The lower-level (850 hPa) ISO pattern is char-acterized by an anticyclonic circulation over the area south of the Changjiang River, the South China Sea, and the Western Pacific, and a cyclonic circulation from the area north of the Changjiang River to Japan.

對逐年夏季的分析表明，無論當年東亞夏季風(fēng)強與否，在所劃分的幾個東亞季風(fēng)區(qū)所有澇的年份里一区二区三区黄片，太平洋同一緯帶上大氣ISO向西傳播都明顯較強，而在這些區(qū)域絕大多數(shù)旱的年份里在线免费看黄色片视频网站，相應(yīng)的ISO向西傳播明顯較弱巴西在线无码AA片。

4For the typical great flood years of the Yangtze River basin,the ISO anticyclone and cyclone system are continue making and move westward and northward to the eastern China and the coastwise western Pacific by the change of ISO during May and August.

4對典型的長江流域特大洪澇年，伴隨著ISO的變化操屄视，夏季5～8月女人十八片，在西太平洋副熱帶地區(qū)和熱帶赤道附近不斷有ISO氣旋環(huán)流系統(tǒng)生成，并向西青草不雅三级在线观看、向北移動到我國東部及沿海地區(qū)国产一级特黄在线视频。

Standing on the bridge on the fortieth anniversary of the event, he looked west, as he had so often, so fruitlessly, four decades earlier, and got to talking about the Guards brewing up their tea, and then on to the relatively light casualities the Guards suffered as compared to the 1st Ariborne, and on to the magnificent performance to the 82nd.

戰(zhàn)役四十周年紀念日那天在线观看黄色毛片，他站在阿納姆橋上，向西張望久青草视频，一如40年前他曾經(jīng)頻繁而無效向西張望一樣caoporen在线精品视频，他談起皇家裝甲師燒水沏茶，談起皇家裝甲師比起第1空降師相對較輕的傷亡四虎成人最新影院网址大全，談起82空降師出色功勛99九色视频在线观看。

And with an elaborate sea-salute, this fellow, a long, ill-looking, yellow-eyed man of five-and-thirty, stepped coolly towards the door and disappeared out of the house. One after another, the rest followed his example; each making a salute as he passed; each adding some apology.

這個大個家伙，是個黃眼珠美女性爱网站、三十四五歲的丑八怪91av视频在线观看，他向西爾弗敬了個很像樣的水手禮，拖著腳步向門外走去亚洲国产黄片，其余的幾個家伙也跟著他離開屋子自拍日韩视频首页在线视频，每個人經(jīng)過西爾弗的身邊都敬個禮，打聲招呼这里视频亚洲视频免费观看,。

It is an intracontinental deformation system resulting from the structural stress caused by the collisions of the Huaiyu terrane moving westwards and the Cathaysia block moving northwestwards.

江南古陸與華夏古陸拼接帶北西側(cè)前震旦紀地層中存在著近東西向褶皺疊加在早期近南北向褶皺上的現(xiàn)象激情网免费视频，這是懷玉地塊向西拼貼、華夏古陸向北西碰撞拼接過程中構(gòu)造應(yīng)力向陸內(nèi)傳遞時形成的構(gòu)造變形系統(tǒng)免费黄色xxxx视频。

LUPIT is expected to track west to west-northwest in the next 12 to 24 hours.

盧碧將於未來 12 至 24 小時繼續(xù)向西或西北偏西移動日韩国产精品免费人成视频，稍后隨著副高接合，盧碧將於其南部向西南偏西移動免费直接看黄。

Since the specific boundaries of the south of the Sino-Mongolian borders Aershan east, along the valley leap Daxinganling chaor to Ulanhot Jalaid Banner near the northeast; and then fold the south, and the Horqin grassland along the eastern edge of the Liaoning Province, near Zhangwu; re - hure qi and paddock off to the west along the south county line southwest southern edge of Inner Mongolia Plateau.

具體界線自阿爾山以南中蒙國界向東一级毛片av全部免费播放，沿綽爾河谷跨躍大興安嶺，到烏蘭浩特東北的扎賚特旗附近中文字幕国产无码；再折向南亚洲A片在线观看片不卡，并沿科爾沁草原東緣到遼寧省彰武附近；再折向西沿庫倫旗和圍場縣南內(nèi)蒙古高原南緣向西南行日本欧美国产激情。

The south-north united tectonic environment and tectonic pattern does not exist. The east-west trend thrusting Nappe structure of Majiatan and Hengshanpu can not represent the whole western margin of Ordos. The attempt to solve the regional tectonic problem with simple tectonic pattern is against the geological theory, especially in the Helan Mountain region.(2) After the geochemical data analysis of Ruqigou basalt in Helan Mountain, the article illustrates that it belongs to continental rift basalt which appeared in the late-Triassic and early middle Jurassic. Meanwhile the article states that the region is located in the rift environment of an extension background and Rudigou is located in the central part of the rift.(3) The article illustrates that the western ridge of Helan Mountain used to be on a slope and topography slowly declines from west to east after analysis and demonstrations of the distribution under XiaoSongshan bedding fault. Through comprehensive analysis of the no-strong deformation and bedding fault features, the article states that the Xiaosongshan bedding fault used to be gravity slip detachment structure and it represents the extension from the east to the west. Based on the above and analysis and demonstrations of isotope age and track datting, the article illustrates that the ? characteristic of the east of the western ridge of Helan mountain being higher than the west is the result of its late tectonic reverse.(4) Through comparison between Rujigou region Mesozoic Era late Triassic period-early and middle Jurassic period deposit and that of Ordos Basin and the analysis of the late Triassic period extension and early -middle Jurassic Period deposit povenevance it sets forth that during the period, Rujigou region was part of a large deposit basin which was closer to the northern povenevance and farther from the western povenevance.

以馬家灘和橫山堡為代表的東西向逆沖推覆構(gòu)造模式在线精品91青草国产在线观看，在整個鄂爾多斯盆地西緣不具有全區(qū)統(tǒng)一性，那種試圖用單一的構(gòu)造模式解決本區(qū)構(gòu)造問題的嘗試我想看黄色一级高清无码视频，無疑是與地質(zhì)實際相悖的国产高清色色，尤其是對賀蘭山地區(qū)；(2)通過對賀蘭山汝箕溝玄武巖地質(zhì)地球化學(xué)測試分析99riav1com，提出其為大陸裂谷玄武巖j国产在线，其形成時代為晚三疊—早中侏羅世，并通過該玄武巖的稀土和微量元素的測試分析資料進行了多種判別分析中文字母强奸乱论，最終確定該區(qū)處于拉張背景下的裂谷環(huán)境国产又大好爽免费视频，汝箕溝地區(qū)大致處于當時裂谷的中心部位；(3)通過對小松山斷層面之下地層分布規(guī)律，結(jié)合其變形特征的分析論證鲁鲁鲁网站，認為當時賀蘭山西麓處于一個由東向西平緩抬高的斜坡環(huán)境欧美日韩精品一二三区，并通過小松山斷層面之下地層的非強烈變形及順層斷層特征等的綜合分析，認為賀蘭山西麓的小松山斷層原本是一重力滑覆斷層最新地址福利影院，它代表了近東西向的拉張欧洲一级高潮喷水A片，在此基礎(chǔ)上通過裂變徑跡測試資料的分析論證對其做了進一步認定，目前賀蘭山西麓東高西低的剖面特征是該區(qū)后期構(gòu)造反轉(zhuǎn)的結(jié)果国产又粗又大又硬又爽免费视频；(4)通過對汝箕溝地區(qū)中生代晚三疊世—早中侏羅世沉積與鄂爾多斯盆地內(nèi)部的對比麻豆精品无码国产在线、晚三疊世延長組及早中侏羅世沉積物源和水流向分析，認為該時期汝箕溝地區(qū)為一更靠近北部物源成人网站香草视频在线观看，而距西部物源明顯較遠的沉積環(huán)境日韩无码肏逼，是一更大型沉積盆地的一部分。

And the westward ISO is usually the low-frequency low and high pressure systems from the Bay of Alaska in northeastern Pacific and the Okhotsk in the northwestern Pacific of mid high latitudes, and the ISO evolving in subtropical easterlies.

進一步分析發(fā)現(xiàn)免费无遮挡无码永久视频在线观看，經(jīng)向風(fēng)ISO的緯向傳播對應(yīng)著大氣經(jīng)向型環(huán)流系統(tǒng)的移動日韩福利片影音先锋在线播放网站视频，向西傳影響東亞夏季風(fēng)區(qū)降水的ISO有來自低緯中東太平洋東風(fēng)流中的低頻氣旋（如副熱帶東風(fēng)帶中ISO的演變）；也有來自中高緯度阿拉斯加灣及鄂霍次克海一帶低頻低壓和高壓(如阻塞高壓和東北太平洋高壓)的向南向西頻散中文字幕日韩三级片一区二区。

Based on analyses of observations from the short-spaced GPS receiver array at Wuhan, the storm-time ionospheric irregularities which resulted in scintillations and rapid TEC fluctuations showed westward drifts between 21∶30 and 03∶00 LT with drift velocities changing from ~40 to ~130 m/s. And based on analyses of observations from the ultra-short spaced GPS receiver chain at Guilin, ionospheric irregularities which resulted in the L-band radio wave scintillations, showed eastward drifts around local midnight ranging from ~70 to ~55 m/s on the quiet-day and westward drifts ranging from ~150 to ~50 m/s before the midnight and eastward drifts after the midnight ranging from ~25 to ~65 m/s on the disturbed day.

短間距臺網(wǎng)和超短間距臺鏈觀測實例的計算結(jié)果表明，暴時武漢地區(qū)引起TEC快速起伏的電離層不規(guī)則結(jié)構(gòu)沿緯圈向西漂移97在线欧美超碰，21∶30至03∶00 LT丁香综合视频露脸，西向漂移速度在約40 m/s至130 m/s的范圍內(nèi)變化；在桂林地區(qū)三级片A片一级片，磁靜日午夜前后引起L波段電波閃爍的電離層不規(guī)則結(jié)構(gòu)沿緯圈向東漂移污污网站在线播放一区二区，漂移速度從約70 m/s下降到約55 m/s，磁擾日午夜前不規(guī)則結(jié)構(gòu)向西漂移嘿咻欧美，速度從約150 m/s下降到約50 m/s久久精品亚洲区二区三区欧美福利，午夜后轉(zhuǎn)為向東漂移，速度從約25 m/s上升到約65 m/s国产视免费性爱视频。

northwestward：向西北方

northwestnorthwestern 西北方 | northwestward 向西北方 | northwestwardly 自西北的

northwestwards：向西北方地

northwestwardly 向西北的 | northwestwards 向西北方地 | norward 北方

westbound：向西進行的

west-southwest 西南西 | westbound 向西進行的 | westering 向西

westbound：向西駛的

west-south-west 西南西 | westbound 向西駛的 | wester 西風(fēng);向西

wester：西風(fēng);向西

westbound 向西駛的 | wester 西風(fēng);向西 | wester 轉(zhuǎn)向西面

westering：向西

westbound 向西進行的 | westering 向西 | westerly 西的

westering：向西/西下的

wesleyanism /衛(wèi)斯理公會教派/ | westering /向西/西下的/ | westerlies /西風(fēng)帶/

westward：西方, 西部, 向西旅行 西方的, 向西的 向西

prehistorian 史前史學(xué)家,史前學(xué)家 | westward 西方, 西部, 向西旅行 西方的, 向西的 向西 | phase variation [遺]相變異, 相轉(zhuǎn)變

westward：向西西方的

Westoncell 韋斯頓電池 | westward 向西;西方的 | westward 向西西方的

westwardly：向西/自西

westward /向西的/西方的/向西/向西方/西方/西部/往西/ | westwardly /向西/自西/ | westwards /西方/西部地/