Lakeshore, the breeding of life's chorea.

湖岸，滋生生活的情愫欧美黑B。

The main water factors of fishpond water in lakeshore and the impact of fish yield were analyzed.

分析了三角帆蚌對(duì)水體的主要水質(zhì)因子變化及魚產(chǎn)量的影響国产一级毛片黑白配。

For example, lakeshore landslip, lake has been filled up, forest and tilth has been destroyed, water quality has gone to bed etc. The reasons for the environment change of Chaohu are mainly attributed to humans disturbance.

在此基礎(chǔ)上，建立了巢湖流域的土地利用分類系統(tǒng)三级片免费激情视频，并對(duì)1987年和2000 年的兩幅遙感影像www.mjjscg.com，采用前分類遙感動(dòng)態(tài)變化監(jiān)測(cè)方法，對(duì)比分析了十幾年來(lái)的土地利用變化情況欧美性爱性爱大片。

Sup2; Today, new scenic spots on the south lakeshore have been added, and the rebuilt Leifeng Pagoda is open to the public.

sup2日日干夜夜操av；只要臺(tái)灣當(dāng)局同一在一個(gè)中國(guó)的原則下解決臺(tái)灣問題，我們可以耐心等待久久综合迷奸。

The community was named after FW Rhinelander, president of the Milwaukee Lakeshore and Western Railroad.

社區(qū)被命名后黄色精品网，又一萊茵蘭德總統(tǒng)密爾沃基湖岸和西部鐵路。

The lakeshore sightseeing road is used by visitors for enjoying landscape of lakes and water. The wetland forest provides recreation facilities such as camping, roaming and climbing. The bathing lakeside is an ideal site for freshwater bath, sunbath and sand bath.

湖濱觀光路供游客觀賞湖光水色自拍日韩在线视频播放免费网站；濕地森林包括林間野營(yíng)黄片久久久、林間漫步J8又大又粗又长又硬不爽、林木攀藤等休閑設(shè)施；濱湖浴場(chǎng)波平沙細(xì)欧美作爱视频一区二区三区，湖水清澈综合在线视频精品专区，空氣清新，是淡水浴人人干人人操女的、陽(yáng)光浴性爱在线视频网、沙浴的理想場(chǎng)所。

Fourth: According to the ecological protection and planning of shanghu urbanwetland park lakeshore line, we found out five kinds of protected wetlandslakeshore:bank revetment of gentle slope water, bank revetment block stone or pine,bank revetment of Natural flora, bank revetment of hydrophile grandstand, bankrevetment of field stone.

4在對(duì)尚湖城市濕地公園岸線的生態(tài)保護(hù)規(guī)劃基礎(chǔ)上午夜在线公开视频，研究出五種適合城市濕地公園的護(hù)岸形式：緩坡入水護(hù)岸国产视免费性爱视频、塊石或松木樁護(hù)岸、大卵石護(hù)岸欧美在线看你懂的免费看、自然植被護(hù)岸色图综合亚洲、親水看臺(tái)護(hù)岸。

By studying reservoir rock characteristics, diagenesis and physical property, investigation showed that there were distributary channel, branch channel, mouth bar, distal bar, sand sheet, lakeshore, shallow lake and limestone flat . we concluded that the reservoir of N1～N21 is low porosity and permeability reservoir with the types of primary porosity and secondary intergranular porosity, which is in the early diagenetic stage B into the late diagenetic stage A subperiod. The role of effecting reservoir physical property is deposition, cementation, dissolution and tectonic rupture. After researching of reservoir, we divided it into three categories and division the favorable facies belt and relatively favorable. We think that the favorable facies belt is braided river delta front and partly shallow lake in east of the Fault Ⅶ. favorable reservoir is in the first and the second class.

進(jìn)一步研究了本區(qū)碎屑巖儲(chǔ)層的巖石學(xué)特征免费观看人成、成巖作用特征曰韩性交业余、物性特征，研究認(rèn)為該區(qū)儲(chǔ)集體類型有分流河道砂體五月婷婷c、分支河道砂體欧洲亚洲自拍、河口壩、遠(yuǎn)砂壩美女频黄、席狀砂砂體国产午夜福利在线观看禁、濱湖砂灘、淺湖砂壩砂體及灰坪欧美又粗又大又长A片；N1層屬于低孔AV剧情麻豆国产在线观看、特低滲儲(chǔ)層，孔隙類型以原生成年人欧美片、次生粒間溶孔為主干鲁鲁鲁鲁鲁鲁；分析了影響儲(chǔ)層物性的因素主要為沉積作用、膠結(jié)作用jiuse200、溶蝕作用和構(gòu)造破裂作用强奸乱伦视频网站；進(jìn)行了儲(chǔ)層評(píng)價(jià)與有利相帶預(yù)測(cè)，將儲(chǔ)層分為三類并劃分了有利區(qū)帶99爱国产、較有利區(qū)帶欧美黄色视频,黑人黄色视频，認(rèn)為Ⅶ號(hào)斷層以東的辮狀河三角洲前緣亞相和部分淺湖亞相是N1的有利儲(chǔ)集相帶，儲(chǔ)層以Ⅰ国产精品久久无码AV片、Ⅱ類為主日本第一页。

During the paleo-geography evolution, inland lacustrine basin began to form, and the two delta skirt in east and west lakeshore are primary formed in Chang 10, lacustrine basin subsidized quickly, lake district enlarged rapidly and destructive delta are developed in Chang 9, delta are more developed in Chang 8, lakeshore line move outward at large range, turbidite developed well near west lakeshore, delta range is decreased in east lakeshore in Chang 7, features of lacustrine basin are changed remarkably, deep lake and half deep lake area is decreased greatly, while delta sedimentary system is developed at its most in Chang 6, framewok is inherited better, but delta′s construction is slowed and is swamping at large scale in Chang 4+5, lacustrine basin began to be silting, shrinking and dying out, and riverway gradually developed well since Chang 3, distributary riverway developed best in Chang 2, because of imbalance subsidence, subsidence center is formed in east Zichang area and in which lacustrine turbidite is sedimented.

在古地理演化過程中，長(zhǎng)10期內(nèi)陸湖盆開始形成，東西兩岸兩大三角洲裙初步形成91久久高清国产自产拍；長(zhǎng)9期湖盆快速下沉www色五月，湖區(qū)迅速擴(kuò)大，三角洲多為破壞性的www.hh6554.com；長(zhǎng)8期三角洲進(jìn)一步發(fā)育美女被插高潮到爽；長(zhǎng)7期湖岸線大幅度向外推移，西部濁積巖發(fā)育国产操穴视频，東部三角洲面積明顯減泄赡晡蘼刖镁镁镁玫缬啊；長(zhǎng)6期湖盆面貌發(fā)生了顯著的變化九九视频这里有精品视频，深湖－半深湖面積大大減少国产在线91播放精品，三角洲沉積體系極為發(fā)育；長(zhǎng)4+5期繼承了長(zhǎng)6的沉積格局夜夜燥天天燥视频，三角洲建設(shè)進(jìn)程減慢欧美性爱A片一级，三角洲大面積沼澤化；從長(zhǎng)3期湖盆開始逐步淤淺欧美A片激情日、萎縮999在线视频免费观、消亡，河道逐漸發(fā)育人人干人人玩人人摸；長(zhǎng)2期分流河道發(fā)育A片免费视频网站入口；長(zhǎng)1期由于差異沉降欧美一区二三区，在東部子長(zhǎng)一帶形成沉降中心亚洲一级av高清毛片，沉積了湖相濁積巖。

Chicago's new six-acre Park at Lakeshore East Is the centerpiece and identity of the 28-acre Lakeshore East along Lake Michigan.

芝加哥的新六英畝公園在 Lakeshore 東方沿著湖密西根州是中心裝飾品和 28畝英畝的 Lakeshore 的相同東方凹凸黄色视频免费观看。