盆地山嶺 的英文怎麼說
中文拼音 [péndeshānlǐng]
盆地山嶺
英文
basin range-
On the basis of analogic methodology, the deep gas resources of the basin is evaluated as 1116. 144 billion cubic meters, which is mainly distributed in the zones of xujiaweizi, miaotaizi, changling, yingshan, and gulong
根據松遼盆地深層天然氣區帶地質評價參數取值標準，進行區帶地質評價，並通過與刻度區類比，得出深層天然氣資源量為11161 . 44 10 ^ 8立方公尺，主要分佈在徐家圍子、廟臺子、長嶺、鶯山、古龍等區帶中。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。Camp belong to the south qinling orogenic belt middle segment palaeozoic strench basin fold indo - chinese epoch drape north part, and belong to the miliangchuan schiefer
礦區所在部位屬南秦嶺造山帶中帶古生代伸展盆地疊加印支期沖褶帶的北部，隸屬于米糧川逆沖巖片。On the basis of the analyses of peripheral ancient land, types of sand stone, light and heavy mineral associations and directions of palaeoflow, it is considered that detrital material of terrigenous origin of the upper palaeozoic in this area come from south provenance and north provenance, respectively, yinshan ancient land in the northern and east qinling ancient land in the southeastern
根據盆地周緣古陸、砂巖類型、輕、重礦物組合及古水流方向等特徵的分析，認為研究區上古生界陸源碎屑物質來自南、北兩大物源區，即北部的陰山古陸和東南部的東秦嶺古陸。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。Based on the study of geological background and structural settings, and with the geological event as the main thread, the author analyzed the development history of the regional ore - forming structures, especially, the new - forming and inherited structural systems since yanshanian movement, and the range - basin structures of marginal - pacific ore - forming domain, and the thermo - uplifting structure of the lushan ore - body as well as the yiwulushan metamorphic core complex, which are three different scale ore - forming structural systems
論文在緊密結合地質背景、構造背景研究的基礎上，以地質事件為主線，分析該地區域成礦構造的成生歷史，特別是燕山運動以來繼承及新生的構造體系格架與濱太平洋成礦構造域的盆嶺構造、閭山巖體熱隆、變質核雜巖等3個不同級別的區域成礦構造系統。Based on the local vegetation, climate and physiognomy, the region could be divided into 5 zones where the abundance of species was not similar : the middle part of qinling mountain with extremely abundant species ( about 40 species ), afterwards in file the lower part of ba mountain and the hills with about 30 species, the lower part of qinling mountain and the hills about 26 species, the middle part of the ba mountain about 20, the hanzhong basin with the least number
以漢中地區農業區劃為研究區域，蝗蟲在5個不l司區劃內的分佈是不同的。秦嶺中山區蝗總科種類最多（ 40種） ，其次分別為巴山低山丘陵區門種） 、秦嶺低山丘陵區（ 26種）和巴山中山區（ 20種） ，漢中盆地種類最少（ 14種） 。Arguments have long existed in the analysis and correlation of the sedimentary environment between jinlingsi - yangshan and fuxin - yixian basins in western liaoning province
摘要遼西金嶺寺羊山盆地與阜新義縣盆地的沉積環境分析與對比，一直存在分歧。During the work period in the southern zone of the east qinling belt, the process of sedimentation, basin quality and its interior structure and configure, important events are studied from the sinian to the triassic, especially through more than one hundred km profile across the southern zone of the east qinling belt. in the technical method, the basin dynamic analysis in the cambrian and the devonian respectively and the cycle events in the late triassic are added to the research of the belt. the some basic and important viewpoints of the orogenic - sedimentology are prompted in the study method, thought and connotation fields in this stage
在東秦嶺南帶沉積盆地演化研究中：通過對東秦嶺南帶從震旦繫到三疊系的沉積作用過程，沉積環境展布和變化，沉積盆地性質、內部結構、層序、配置和發展演化，沉積過程中重大地質事件研究；隨著全球沉積地質計劃在全球的推廣和展開，在研究內容和技術方法上，增加秦嶺造山帶層序地層學以及沉積盆地動力學探索等沉積地質學前緣學科的研究，這樣從更深入和更廣闊的角度進行了這個造山帶的沉積盆地分析，在研究方法、思路和內涵上開拓了造山帶沉積學的一些基本觀點。Through comparing the tectonic sequences stratum of triassic - paleogene period in the east of hubei, in jingmen - dangyang basin, in zigui basin and in the northeast of sichuan, on the southern margin of the eastern qinling and dabie orogenic belt, three main tectonic sequences are divided
摘要通過對東秦嶺大別山造山帶南緣鄂東地區、荊當盆地、秭歸盆地和川東北地區三疊紀古近紀的構造層序對比研究，劃分出三個大的構造層序，並分析了中上揚子地區印支期以來沉積盆地性質轉換和遷移過程與構造層序的耦合關系，揭示了東秦嶺大別造山與成盆作用過程。分享友人