秦嶺山地 的英文怎麼說
中文拼音 [qínlǐngshānde]
秦嶺山地
英文
qinling shandi-
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。Based on the analysis of the data on global metallogeny in the framework of geodynamics and study of the processes of continental evolution and metalloeny of of sanjiang, qinling and xingan - mongolia orogenic belts, we have reconsidered the geodynamic evlution and metallogeny during indosinian to early - yanshan movement in china, and established large - scale metallogenic model on intracontinental evolution we in orogenic belts. the main results are summarized as follow. ( 1 ) systematically gathering the data about large - scale and superlarge - scale deposits in the world and drawing up the map of global tectonics and metallogeny ; finding out the segmentation of circle - pacific ocean metallogenic belt and informing that the giant deposit clusters are the prominent feature of global metallogeny
本文在總結全球大規模成礦的地球動力學背景資料基礎上，通過深入解剖和系統對比我國三江造山帶南段、東秦嶺造山帶和興蒙造山帶中南部等典型造山帶關鍵地區以陸內演化過程為核心的地球動力學演化歷史及其成礦特徵，重新認識了我國大陸印支?早燕山期的動力學演化過程及其成礦效應，建立了關于造山帶陸內演化階段主要過程中的大規模成礦模式。The number of species in the southern slope of qinling mountain was most abundant because of distribution of some palaearctic species to the top of qinling mountain, especially species of oedipodidae, another reason may b. e the large number of endemic species in this area
秦嶺南坡種類最多，主要是有部分古北界的種類滲透分佈在中、高山地帶，特別是斑翅蝗科的種類，另外還有部分特有種。( 7 ) showing and determining the evidence and timing of the lithophere delamination occurred in qinling orogenic belt. pointing out the gold deposit in xiaoqinling - xiongershan region are mostly formed during indosinian to early - yanshan movement, related to mantle fluid injecting caused by lithosphere delamination and plutonic activity caused by further large - scale tectonic extension
初步闡述了東秦嶺地區的成礦分區和成礦特點，指出小秦嶺一熊耳山地區金礦形成的主要時期是印支一早燕山期，並且與巖石圈拆沉作用所引起的地慢流體活動和之後進一步大規模伸展作用產生的深源巖漿活動密切相關。On the basis of the types of sand stone, light and heavy mineral associations, planimetric map of sedimentary facies and directions of palaeoflow, it is considered that detrital material of terrigenous deposit of chang6 - 8 oil - beds in this area come from southwest provenance, northeast provenance, west provenance and south provenance, respectively, which are the denudation area of huating - longxian county in southwestern, yinshan ancient land in the northern, the denudation area of yantong mountain and tongxin to the west of yangjiajuzi - yinjiacheng county and qinling ancient land in the southern
根據砂巖類型、輕、重礦物組合、沉積相帶平面展布及古水流方向等特徵的分析，認為研究區延長組長6 ? 8油層組陸源碎屑物質來自西南、東北、西部和南部四大物源區，分別為西南華亭?隴縣一帶剝蝕區，北部陰山古陸，西部的楊家咀子、殷家城以西的煙筒山、同心地區剝蝕區和南部秦嶺古陸。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。Abstract : to the principle and project that tu guangazhi proposed in 1990, the gold ore deposits in qinling ( shaanxi ) may be classified into fouowing types : archean high - grade gneiss type, fine grained fragmental rock - carbonate rock - silicilith type, metamorphic fragmental rock type, volcanic rock type, explosive breccia type, intrusive rock exo - and endo - contact zone type. inthis paper, the geological characteristics, metallogenic geological setting, the source of ore - forming materials, digenic mechanism and metallogenetic epoch of gold ore deposits are also discussed
文摘:參照塗光熾先生（ 1990 ）提出的礦床類型劃分原則與金礦分類方案，將陜西秦嶺地區原生金礦劃分為太古界綠巖建造型、細碎屑巖-碳酸鹽巖-硅質巖建造型、變質碎屑巖型、火山巖建造型、隱爆角礫巖型和侵入巖內外接觸型金礦，並對各類型金礦的地質特徵、成礦地質背景、成礦物質來源、礦床形成機制及形成時代等問題進行了論述和討論。In the west qinling, qilian and longshoushan metallogenic zones, some larger - ultra larger mineral deposits were formed throughout a model of " bearing " in long course of geological evolution. studying their geologic setting of " formation " and condition of late " development " would help us to objectively realize rules for the metallization and enrichment and define reasonable thinking for research and plan for exploration
甘肅西秦嶺、祁連、龍首山等成礦帶的大型-超大型金屬礦床，是在地質構造發展演化過程中「生長」而成的；研究分析其「生」成背景與後期成「長」的條件，有利於客觀認識成礦與富集規律、合理確定研究思路與勘查方案等。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。Geology, distribution and classification of gold deposits in the western qinling belt, central china
西秦嶺地區造山型與卡林型金礦床The xiaoqinling area locates in the south margin of north china block which is bounded on the north by the taiyao fault and on the south by the luonan fault
小秦嶺位於華北地塊南緣構造帶，夾持在太要-武家山斷裂和洛南-欒川斷裂之間。According to luonan fault and shandan fault extending roughly from east to west, the qinling erogenic belt is divided into three parts : the south margin of north china block, the northern qinling and the southern qinling
秦嶺造山帶內部以洛南-欒川斷裂和商丹斷裂帶為界將其劃分為華北地塊南緣構造帶、北秦嶺構造帶和南秦嶺構造帶。The north area of weihe river is located in the joint of the qilian - north qinling orogenic belt
摘要天水渭北地區地處祁連與北秦嶺造山帶結合部位。The area in question has great conservation value as following aspects : the population of butterfly shows great species abundance ; the heterogeneity of habitat revealed by the presence of multi - subspecies and multi - morphological species provides animals a steady habitat ; the faunal character and vertical distribution of butterflies show great value of ecological study ; the mid - mountain 8002600 ? m that has better environmental condition and less human disturbance is a typical
秦嶺對東洋種的阻隔作用大於對古北種的作用。中山地帶8002600m即暖溫帶落葉闊葉林和中山針闊葉混交林帶環境狀況良好，氣候條件優越，受人為干擾少，因而物種豐富多樣性較大。研究地區具有很高的保護價值。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。In this paper, a research of spatial distribution of solar radiation and temperature over mountainous area of qinling is presented. the research is based on monthly mean temperature and sunshine ratio data of 36 meteorological observe stations over qinling zone in 1971 - 2000, and xian solar radiation data in 1961 - 2000, and 1km 1km dem data over qinling zone
本文用秦嶺地區36個氣象觀測站1971 - 2000年30年氣候整編資料的月平均氣溫、日照百分率資料， 1961 - 2000年西安日射資料，以及秦嶺地區1km 1kmdem數據，對秦嶺地區山地輻射和氣溫空間分佈進行研究。Carbon storage and carbon density of pinus tabulaeformis and pinus armandii forests at huoditang forest region in qinling mountain
秦嶺火地塘林區油松和華山松林的空間分佈格局及碳儲量與碳密度研究If project ntfp development activities are successful, the experience can be replicated in other part of the qinling mountain
如果非木製森林製品的開發活動取得成功的話，那麼，該開發經驗可以在秦嶺山脈的其它地區進行推廣。Using mountainous climate theory and gis technology, a series of radiation spatial distribution models has been set up, and the spatial distribution over qinling zone has been calculated
根據山地氣候學原理，利用gis技術，建立秦嶺地區輻射空間分佈模型，計算秦嶺山地天文輻射空間分佈。分析氣溫空間分佈的影響因子，建立秦嶺山地月平均氣溫空間分佈模型，計算秦嶺山地月平均氣溫空間分佈。Further, based on the survey and calculation the height of the caves above the luohe river, we can divide the five caves into five stages as following ( from upper to lower ) : 430ka ? p, 262ka ? p, 162ka ? p, 100ka ? pand57ka ? p
本文所研究的材料采自秦嶺山區洛河北岸同?地區不同高度的洞穴之中，屬田鼠亞科的三個種：跟田鼠microtusoeconomus 、苛嵐絨（鼠乎）鼠caryomysinez和洮州絨（鼠乎）鼠c分享友人