西南部大盆地 的英文怎麼說
中文拼音 [xīnánbùdàpénde]
西南部大盆地
英文
great basin-
Do to fit energetical tower dose and mountain, lazi of a, the east of county from in the west tasha of keshen area storehouse, dose of a tower of mulberry in south of hotan prefecture of china economy, tower dose of crick of iron, willow assorted tower dose, to in the east don t county respectful to draw solemn peaceful tower dose in north wing in south aerjin mountain
和闐玉分佈於塔里木盆地之南的昆侖山。西起喀什地區塔什庫爾干縣之東的安大力塔格及阿拉孜山，中經和田地區南部的桑株塔格鐵克里克塔格柳什塔格，東至且末縣南阿爾金山北翼的肅拉穆寧塔格。3. it was rocky hills and relatively high in the yangtze river mouth area along changzhou, wuxi, changshu, kunshan and qingpu, which belonged to changzhou - kunshan zone according to holocene delimitation from the final stage of the liangzhu culture to the stage of the maqiao culture, due to the expansion of taihu basin and large water areas, maqioa cultural sites were concentrated on rocky hills and cheniersin the east of taihu to the west of shanghai
3 、蘇南常州、無錫、常熟、崑山和青浦一帶曾經是長江河口地區的基巖山地，在全新統地層分區上屬于常州一崑山區，是古地面地勢相對較高的地方。良渚文化末期至馬橋文化期，為太湖湖盆體系擴大時期，水域較大，所以馬橋文化遺址集中於太湖東部與上海西部地勢較高的基巖山地和砂堤之上。Yibin lies in southern of sichuan basic, the first city along changjiang river ten thousand lies cruise. it is the converge spot of jinsha, min and changjiang river. it is an ancient city, over 2000 years history, the famous liquor production capital, over 3000years making spirits history, the hometown of the world - famous wuliangye
宜賓市位於四川盆地南緣，川、滇、黔三省結合部，處于大西南的腹心地帶，金沙江、岷江、長江匯合處，是長江經濟帶西端的支撐點，是國家16個重點開發區之一? ? 「攀西? ?六盤水地區」的重要組成部分。Au ve si cle avant j. c., la france est habit e par trois grandes peuplades : les gaulois dans le nord et, le centre, les ligures au sud - est et les ib res dans le bassin de la garonee. au cours de lhistoire la france conna ? t un certain nombre dinvasions et dinfiltrations qui accentuent encore la richesse et la complexite de la nation fran ? aise
公元前四世紀，法國曾有三個大的民族：北部和中部的高盧人，東南部的利古里亞人及加龍盆地的依澤爾人.法國歷史上經歷過許多次外族入侵和滲透，因而導致了法蘭西民族諸多而復雜的人種成分。Based on an integrated analysis of the surface geological, aeromagnetic, gravity, mt and seismic data from the area of mangnai to serteng mountains in the western qaidam basin, the authors think that the qaidam basin is sandwiched between the north kunlun block and serteng tectonic belt, including two first - order tectonic units the qaidam block and the southern margin of the qilian block and four second - order tectonic units the northern margin of the north kunlun block, qaidam basin, serteng tectonic belt and suhai lake basin in the south of the qilian block
摘要通過柴達木盆地西部茫崖賽什騰山地表地質、航磁、重力、大地電磁測深和地震資料的綜合分析，認為柴達木盆地夾持在昆北地塊與賽什騰構造帶之間，其中包括柴達木地塊與祁連地塊南緣2個一級構造單元和昆北地體北緣，柴達木盆地，賽什騰構造帶和祁連地塊南部的蘇干湖盆地等4個二級構造單元。The middle yangtze region in this paper refers to the most part of hubei and hunan provinces bounded on the north by the qingfeng - xiangguang fracture, on the west by western border of hubei province, and on the south by hunan - guizhou - guangxi deep sea basin
摘要中揚子地區指青峰湘廣斷裂帶以南，湘黔桂海盆以北，鄂西恩施龍山一線以東的湖北省和湖南省的大部分地區。Gubei slope locates in the middle structure area of bohaiwan basin which stretch toward near north and south, and the faults which tend towards east and west spread all over of the whole district. three huge faulty trap whic h control the sediment formation growth distribute in order, which result in the stratigraphy dropping in step along the slope
孤北斜坡帶地處于渤海灣盆地中部近南北向伸展的構造區上，近東西走向的斷層及其斷裂帶縱橫全區，三階大斷裂沿斜坡規律性分佈，基本上控制了全區地層的發育，使得地層沿斜坡坡降式分佈。The research on the lithologjcal and mineral parameters and the sedimentary fades of different periods of mesozoic strata shows that the northern boundary of yanqi basin is almost the same, but great differences existed in the southwestern yanqi basin, that is, the sedimentary range of mesozoic original basin is more bigger than present basin
中生代地層各種巖礦參數和各時代沉積相研究表明，今焉耆盆地北部與原始沉積邊界較為相近；西南和南部的邊界今古差異較大，即在中生代原始盆地沉積范圍要比今盆地范圍要廣。The positive load take absolutely advantage in the first spatial pattern of year and seasons. especially that the precipitation field load of winter is all positive. not in the southwest of china because of southwest monsoon etc. system ; the characteristics of the second spatial pattern are that most of the area is taken up by positive load in year and four seasons, the west of talimu basin is the center of negative load of the year, spring and autumn vector fields ; east of zhungeer basin is the center of positive load of the third spatial pattern of year, spring, summer and winter, the center of negative load is often in east of chaidamu basin, but the distribution center of autumn is in east of zhungeer basin ; the distribution of the fourth spatial pattern is difficult to describe and forms several centers of positive and negative load ; several centers of positive and negative load also appear, the distribution of load fields of the fifth spatial pattern of year, spring and winter represents the situation of " +, -, + " from southeast to northwest ; the complexity of the sixth spatial pattern is more stonger than that of the fourth and the fifth spatial pattern, several centers of load fields of year and each season often appears inverse situation of the positive and the negative load. but the centers are still most in zhungeer basin, chaidamu basin and talimu basin
第一空間型中，年和四季都是正荷載占據絕對優勢，特別是冬季降水場皆為正值，只是西南地區由於受西南季風等系統的影響，表現為與其它地區的不同；第二空間型的特點如下：年和四季分佈皆為正荷載占據大部分區域，負荷載中心年、春季和秋季分佈中都是位於塔里木盆地西部地區；第三空間型正荷載高值中心除秋季外都是處在準格爾盆地以東地區，負荷載中心多在柴達木盆地以東地區，秋季卻處于準格爾盆地以東地區；第四空間型分佈就較復雜無章法可言，形成多處正負荷載中心；第五空間型特徵是這樣的，同樣是多個荷載中心出現，年、春季和冬季中的荷載場分佈從東南到西北大體呈現「 + 、 - 、 + 」的特點；第六空間型分佈的復雜程度較之第四、第五空間型更大，年和各季分佈比較中多個荷載中心常出現正負相反的情況，但中心仍以柴達木盆地、準格爾盆地和塔里木盆地為主。分享友人