变幅大，一般厚3～20m；平原区第四系广布分区，由南西向北东逐渐增厚，一般厚30～60m.2、平原区第四系自下而上大体由五个完整或不完整的沉积旋回构成：底部上更新统全塘组，由河流相—河湖相的沉积旋回构成；中部上更新统嘉善组，由河流相—浅海相—河湖相两个沉积旋回构成；上部全新统滨海组，其下中两段由滨海海湾相—河湖相的两个沉积旋回构成，上段由西湖、蒋村—古荡、湘湖等低洼处沉积的湖沼相和其他地区沉积的滨海河口相构成。3、第四纪以来，研究区内褶皱、断裂活动微弱，构造运动对第四系沉积的影响不大，古地形、古水系的发育、变迁和海侵是杭州市第四系沉积的主要控制因素：古地形构成了第四系沉积的基底，水系与海侵在其后的不同阶段或分别或联合的主导了区内的第四系沉积。4、水系的发育、变迁和海侵的共同原因是天气变化，正是由于第四纪以来"冷热交替"的天气特点形成了杭州市第四系"软硬互层"的特殊沉积结构。

The Es formation was divided into seven third order sequences based on the seismic, drilling and logging data, and plans deposition system plane distribution maps of different time were plotted by dominance phase principle. The lower Es4 is flood-overlake facies mainly; the upper Es4 is meandering stream and braided river delta deposition above the shore shallow lake background; in the Es3 period, the south mainly developed braided river, meandering stream delta, the northeast area main developed meandering stream delta, the middle area mainly developed semi-deep lakean d deep lake sediments. From lower Es3 to upper Es3, the delta scale gradually increased and the depositional area gradually moved to the east and the southeast; the Es2 period was dominated by shore-shallow lake sediments and widely developed braided river delta and delta deposits; the Es1 period was dominated by shore-shallow lake shoal deposits, and in the south developed meandering stream and braided river delta deposits.The lothological traps of the Shahejie group are mainly fluxoturbidite and stratum lateral pinch-out, and its formation and the distribution of the lothological trap were controlled mainly by the basin structure characteristic, palaeogeomorphology and tectonic activity and so on. It had a beneficial geological condition to develope sublacustrine slump turbidite fans in Jishan, Jiangjiadian and Wawu.

利用地震、钻井、测井等资料，将古近系沙河街组划分出7个三级层序，通过剖面沉积学分析，以优势相原则绘制不同时期各亚段沉积体系平面分布图：沙四下总体以洪水-漫湖沉积为特征，沙四上沉积时期是在滨浅湖背景之上发育了曲流河三角洲和辫状河三角洲沉积；沙三段沉积时期南部主要发育辫状河、曲流河三角洲，西北部地区发育曲流河三角洲，中部地区主要为深湖—半深湖沉积；由沙三下至沙三上，西北部三角洲规模逐渐增大，沉积范围逐渐向东、东南方向推进；沙二段沉积时期为滨浅湖沉积，在背景之上广泛发育了辫状河三角洲和三角洲沉积；沙一段以滨浅湖滩坝沉积为特征，南部发育了曲流河三角洲和辫状河三角洲沉积；沉积地层中的岩性圈闭以滑塌浊积岩岩性圈闭和地层侧向尖灭型岩性圈闭为主，其形成和分布主要受盆地结构、沉积古地貌和构造活动强度等因素控制，北部基山、南部江家店和瓦屋具有发育滑塌浊积扇的良好地质条件。

Course north has lock of new city of door of Hanjiang chaste tree, via the join river channel of new excavate, into Xi Jing river, Yan Jiahe, twin store canal, rash inn lock enters long lake, lock of members of a family passing custom arrives inside Jing He, by Huan Zi buccal lock enters snail hill trunk canal, from Hong Hu snail hill lock exports the Yangtse River south.

航线北起汉江荆门新城船闸，经新开挖的连接河航道，进西荆河、殷家河、双店渠、鲁店船闸入长湖，过习家口船闸到内荆河，由宦子口船闸进螺山干渠，南从洪湖螺山船闸出口到长江。

To finish it, this essay puts forward the demands to the changing of Chinese teachers in carrying out the curriculum: the teachers should change themselves from "authority" to "anti-authority", from "guide" to "accelerator", from "supervisor" to "friend", from "building the spirit" to "practicing the spirit", from "a pool" to "a running river", from "challenge" to "accepting the challenge", from "candle" to "fruit tree", from "ruler" to " the chief in the equality", from "gardener" to "the "the leader of human life.

最后，对物理教师的角色转变提出了形象的具体目标：由&权威&向&非权威&转变，由&指导者&向&促进者&转变，由&导师&向&学友&转变，由&灵魂工程师&向&精神教练&转变，由&信息源&向&信息平台&转变，由&一桶水&向&生生不息的奔河&转变，由&挑战者&向&应战者&转变，由&蜡烛&向&果树&转变，由&统治者&向&平等中的首席&转变，由&园丁&向&人生的引路人&转变。

It is the source of the Green River, a tributary of the Lillooet River, and is fed by the River of Golden Dreams, which issues from Alta Lake, which is at the height of land dividing the Green River drainage from that of the Cheakamus River to the south, which is a tributary of the Squamish River.

它是绿色源头，一个利卢埃特河的支流，是由黄金梦，从阿尔塔湖，在土地划分绿河从Cheakamus河的排水问题的高度是哪吃河在南方，这是史夸米殊河的支流。

Lonely Planet advises tourists to steerclear of[2]Chocó on the Pacific coast, Putumayo in the far south "anywhere east of the Andes", where there are still guerrillas.

孤独行星&公司建议游客避开太平洋沿岸的乔格、最南端的普土马由河地区以及&安第斯山脉东部各地区，因为8 Tt t 8。

Lonely Planet advises tourists to steerclear of[2]Chocó on the Pacific coast, Putumayo in the far south and "anywhere east of the Andes", where there are still guerrillas.

孤独行星&公司建议游客避开太平洋沿岸的乔格、最南端的普土马由河地区以及&安第斯山脉东部各地区，因为这些地方仍有游击队出没。

Lonely Planet advises tourists to steer clear of[2] Chocó on the Pacific coast, Putumayo in the far south and "anywhere east of the Andes", where there are still guerrillas.

&孤独行星&公司建议游客避开太平洋沿岸的乔格，最南端的普土马由河地区以及&安第斯山脉东部各地区&，因为这些地方仍有游击队出没。

Lonely Planet advises tourists to steer clear of[2] Chocó on the Pacific coast, Putumayo in the far south and "anywhere east of the Andes", where there are still guerrillas.

孤独行星&公司建议游客避开太平洋沿岸的乔格、最南端的普土马由河地区以及&安第斯山脉东部各地区

It grew up by the river Granta, as the Cam was once called.

因为凸轮曾经叫，它由河Granta长大。

In this paper, the requirement analysis, design and implementation of the system are introduced in detail.

此论文详细介绍了系统的需求分析，系统设计和具体实现。

In the context of economic globalization is increasingly deepening, China's economy can not be spared.

在经济全球化日益加深的背景下，中国经济不可能做到独善其身。