嶺紀 的英文怎麼說
中文拼音 [lǐngjì]
嶺紀
英文
mineki-
Distant effect of jurassic collisions of qiangtang terrane, lasa terrane and paleo - pacific land onto the eurasian land made east qinling - dabie mountains in a compressional circumstance for a long time, and suppressed its orogenic extension ; whereas, cretaceous late - collisional extension and appearance of west pacific trench - arc - basin system relieved east qinling - dabie mountains of external compression, instantly result in violent orogenic lithosphere delamination - extension and depressurized - calefactive melting, and consequently, led to the formation of large scale early cretaceous granitoids and intermediate - acidic volcanic rocks
羌塘地體拉薩地體和西太平洋古陸在侏羅紀與歐亞大陸拼貼碰撞的遠距離效應使東秦嶺大別造山帶長期處于擠壓環境，伸展作用被抑制白堊紀的碰撞晚期伸展和西太平洋溝弧盆體系的遠距離效應使東秦嶺大別地區的外部擠壓消失，導致造山帶巖石圈迅速強烈拆沉伸展和減壓增溫熔融，從而形成大規模早白堊世花崗巖類和中酸性火山巖。From the cambrian to the early middle ordovician, the cambrian radiolaria and the early ordovician conodonts of the erlangping trough in the northern part of eqm, and the cambrian trilobites and early ordovician conodonts as well as cephalopods of the northern xichuan shelf in the southern part of eqm belonged to the south china province, while the cambrian trilobites and the early ordovician conodonts of the southern xichuan shelf belonged to the south china province with some elements of the north china province
在寒武紀至中奧陶世早期，東秦嶺北部二郎坪海槽的寒武紀放射蟲和早奧陶世牙形石與東秦嶺南部浙川陸棚北部的寒武紀三葉蟲、早奧陶世牙形石和頭足類屬華南生物省，而浙川陸棚南部的寒武紀三葉蟲和早奧陶世牙形石屬于華南生物省，兼有華北生物省分子。Distribution and occurrence of permian coal bearing measures in matouling well field
馬頭嶺井田二疊紀含煤巖系分佈賦存規律Thus, it can be clearly recognized that the global continents located at near equator and southern hemisphere, showed the characteristics of range along latitude ; chinese continental blocks still located among the laurentia, siberia and gondwana in paleozoic ; following the fast moving of siberia plate to northwards, the amalgamation in north - south direction at the western parts of laurentia and gondwana, subducted the lapetus and rheic oceans, until to form the uniform pangea in the late stage of paleozoic ; however australia and india plates in eastern gondwana move and disperse gradually to southwards, to extend crust and form the paleo - tethys ocean ; the chinese continental blocks and adjacent blocks still located in paleo - tethys ocean, preserved the status of dispersion, gradually moving to northwards, showed the characteristics of range along north - south orientation, until carboniferous and triassic a series of local collisions happened in tianshan - hing ' anling, kunlun, qinling - dabie, jingshajiang and shaoxing - shiwandashan zones, thus the most part of chinese continental blocks amalgamated to eurasia continent
由此可以清晰地看出，在古生代早期全球各大陸的主要部分都位於赤道附近及南半球，大致表現為沿緯度、呈東西向排列的特徵，中國及鄰區的小陸塊群在古生代始終都處在勞倫大陸、西伯利亞與岡瓦納大陸之間；隨著西伯利亞大陸的快速北移，在勞倫大陸與岡瓦納大陸的西部地區發生南北向拼合，亞皮特斯洋和里克洋的消亡，到古生代晚期形成統一的泛大陸；而岡瓦納大陸的東部（澳大利亞和印度等）則逐漸向南移動、離散，地殼張開，構成古特提斯洋；中國及鄰區的小陸塊群則一直處在古特提斯洋中，保持離散狀態，總體上緩慢地向北運移，並逐漸轉為近南北向的排列方式，石炭紀到三疊紀才在天山興安嶺、昆侖山、秦嶺大別、金沙江和紹興十萬大山等地段發生一系列局部性的陸陸碰撞，使中國大陸地塊的大部分逐漸併入歐亞大陸。Since quaternary period, because of the rising of the daxinganling mountains and the yanshan mountains this area is the boundary of the geology, geomorphy and climates of the east and west china and north china and northeast china, and it is the sensitive area of the environmental change, too
內蒙古克什克騰旗位於大興安嶺山脈和燕山余脈七老圖山脈的交匯處，第四紀以來，由於大興安嶺山脈和燕山山脈的隆升，本區又成為中國東西部和華北與東北地區地質地貌和氣候上的分界線，也是環境變化的敏感地區。Lingnan begins a new era of internationalisation
嶺南大學開創國際化新紀元From the late carboniferous to the end of permian, the spores of the shishuyuan trough were from the north china province, and the marine sediments were absent in the southern part of eqm
晚石炭世至二疊紀末，柿樹園海槽的孢子見于華北生物省，東秦嶺南部缺乏海相沉積。This extensional activity is similar to the basin - and - range province of western america, and can be thought as an intra - continental tectonic system
此外，揚子地塊西緣二疊紀的大陸伸展作用類似於美國西部的盆嶺區，總體表現為大陸板塊陸內構造體制。Sequence of primary sedimentary structures and sedimentary environment for the permian coal measures in the luling mine of the huaibei coal field
淮北煤田蘆嶺井田二疊紀含煤巖系原生沉積構造序列與沉積環境Late quaternary slip - rate on the altun fault west to the qarqan river
西秦嶺北緣斷裂帶黃香溝段晚第四紀水平位移特徵及其微地貌響應Taizhou wuzhou shoes co., ltd. located in the seashore resort city - wenling city zhejiang province, founded in 1980s, is a professional shoes corporation that combines manufacture, research and sale together
浙江臺州五洲鞋業有限公司，座落於千年之光的海濱之城溫嶺市，公司創建於19世紀80年代，是一家專業從事產，學，研，銷為一體的鞋業公司。Lingnan university " lingnan " or " the university " received hk 1. 2 million donations from ms. bess tsin man - kuen, director of karmax ltd. in recognition of ms. tsin s generous support, the university named its language laboratory in memory of ms. tsins father mr. tsin shui - sang, who was a late alumnus of the guangzhou lingnan university
嶺南大學下稱嶺大獲嘉銘有限公司董事及仁濟醫院董事局主席錢曼娟女士捐贈港幣一百二十萬元。由於錢女士的父親錢瑞生先生生為前廣州嶺南校友，嶺大將實驗室命名為錢瑞生語言實驗室，以作紀念。Yung fung shee memorial centre, 79 cha kwo ling road, kowloon
九龍茶果嶺道79號容鳳書紀念中心G f, yung fung shee memorial centre, 79 cha kwo ling road, kwun tong, kln
九觀塘茶果嶺道7 9號容鳳書紀念中心地下Situated in the east of lo wai, tang chung ling ancestral hall is the main ancestral hall of the tang clan in lung yeuk tau. the hall was built in the early 16th century in memory of tang chung ling, the founding ancestor
松嶺鄧公祠，位於老圍東面，於十六世紀初為紀念開基祖鄧松嶺公而建，是龍躍頭鄧氏的祖祠。With a fascinating gondola ride to the top of the sulphur mountain will accomplish an excellent view of scenery. the visit will even complement with a short stop at the bow falls and shopping time in the banff city center area
山峻嶺，繼而參觀班芙市內之弓河瀑布拍照留念，各團友更可在市中心隨意選購紀念品及午膳，繼前詩情畫意的露意詩湖，面對長年累月為冰雪掩蓋的維多利亞冰川，超然脫俗。Tung chung ( citygate fu tung ), airport supporting area, airport passenger terminal, tsing ma, tai wo ping chak on, lok fu wang tau hom, wong tai sin, diamond hill, ngau chi wan choi hung ( east ) ping shek, kai yip richland gardens, ngau tau kok telford gardens, kwun tong ( millennium city yue man square ), kwun tong recreation ground tsui ping ( south ), lam tin ( sceneway garden kai tin ), sheung tak kwong ming, tiu keng leng, tseung kwan o town centre, hang hau, king lam, po lam metro city
東涌（東薈城富東） ，機場後勤區，機場客運大樓，青馬，大窩坪澤安，樂富橫頭? ，黃大仙，鉆石山，牛池灣彩虹（東）坪石，啟業麗晶花園，牛頭角九龍灣（德福花園） ，觀塘（創紀之城裕民坊） ，觀塘游樂場翠屏（南） ，藍田（匯景啟田） ，尚德廣明，調景嶺，將軍澳市中心，坑口，景林，寶林新都城Lectures which investigate into the relationship between christianity and chinese cultures are held in memory of the rev. pommerenke who donated the site at tao fung shan to the chung chi college. the site was given to him by the rev. dr. j. stewart kunkle who was a former principal of union theological seminary, ling nam university, canton
為紀念捐出小道風山土地（現屬崇基學院所有）之萬倫牧師及約翰牧師（前附屬嶺南大學之協和神學院院長） ，教牧事工部邀請學有所長之學者，主講萬倫基督教與中國文化講座。On the basis of extensive field investigations and laboratory analyses on the carboniferous strata and fossils in the west qinling. to the carboniferous of lixian, there has systematically been studied in the lithostratigraphy and biostratigraphy. at the same time, a diverse of fossils form this area have detailedly been described and discussed
在對西秦嶺石炭紀地層和古生物化石資料進行廣泛的野外收集和室內分析處理的基礎上，對研究區石炭系進行了系統的巖石地層和生物地層學的劃分和對比；對所獲古生物化石進行了系統的描述和歸屬討論，形成了一套內容豐富的西秦嶺石炭紀地層古生物研究新資料。The genesis of spots in ore - bearing rock of baguamao gold deposit has been elaborated, through the geologic background, the characteristics of ore - bearing bed, the mutiperiodic mineralization and the mineral composition. the author indicates that the mottled structure of devonian system in qinling mts. resulted from the mutiperiodic activity of ore fluid and connected with the gold mineralization ， in addition ， it could be regarded as one of the important marks for gold mineralization
主要從成礦地質背景，含礦層特徵和多期成礦等方面闡述了八卦廟金礦含礦巖石中斑點的物質組成及其特徵，指出秦嶺泥盆紀含礦巖石中斑點狀構造為成礦流體多期作用的結果且與金礦化關系密切，可作為金礦化的重要標志之一。分享友人