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Home > chinese-english > "古特提斯" in English

English translation for "古特提斯"

paleotethys
Example Sentences:
1.The studies on the volcanic rocks from these two areas provide new evidences for understanding the paleo - tethyan evolution
这两个地区的火山岩研究为了解古特提斯的演化提供了新的证据。
2.Shrimp dating of carboniferous jinshajiang ophiolite in western yunnan and sichuan : geochronological constraints on the evolution of the paleo - tethys oceanic crust
古特提斯洋壳演化的同位素年代学制约
3.All in all , in carboniferous nujinshan ophiolite melange , petrographic category and their geochemical characteristics can be correlated with representative ophiolite melange in the world . this discovery offered a convincing evidence from petrology , it tes
这一发现提供了一个令人信服的岩石学证据,它表明了昌宁?孟连构造带的确是古特提斯洋的残迹。
4.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陆的主要部分都位于赤道附近及南半球,大致表现为沿纬度、呈东西向排列的特征,中国及邻区的小陆块群在古生代始终都处在劳伦大陆、西伯利亚与冈瓦纳大陆之间;随着西伯利亚大陆的快速北移,在劳伦大陆与冈瓦纳大陆的西部地区发生南北向拼合,亚皮特斯洋和里克洋的消亡,到古生代晚期形成统一的泛大陆;而冈瓦纳大陆的东部(澳大利亚和印度等)则逐渐向南移动、离散,地壳张开,构成古特提斯洋;中国及邻区的小陆块群则一直处在古特提斯洋中,保持离散状态,总体上缓慢地向北运移,并逐渐转为近南北向的排列方式,石炭纪到三叠纪才在天山兴安岭、昆仑山、秦岭大别、金沙江和绍兴十万大山等地段发生一系列局部性的陆陆碰撞,使中国大陆地块的大部分逐渐并入欧亚大陆。
5.Our research work was carried out effectively and fruitfully . this will give exact chronology and sedimentary evidence to the research of the biostratigraphy and thrust slice type stratigraphy of the nongba area ; will provide more full and accurate geological gist for the tectonic evolutions of paleotethyan located in southern part of " three rivers " ; and will provide new reference to the paleolithofacies palaeogeography pattern reconstruction of the changning - menglian oceanic basin
这些工作将为滇西南耿马弄巴地区生物地层学和造山带地层学的研究提供准确的时代和沉积学证据;为“三江”南段古特提斯的构造演化提供更为翔实的地质依据,也为恢复昌宁?孟连洋盆的古地理格架提供了新的参考。
6.There are 25 genera and 47 species of conodont , 4 genera and 6 species of coral and some foraminifera . ch . 4 biostratigraphical regions based on the study on the conodont , coral and foraminifera fossils in research area , it was discovered that the biota features are resemble to the south china . so a conclusion can be drawn that the research area and south china belong to the same biogeographical region
生物地层分区本文通过对牙形刺、蜒类、珊瑚等化石的对比研究,发现研究区的生物群特征与华南区生物群相近,这表明在该区早、晚石炭世与华南区及东古特提斯区同属一个生物地理区系。
7.The study areas are located in the jinshajiang zone , nw yunnan and sw part of the shizong - mile zone ( jianshui ) , se yunnan respectively , and tectonically belong to the east part of the paleo - tethys tectonic domain . the jinshajiang zone in nw yunnan was a joint terrain between the yangtze and the gondwana blocks , and the shizong - mile zone delineates a suture line between the yangtze and cathaysian blocks
研究区分别位于滇西北金沙江带和滇东南师宗-弥勒带西南段建水地区,构造上位于古特提斯构造域的东段,其中滇西北金沙江带是扬子陆块与冈瓦纳陆块的交汇部位,而师宗-弥勒带则分隔了扬子陆块与华夏陆块。
8.Based on the geological , stratigraphic and geochemical characteristics of the ophiolitic melange , island - arc and rift volcanic rocks from the jinshajiang zone , an archipelagic tectonic model with multi - rift and multi - subduction is proposed to explain the evolution of jinshajiang paleo - tethys . the ophiolitic melanges of the jinshajiang zone are mainly outcropped at baimangxueshan , tongduo , gongka , dongzhulin and jiyidu in the deqin county . the geochemistry of major and trace elements of the jinshajiang ophiolite shows its geochemical characteristics are similar to those of the more and island - arc volcanic rocks , but different from those of the typical n - mopjb
金沙江蛇绿混杂岩主要分布在德钦县的白茫雪山、通多、共卡、东竹林和吉义独地区,主量和微量元素地球化学特征研究表明,金沙江蛇绿岩不具有典型n - morb的地球化学特征,而具有介于morb和岛弧之间的地球化学特征,暗示它并非形成于宽阔的大洋环境,不是古特提斯在滇西北地区的主缝合带,可能是古特提斯多岛洋体系中的一个弧后盆地。
Similar Words:
"古特施泰因" English translation, "古特什" English translation, "古特水坝索赔案" English translation, "古特斯穆茨" English translation, "古特松" English translation, "古特提斯海" English translation, "古特瓦尔德" English translation, "古特瓦尔多娃" English translation, "古特瓦因" English translation, "古特韦洛娃" English translation