盆嶺地形 的英文怎麼說
中文拼音 [pénlǐngdexíng]
盆嶺地形
英文
basin and range landscape-
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。The city had over 250 thousand inhabitants in 2000, of which the majority was uyghurs. because of its geographical condition, the foehn phenomenon occurs and raises average temperature to 32. 7 degrees in july
由於吐魯番盆地四周的山嶺高聳,盆地內部受熱快而散熱慢,形成了那裡夏天高溫乾燥的氣候,在舉辦自行車賽的7月,平均氣溫高達32 . 7度。Basin and range landscape
盆嶺地形Based on the theory of plate tectonics and the new knowledge of continental dynamics, this paper starts mostly with tectonic analysis and then makes a comprehensive view on the characteristic of stratum composition, gold mine mineralized, magmatic activity as well as ruptures activity to discuss the yanshanian tectonic evolution of the xiaoqinling area under the regional tectonic framework of qinling orogenic belt
本文以板塊構造理論和大陸動力學研究的新認識為指導,採用以構造分析為主線,結合區內地層沉積、金礦成礦、巖漿活動以及南北兩側斷陷盆地形成演化等綜合分析,在秦嶺區域構造大框架下對小秦嶺燕山期的構造演化特徵進行探討。The mega - scale basin - and - range tectonics and other micro - geomorphology created favourable tectonic and geomorphologic conditions for the ore - formation of in - situ leachable sandstone - type uranium deposits
新構造所形成的巨型盆嶺構造及其它微地貌為可地浸砂巖型鈾礦成礦創造了有利的地質構造和地貌條件。These phenomena show that the fault has strongly activities at the same time. at that time tan - lu fault zone occurred a large - scale left - lateral displacement. the strike - slip movement on the tan - lu fault zone cau sed the zhangbaling uplifting which became source region and the hefei basin appeared strike - slip flexure at the west side of the fault
說明了控盆斷裂?郯廬斷裂帶在該時期具有強烈活動,且以大規模走滑運動為主,郯廬斷裂帶的走滑使得東側張八嶺進一步快速隆升,仍構成沉積物源系統;在斷裂西側,合肥盆地因走滑而撓曲,形成沉積可容空間。分享友人