拉基火山 的英文怎麼說
中文拼音 [lājīhuǒshān]
拉基火山
英文
laki-
Chagan sag is a secondary tectonic unit in chagandelesu depression, northeastern yingen - eji ' naqi basin, and the basement of the basin is a paleozoic fold belt of continental margin or island arc at the connection region of north china plate * tarim plate and kazakstan plate, with the character of erogenic belt. in working area and its adjacent area, the forming tectonic setting of indosinian intrusion was that orogenic belt pressed strongly, intracontinental subduction ; that of early yanshan movement epoch was the stress field transferred from compression to extension meanwhile the incrassate crust of orogenic zone turned to extensional collapse ; and that of early cretaceous volcanics was that the area structure extensional collapse further more during the post period of orogenic phase
查干凹陷屬于銀根?額濟納旗盆地東北端查干德勒蘇坳陷內的一個次級構造單元,其盆地基底為古生代時期華北板塊、哈薩克斯坦板塊和塔里木板塊交接部位形成的陸緣或島弧褶皺帶,具有古生代造山帶的性質。研究區及鄰區印支期侵入巖形成於造山帶強烈擠壓陸內俯沖的構造環境;燕山早期侵入巖形成於由擠壓轉向拉伸、造山帶的增厚陸殼開始發生伸展垮塌的構造環境;早白堊世火山巖形成於造山期后進一步發生伸展垮塌的區域構造環境。And apatite. by these analyses and comparison with general granite both in china and the world and with the granite in other au or cu belt in china, the characteristics of the granite in this area are concluded as follows. it belongs to magnetite - i or syntectic granite and has crust - mantle mixed characteristics ; it was formed mainly by crystallization differentiation of melting magma and multiphase varied intrusion ; the degree of differentiation evolvement is not high ; the granite and its enclaves p. re congenetic ; the range of temperature is about 500 - 700, the range of pressure is about 2. 50 gpa - 4. 35 gpa, and the range of oxygen fugacity ( lg fo2 ) is - 15. 53 - - 14. 00 ; most granite bodies formed before the collision of plates, and few formed after the collision of plates
通過對測試數據的分析與綜合研究,並同中國和世界一般花崗巖類以及中國主要金、銅成礦巖體的花崗巖類進行對比,得出本區花崗巖類巖石具有以下特徵:屬磁鐵礦-型或同熔型花崗巖,其巖漿物質具殼幔混源特徵:主要由熔融態巖漿經結晶分異作用,通過多期變速上侵而形成;其分異演化程度較低;寄主巖基和包體具有同源性;巖石的形成溫度范圍約為500 - 700 ,壓力大約為2 . 50gpa - 4 . 35gpa ,氧逸度值1gfo _ 2為- 15 . 53 ? 14 . 00 ;該巖帶主要形成於板塊碰撞前消減的活動板塊邊緣期,為燕山至喜馬拉雅早期的大陸邊緣火山弧環境的產物。Two of the most active volcanoes in the world, mauna loa ( 4, 170 m high ) and kilauea ( 1, 250 m high ), tower over the pacific ocean at this site
世界上最活躍的兩個活火山冒納羅亞山(海拔4 , 170米)和基拉韋厄火山(海拔1 , 250米) ,就象太平洋上的兩個巨塔般聳立在夏威夷國家公園內。The formation of the enriched mantle ( em1 ) is attributed to the strong metasomatism - taking place between subducted yangtze lower crust and nc ( north of china ) ancient lithosphere
2 、火山巖、堿性超基性脈巖和基性脈巖(除少數外)都形成於大陸板內拉張環境。From an elevation of 1000 meters at the north end of the valley, the land slopes down steadily and for 70 miles the floor is below sea level, reaching a low point of - 86 meters at badwater, the lowest point in the western hemisphere and is considered to be one of the hottest places in the world during the summer season. every year between november and april, the weather is perhaps the most suitable for travelers
是日參觀美國面積最大的火焰谷死谷國家公園,包括公園內景色瑰麗的拉培斯基山丘zabreski point ,與全美國最低點的壞水區bad water ,此處低於海平面282尺,雖是全球最熱地區之一,每年十一月至來年四月天氣清涼,為旅遊最佳季節。During my master " degree investigation, i mainly focused on the coarse - grain stratigraphy within mesozoic basins in chengde and pingquan districts, the eastern yanshan, and did systemic provenance analysis and paleo - current direction measurement and studied the relationship among basin evolution, volcanism and tectonism. then i summarized the mesozoic basin development and the coupling characters of basin and mountain. the evolution of basin and mountain in this area can be divided into several stages : the stage of compression uplift and flexural basin during the triassic through the early jurassic, the stage of structural compression - volcanism and foreland basin during the middle and late jurassic and the stage of rift basin in the cretaceous
在野外典型路線調查的基礎上,對燕山地區東段承德、平泉地區的中生代盆地中發育的粗碎屑沉積層,進行了系統的物源分析與古流測定,並在此基礎上重點剖析了盆地的發育、火山活動、構造變動三者之間的關系,總結了本區中生代盆地發育規律及盆山耦合特徵,並將盆山演化劃分為:三疊紀?早侏羅紀的構造擠壓隆升與撓曲盆地發育階段階段,中晚侏羅紀的構造擠壓?火山活動與類前陸盆地發育階段,早白堊世的拉張斷陷盆地發育階段。You are going to explore the most beautiful view of death valley - scotty s castle. enjoy the unrivalled scenery at zabreski point. then, visit the lowest point of the united states - bad water
驅車前往美國面積最大的火焰谷死谷國家公園,參觀斯卡提斯古堡scott s castle景色瑰麗的拉培斯基山丘zabreski point ,以及美國最低的地點,低於海平面- 282 feet以下的壞水區badPermian series distributed widely in the baisin. lower permian series was composed of acid, neutral, and basic volcanics, subvolcanic rocks, volcanoclastic rocks and few normal sedimentary rocks. from western to eastern, the volcanics transited from acid volcanics to neutral and basic volcanics
二疊系在盆地內部分佈廣泛,下二疊統卡拉崗組主要發育酸、中、基性火山巖、次火山巖、火山碎屑巖及少量正常碎屑巖,由西向東火山巖由中、酸性向中、基性過渡。Under the cooperation of lifts and mantle fluids, the melting point of mantle peridotite fell, and then, extensive melting took place in the enriched mantle, which resulted in the appearance of abundant mafic dikes, ultramafic dikes and contemporaneous volcanic rocks in shandong province
綜合堿性超基性脈巖和已知的青山組的火山巖、基性脈巖年齡數據,認為山東地區中生代地殼拉張至少存在四次:即約80ma 、 100ma 、 120ma和140ma 。For helping to build paradise, kilauea ( hawaii ), one of the world ' s most active volcanoes blasts onto the list at number ten
作為世界最活躍火山之一的基拉韋厄火山,在十大自然奇觀中名列第十。From the itting lava of kilauea , to the raging rapids3 of the colorado , the natural wonders of the world are dynamic4 proof of this ectacular planet we call earth
從基拉韋厄火山噴涌而出的巖漿,到科羅拉多滔滔的激流,這些世界自然奇觀生動地證明了我們稱之為「地球」的這個星球是多麼獨特、美麗。From the spitting lava of kilauea , to the raging rapids3 of the colorado , the natural wonders of the world are dynamic4 proof of this spectacular planet we call earth
從基拉韋厄火山噴涌而出的巖漿,到科羅拉多滔滔的激流,這些世界自然奇觀生動地證明了我們稱之為「地球」的這個星球是多麼獨特、美麗。分享友人