dabie 中文意思是什麼
dabie
解釋
棟別-
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。 -
We faced a grim and perilous situation, but i should say that on the whole, we accomplished the shift to strategic counteroffensive quite smoothly, moving rapidly into the dabie mountains
當時形勢相當嚴峻，相當險惡，但是整個地看應該說是很順利地實現了戰略反攻的任務，躍進到大別山。 -
The dabie complex suffered denudation in neogene and constitutes the source rocks of zhengyangguan formation
大別雜巖在新第三紀已經遭受剝蝕，構成了正陽關組的物源。 -
4. it is the first time that eclogite conglomerates are discovered in maotangchan and fenghuangtai formations. this suggests that ultra - high pressure metamorphic rocks in the dabie orogenic belt exhumed to the earth ' s surface in lower cretaceous. the geochemistry data indicates that the protoliths of the eclogite gravels formed in a structure setting of volcanic arc
首次在毛坦廠組、鳳凰臺組中發現了榴輝巖礫石，這一發現表明大別造山帶超高壓變質巖在早白堊世已經折返到地表，而且地球化學研究表明這些榴輝巖礫石的原巖形成於巖漿島弧構造背景。 -
A large number of studies of geochronology and geochemistry indicate that mesozoic intermediate - felsic rocks from the dabie orogen have originated from recycling of the subducted yangtze continental crust itself
摘要大量的同位素地質年代學和地球化學研究表明，大別山中生代中酸性巖為俯沖揚子陸殼再循環的產物。 -
Tianxiang goup is booming, just like an eagle flying towards a bright and brilliant future out of the dabie mountains
天翔集團尤如大別山上奮飛的雄鷹，展翅翱翔，一日千里，朝著光輝燦爛的明天騰飛！ -
East qinling - dabie mountains ; lithosphere delamination ; granitoid ; uhpm ultra - high pressure metamorphite
東秦嶺大別造山帶巖石圈拆沉花崗巖類超高壓變質巖 -
Granulite - facies retrograde metamorphism of garnet pyroxenite in muzidian, northern dabie mountains
北大別木子店石榴輝石巖的麻粒巖相退變質作用 -
An evaluation of zircon u - pb dating for metamorphic rocks and comments on zircon ages of dabie orogen
兼論大別造山帶鋯石定年 -
Multiple rotation and amalgamation processes of dabie - tanlu - sulu orogen
蘇魯造山帶復合旋轉拼貼作用 -
Architecture, kinematics and deformation analysis in dabie - sulu collision zone
運動學和巖石變形分析 -
This session will present new structural, mineralogical, petrochemical, geochronological, and geophysical data based on the drilling results and associated field studies, particularly in the dabie - sulu region
本專題將展示蘇魯地區基於鉆進和相關野外調查所獲得的構造學、礦物學、巖石學、地球化學、地球物理等方面的新的資料。 -
This research focuses on the sedimentology, basin analysis and tectonic evolution of mesozoic strata in the north margin of the dabie orogenic belt, using an integrated approach of modern sedimentology, continental dynamics, petrology, geochemistry and isotope chronology. the topics of the study include : ( 1 )
以現代沉積學和大陸動力學理論為指導，結合巖石學、地球化學、同位素年代學等諸多學科，對大別山造山帶北緣地區中生代地層進行沉積學、盆地分析以及構造演化研究。 -
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。 -
This indicates that the exhumation of the dabie orogenic belt was diachronous, and that its uplift happened from east to west and was mainly controlled by the ne fault system
揭示了大別山造山帶的折返是穿時的，隆起自東向西進行，而其控制因素主要為ne向的斷裂體系。 -
6. the mesozoic sedimentation in the north margin of the dabie orogenic belt is diachronous. from east to west, the onset of the sedimentation is successively in lower - middle jurassic, middle - later jurassic and lower cretaceous
大別山北緣中生代沉積作用具有穿時特徵，沉積作用開始時間自東向西依次為早中侏羅世、中晚侏羅世和早白堊世。 -
Through studying the stratigraphic framework of tectonic sequence, the characteristics of deposits and multi - episode tectonic movements show the eastern qinling and dabie orogenic movement and basin formation processes
晚白堊世至古近紀區域構造背景發生重大變化，構造層序記錄了晚燕山期地殼快速均衡隆升，伸展斷陷盆地形成演化過程。 -
Discovery of eclogites in the qichun areas in the southern slope of the dabie mountains and some related problems
大別山南坡蘄春等地榴輝巖的發現及相關問題 -
This paper describes distribution characteristics of helium isotopos and some trace elements in different types of rocks along dabie mountain ultrahigh pressure metamorphic complex belt as well as along liuan - caihe geo - science profile, and deals with their affecting factors and geological significance
摘要報導了大別山超高壓變質雜巖帶不同巖石類型及六安蔡河地學剖面中氦同位素和某些微量元素的分配分佈特徵，並討論了它們的影響因素及其地質意義。 -
Gravel features and tectonic implication in the carbonifereous huyoufang formation on the northern margin of dabie orogenic belt
大別造山帶北緣石炭系胡油坊組礫石特徵及其構造意義
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