middle mountains 中文意思是什麼
middle mountains
解釋
中山-
This famous temple to the god of healing and the sun was built towards the middle of the 5th century b. c. in the lonely heights of the arcadian mountains
這座著名的神廟為了紀念阿波羅太陽神和拯救人類的神而建，它修于公元前5世紀中期，坐落在荒無人煙的阿卡迪亞群山之間。 -
The quaternary incompact deposit provides the material basis for the formation and activities of mud - rock flow with its special geology structure, dazhaigou - haizigou valley has a landform consists mainly of rising middle mountains and monoclinical middle mountains
它們為泥石流的形成與活動提供了物質基礎。受地質構造制約，大寨溝? ?海子溝流域的主要地貌類型是斷塊隆升中山和單斜中山。 -
From i planned for ink and wash ? exhibition of works of ten famous chinese painters to the later southeast china ? exhibition of chinese oil painters sketch works, once upon a time at west lake ? exhibition of stories and archives of west lake and 11 artists, a painting a world ? exhibition of works of contemporary young and middle - aged chinese ink and wash painters, natural scene ? exhibition of works of emerging painters in jiangsu, zhejiang and shanghai, and series exhibition of flowers and birds, waters and mountains, and figure paintings of artists of zhejiang, jiangsu and shanghai, all of these exhibitions actually reflected my observation and thinking over the cultures of jiangsu, zhejiang and shanghai from the point of comparison
從我策劃水墨狀態?中國畫名家十人展開始，到后來的在江南?中國油畫家寫生展、曾經西湖?一個西湖和十一位藝術家的故事文獻展、一畫一世界?當代中青年水墨畫家邀請展、自然風?江浙滬新銳畫家邀請展和江浙滬花鳥、山水、人物系列展等等，這些展事活動全過程事實上是我從比較學的角度對江蘇、浙江和上海三地文化所做的觀察與思考。 -
Abstract : this paper describes in detail the structural characteristics of the taiansi - gangou - cangping fault macroscopically and microscopically, and distinguishes the fault is the main slip ( decollement ) plane in the middle and southern sector of the frontal nappe belt in longmen mountains
文摘:泰安寺-干溝-蒼坪斷裂是龍門山前緣推覆構造帶中南段主滑面，文章詳細描述了該斷裂在宏觀和微觀上的構造變形特徵。 -
Stratigraphic sequence of the early - middle permian reef in western east kunlun mountains
中二疊世生物礁相地層層序 -
The basement of the basin is consist of precambrian crystal basement and paleozoic folding basement, while the cover has undergone the evolution of intra - continental rife in permian, down warped basin in triassic - cretaceous period and inter - mountains basin in tertiary. the main sediments are huge - thick volcanic rock, shallow intrusive rock and tuff in early permian, dark mudstone, marl and muddy dolostone in lucaogou formation in middle permian, huge thick volcanic rock, intruder in tiaohu formation in middle permian, miscellaneous sandy gravel, sandstone and gray mudstone in triassic ( the red is under the gray, and huge - thick dark gray, gray sandy gravel, sandstone, mudstone with coal layer in jurassic
盆地基底由前寒武紀結晶基底和古生代褶皺基底組成，盆地蓋層則經歷了二疊紀的裂谷盆地、三疊紀?白堊紀的坳陷盆地和第三紀后的山間盆地的演化過程。盆地主要沉積了下二疊統巨厚火山巖、淺成侵入巖和凝灰巖；中二疊統蘆草溝組的暗色泥巖、泥灰巖、白雲質巖石以及條湖組的巨厚層火山巖、侵入巖；三疊系雜色砂礫巖、砂巖及灰色泥巖（下紅上灰） ；以及侏羅紀厚層深灰、灰色砂礫巖、砂巖、泥巖夾煤層。 -
We have conducted this campaign from the mountains of afghanistan, to the heart of the middle east, to the horn of africa, to the islands of the philippines, to hidden cells within our own country
我們已經展開行動，從阿富汗山區到中東腹地，從非洲之角到菲律賓諸島，同時不放過隱藏在我國國內的恐怖團伙。 -
Mount tapa, mount tafen, and central mountains are called " the three peaks of taiwan ". historical records of tapa can be traced back to middle qing dynasty. it was known as the pail mountain because of its shape, or heavenly wood mountain, or pakpak basin mountain
有關大霸尖山的記載，早在淡水廳志上就稱它為熬酒桶山，苗栗縣志上則稱之為沖天木山或巴克巴克窪山，早在清代中期，騷人墨客的詩詞中，就有歌頌大霸尖山的作品了。 -
Mount tapa, mount tafen, and central mountains are called " the three peaks of taiwan ". historical records of tapa can be traced back to middle qing dynasty. it was known as the pail mountain because of its shape, or heavenly wood mountain, or pakpak basin mountain. there is also a poem " queer peak of tapa " by zhi - ting, which i am incapable to translate
有關大霸尖山的記載，早在淡水廳志上就稱它為熬酒桶山，苗栗縣志上則稱之為沖天木山或巴克巴克窪山，早在清代中期，騷人墨客的詩詞中，就有歌頌大霸尖山的作品了。 -
On the basis of lots of forerunners " data and my research in this thesis, i put forward that the formation and evolution of the west sichuan foreland - like basin were controlled asynchronally by thrust action of two tectonic zones ? longmen mountains and micang - daba mountains, and divided the west sichuan foreland - like basin into three evolutionary phases - - early margin foreland basin stage ( t3m - t3t ), middle foreland - like basin stage ( t3x - j3p ) and late shrinking and extinct stage ( k1 ? 2 )
在收集眾多前人資料和本論文編寫階段實際觀測研究的基礎上，提出和論證了川西類前陸盆地的形成和演化受龍門山和米倉山?大巴山兩構造帶非同步逆沖推覆作用的復合控制，並將川西類前陸盆地的構造演化劃分為三個階段：早期邊緣前陸盆地演化階段（ t _ 3m ? t _ 3t ） 、中期類前陸盆地演化階段（ t _ 3x ? j _ 3p ） ）和晚期萎縮消亡演化階段（ k _ 1 ? e _ 2 ） 。 -
Linfen lies in the southwest of shanxi province, and the middle reaches of the yellowriver and by fenhe river, with taiyue mountains to the east, luliangt ot he west
臨汾市位於山西省西南部，黃河中游，汾水之濱，東倚太岳，西靠呂梁，中部是遼闊富饒的盆地。 -
108 highway is the south and north mainline to run through middle - west area in my country, and is the main artery of west area economy developing. guangyuan north section of 108 national highway lies in low mountains, and its slope often is unstable
四川省是西南地區經濟發展的龍頭， 108國道是我國中西部地區縱貫南北的主幹線，是西部經濟發展的大動脈，而108國道廣元北段地處低山地段，邊坡失穩現象較常見。 -
Its situated in the middle section of picturesque island ring road against green mountains facing white beach stretch and vast blue sea
酒店位於風景如畫的廈門環島路中段，前鄰潔白綿延的沙灘和碧波萬傾的大海，后與青山綠水相依。 -
Second, gonggeer - one dose of middle massives of assorted tower of willow and common dose of zhengdong jade - willow tower not assorted dose massif not middle last the kunlun axle department not alpine of the mountains not west, including mulberry of tower incompatible, card tower the dose and willow tower a part of the dose not assorted not ancient not blue
二公格爾柳什塔格中間地塊和闐玉公格爾柳什塔格中間地塊位於西昆侖山的高山軸部，包括桑株塔格格不入卡蘭古塔格及柳什塔格的一部分。 -
The distributions of source rocks, reserviors and faults / fissures, and conservation are the critical factors in poolforming and enrichment of gas in the foreland basin. 6. the thrust belts of longmen mountains are potential prospects in the basin with the concentrated structural traps, strucrural - fissuring traps, and faults connecting between the shallow and middle formations
6 、龍門山山前沖斷帶具有較大的油氣潛力，構造圈閉、構造-裂縫型圈閉發育，中淺層構造同步發育或有斷裂溝通，具有中淺層均含氣的特徵。 -
The petrological and geochemical characteristics and petrogenesis significance of spilite from lower permian dashizai group in the middle section of da hinggan mountains
大興安嶺中段二疊系大石寨組細碧巖的巖石學地球化學特徵及其成因探討 -
The flora of laojun mountain nature reserve is close to the subtropical type which is spread in hengduan mountains, middle china and east china, though it is in the cross area of yunnan, guizhou and guangxi characterized with the transition from tropical to subtropical zones
保護區處于區系地域交匯處，與雲南高原和滇黔桂地區屬熱帶與亞熱帶的過渡性質的特徵較不相符，而接近於橫斷山脈和華中、華東地區，區系表現為亞熱帶性質。 -
The month average and the year average water vapor press in chongqing both show that : the water vapor press decreases with the increasing of sea level elevation ; the water vapor press values in north - west and middle hill areas are middle and high ; the water vapor press values in north - east and south - east mountain areas are relatively low. the sea level elevation in north - east and south - east mountain areas of chongqing is higher, especially the north - east mountains are more rugged than the north - west mountains, and the decreasing of water vapor press with the increasing of sea level elevation is more distinct, so the lowest value often appears in the north - east mountains not in the north - west mountains. the seasonal change of water vapor press in chongqing is also distinct : the values of water vapor press are low mostly in winter, and the high values are relatively less ; the values of water vapor press are middle and high mostly in summer, and the low values are relatively less, the values in spring and autumn are between them
重慶市全年各月月平均和年平均水汽壓都表現出：隨著海拔高度的增加，水汽壓逐漸減小；西北部和中部的丘陵低山地區一般為水汽壓的中高值區；東北部與東南部的山地地區的水汽壓則相對較小重慶市東北東南山地地區海拔高度較高，尤其是東北山區的山地較東南山區的起伏更大，水汽壓隨海拔高度的減小更加明顯，因此各月的最小值往往出現在東北山區而非東南山區重慶市水汽壓的季節變化也很明顯：冬季水汽壓多為小值，大值較少；而夏季多為中、大值，小值較少；春秋季則介於兩者之間。 -
Rising middle mountains abounds with steep slops and cliffs and monoclinical middle mountains high slants. this make them easy to collapse in high slants and slope failure usually happens in acclinal slopes. regional geology structure exerts an obvious constraints on the water system of the dazhaigou - haizigou valley
斷塊隆升中山坡面多陡坡和峭壁，單斜中山的逆傾坡以峻坡為主，易產生林金沙江白鶴灘水電站庫區大寨溝、海子溝流域泥石流形成環境與流量研究料崩塌，而單斜中山的順傾坡上易形成滑坡。 -
In the later stage, the garden environment pattern remains all four kinds of middle stage, and there is a new pattern of " the ditch between the mountains " appeared
在後期，園林環境模式在繼承中期四類模式的同時，又有新的模式產生，即峰間縈澗模式。
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