泥炭形成 的英文怎麼說
中文拼音 [nítànxíngchéng]
泥炭形成
英文
peat formation-
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。Thick accumulations of peat can form only if the swamp basin slowly subsides.
只有當沼澤盆地慢慢下陷時，厚厚的泥炭堆積才能形成。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。Peat, the first stage in the formation of coal, is a low-rank material.
泥炭是煤形成的第一階段，是一種低質煤。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。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。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