泥炭環 的英文怎麼說
中文拼音 [nítànhuán]
泥炭環
英文
peat ring-
Paleoclimatic and paleoenvironmental evolution since the late glacial epoch as recorded by sporopollen from the hongyuan peat section on the zoig 234 ; plateau, northern sichuan, china
川北若爾蓋高原紅原泥炭剖面孢粉記錄的晚冰期以來古氣候古環境的演變According to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field, including lithology, size distribution, sedimenta ry structure, geochemistry and paleontology etc., the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt. it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal. the peat flat is the important paleoenviron ment for coal accumulation. the tidal channel destroys the coal bed. the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation
根據肥城煤田石炭系太原組的巖性、粒度分佈、沉積構造、地球化學及古生物等沉積特徵，將該區晚石炭世古地理劃分為碳酸鹽開闊臺地和潮坪環境，認為太原組形成於潮汐作用為主的陸表海海岸，泥炭坪是成煤的重要古地理環境，潮渠對煤層有一定的破壞作用，地殼的脈動性振蕩作用是控制沉積環境演化和聚煤作用的主要因素。Abstract : according to sedimentary characteristics of the carboniferous taiyuan formation in feicheng coal field, including lithology, size distribution, sedimenta ry structure, geochemistry and paleontology etc., the carboniferous paleoenvironme nt of this area is divided into carbonate open platform and tidal flat environme nt. it is recognized that the taiyuan formation is formed in the epicontinental c oast which is dominated by the tidal. the peat flat is the important paleoenviron ment for coal accumulation. the tidal channel destroys the coal bed. the pulsative vibration of the crust is the major factor which controls the evolution of the sedimentary environment and the coal accumulation
文摘:根據肥城煤田石炭系太原組的巖性、粒度分佈、沉積構造、地球化學及古生物等沉積特徵，將該區晚石炭世古地理劃分為碳酸鹽開闊臺地和潮坪環境，認為太原組形成於潮汐作用為主的陸表海海岸，泥炭坪是成煤的重要古地理環境，潮渠對煤層有一定的破壞作用，地殼的脈動性振蕩作用是控制沉積環境演化和聚煤作用的主要因素。Phytolith plays an important role in the study of paleobotany and paleo - environment because of its small, high yield, and its ability of anti - erosion and high - temperature resistant
摘要泥炭地作為環境變化的敏感帶，成為當前環境氣候研究的熱點之一。Development and creation of the green peat fertilizer
泥炭綠色環保肥料的發展與創新In qinshui basin, the fresh - water peat swamp facies and forest peat swamp facies were the sedimentary environments of forming good reservoirs, but the drained peat swamp fecies was difficult to form good reservoirs in general
在沁水盆地，活水泥炭沼澤相以及森林泥炭沼澤相是形成有利儲層的沉積環境，而乾燥泥炭沼澤相一般難以形成有利的儲層。Although maqiao sites were high and no silt or peat layers, cultural missing rinks possibly existed between the liangzhu culture and the maqiao culture
雖然綽墩遺址地勢較高，遺址上沒有形成淤土層和泥炭層，但綽墩遺址良渚文化與馬橋文化之間可能存在著文化缺環。Jakarta, indonesia a new wwf monitoring report released today reveals that asia pulp paper, one of the world s largest paper and pulp companies, is going to destroy one of the most delicate of all remaining ecosystems in indonesia - the peat swamp forests of kampar peninsula in sumatra
世界自然基金會今天發放的最新監察報告，揭露全球最大的紙漿及紙張生產商之一金光集團又稱亞洲漿紙業有限公司下稱金光集團，計劃把印尼蘇門答臘坎帕半島的泥炭沼澤林，亦即該國僅餘的生態系統中最脆弱的一環徹底摧毀。Pollen analysis a means of obtaining information on the composition and extent of past floras and environments by examining fossil pollen grains, spores, and similar structures in peat and sedimentary deposits
花粉分析：指通過檢測花粉化石、孢子以及在泥炭和沉積物中類似的結構，以獲得歷史上曾有過的植物區系、組分以及分佈范圍與環境信息的方法。It shows that phytolith has its own advantage in paleo - evironmental reconstruction of peat bogs, and will be of great help in discriminating the palaeo - climatic change
對泥炭沉積中的植硅體進行了分析，初步證實植硅體對重建泥炭地古環境變遷模式起著重要的作用，對提高古氣候變化的解析度有很大的幫助。Since the end of 1980 " s, geologists have paid more and more attention to the tropical woody and domed peats and peatland in southeast asia, have got generous data and observation results, and have opened up a new prospect in correlation of peat with coal - forming environment
80年代末以來，人們逐漸把注意力集中在東南亞熱帶木本穹丘狀高位泥炭和泥炭地，獲得了大量數據資料和觀察結果，開創了泥炭與煤形成環境對比研究的新局面。The results are shown as the followings : on the basis of studies of depositional environment of source rock and its petroleum potential assessment, the biomarker compositions of the five source beds ( hq, j2k, jiy, tjt, tsh ) in kuche basin are analyzed in detail and the effects of depositional environment and maturity on the biomarker compositions are also discussed. the results show that there is not clear correlation between the distribution of biomarker composition and the ages of triassic and jurassic. it is proposed for the first time in the kuche basin that the changes of biomarker composition in the coal can be classified into three stages with the maturity, and the regular changes of different biomarker parameters in the coal are revealed
以烴源巖沉積環境為背景，詳細剖析了庫車前陸盆地五套烴源層（ j _ 2q 、 j _ 2k 、 j _ 1y 、 t _ 3t 、 t _ 3h ）中煤、炭質泥巖、湖相泥巖、煤系泥巖的生物標志物組成特徵，分析了沉積環境、成熟度對生物標志物組成的影響，指出同一烴源層在盆地不同地區生物標志物組成的差異，並認為生物標志物組成特徵與三疊系和侏羅系的時代對應關系不明顯。Based on geological environment, bi - model volcanic series, sedimentary formation and geochemical features of volcanic rocks, it is held that the deposits were most probably formed in the carboniferous back arc rifted environment
根據礦床產出地質環境、雙峰式火山巖系、沈積建造以及火山巖地球化學特徵，推斷昆侖式火山巖型塊狀硫化物銅礦床最可能形成於泥盆紀石炭紀弧后拉張構造環境。分享友人