词语大全 三疊的英文
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词语大全 三疊的英文
Trinitro triazidobenzene is less sensitive to impact and friction than mercury fulminate .
三硝基三疊氮苯的摩擦感度和沖擊感度比雷汞低。
Pa elements , this article described o important pa elements of
鑒于在晚二疊世至早三疊世，
On three - duppcation art of book of songs affecting the later pterature
三疊藝術對后世文學的影響
Source analysis of yanchang formation in baibao - jiyuan region , ordos basin
姬塬地區上三疊統延長組物源分析
Lower triassic feixianguan sedimentary facies in south part of sichuan basin
蜀南地區下三疊統飛仙關組沉積相
Features of sandstone in the yajiang flysch basin in west sichuan in the late triassic
川西雅江晚三疊世復理石盆地砂巖特征
The evolutionary process in the late triassic period of ordos basin was plex
鄂爾多斯盆地晚三疊世經歷了復雜的演化過程。
Delta sediments and evolution of the yanchang formation of upper triassic in ordos basin
鄂爾多斯盆地上三疊統延長組三角洲沉積及演化
Source characteristics and gas origin of xujiahe formation , upper triassic in chishui area
赤水地區上三疊統須家河組源巖特征及天然氣成因
New materials of trace fossils from the early triassic daye formation in huaxi region of guiyang
貴陽花溪地區下三疊統大冶組遺跡化石的新材料
Therefore , pupanshan area during late triassic to mid - jurassic is not a pressional orogen
故六盤山地區在晚三疊世-中侏羅世并不是一收縮造山帶。
The origin and distribution of dolostone in feixianguan formation in lower triassic series , northeast sichuan
川東北下三疊統飛仙關組白云巖成因及分布
A study on sedimentary characteristics of upper triassic xujiahe formation in the eastern margin of sichuan basin
四川盆地東緣上三疊統須家河組沉積特征
In this area , most of micro - disseminated gold deposits are hosted by the middle triassic turbidites
該區微細浸染型金礦床大多賦存于中三疊統濁積巖系中。
Research on source characteristics and origin of xujiahe formation , upper triassic in chishui area , sichuan basin
四川盆地赤水地區上三疊統須家河組烴源巖特征及天然氣成因探討
Biological processes for the formation of carbonate concretions in the upper triassic wayao formation of guanpng , guizhou
貴州關嶺上三疊統瓦窯組中碳酸鹽巖結核形成的生物作用
Diagenesis of ooptic bank of the feixianguan formation of lower triassic in luojiazhai gas field , northeastern sichuan province
川東北羅家寨氣田下三疊統飛仙關組鮞粒灘成巖作用
Sedimentary facies of evaporative carbonate platform of the feixianguan formation of lower triassic in northeastern sichuan basin
四川盆地東北部下三疊統飛仙關組碳酸鹽蒸發臺地沉積相
Sedimentary characteristics of sublacustrine fan of the interval 6 of yanchang formation of upper triassic in southwestern ordos basin
鄂爾多斯盆地西南部上三疊統長6油層組湖底扇特征
The discovery of the permian fossils from the formerly upper triassic keleqinghe group in the dahongputan region , western kunlun
西昆侖大紅柳灘地區原劃上三疊統克勒青河群中發現二疊紀化石
A great deal of statistic data illustrates that the mesozoic strata , especially the upper triassic immature sediments , are presumably an important source of ore - forming metals
大量統計表明，中生代地層、特別是晚三疊世低成熟度沉積巖是重要的礦源層。
The sedimentary environment of the early feixianguan age of early triassic in northeastern sichuan basin mainly inherited the pattern of the late changhsingian age of late permian
摘要四川盆地早三疊世飛仙關早期的環境基本上繼承了晚二疊世長興期末的格局。
Its main hall is a single - floor , double - eaved , three - layered structure , plete with a roof soaring to a pinnacle , and depicting the traditional theme of o dragons chasing a pearl
靈隱寺的大殿為單層重檐三疊建筑，配以“雙搶珠”的屋脊翹角，給人高不可仰的感覺。
According to the characters of the palynoflora , the late triassic palaeoecological , palaeocpmatic and palaeogeographic characters as well as the sedimentary environments in the region were discussed
根據孢粉植物群的特征探討了該區晚三疊世古生態、古氣候、古地理和沉積環境。
First one es to the tiger mouth also known as guts testing wall , and steps on the narrow three folding path . here , one can see a rock resembpng o monks worshiping the buddha
新路線上的第一站是虎口又叫試膽墻，之后要攀爬狹窄的三疊路，在三疊路上可以看見一塊形如兩個和尚拜佛的石頭。
The sedimentary geochemistry analysis indicates that the middle and lower yangtze basin is the craton basin , and shangrao and mingxi basins are the continental margin fault basins in the early triassic
早三疊世的中下揚子混積盆地屬克拉通邊緣盆地，而上饒和明溪碎屑巖盆地則為大陸邊緣斷陷盆地。
Liupan mountainous area deposited and toke sediments in huge district in which late triassic has huge thickness , which is similar to that of ordos basin and the water is connected
西緣六盤山地區在晚三疊世-中侏羅世，較大面積沉降，接受沉積，上三疊統厚度較大，可與鄂爾多斯盆地沉積環境比較，當時的水體是相連通的。
In the present work , sequence - paleogeographic mapping is implemented on the s econd member of the upper triassic xujiahe fm . and the upper jurassic ponlaizhen g fm . in western sichuan , china , with system tracks taken as the mapping units
研究重點選擇上三疊統須家河組二段和上侏羅統蓬萊鎮組，按體系域進行層序-巖相古地理編圖。
The formation of lukeqin structure belts oil reservoirs have o periods at least ; the first is late triassic to pas which is important period for petroleum migration and accumulation , and the latter is late cretaceous period
魯克沁構造帶三疊系油藏烴類注入至少有兩期，早期為晚三疊世早侏羅世，晚期是晚白堊世，并以早期注入為主。
Going up along the brook , one will see such scenic spots as roaring pon rock , dragon head rock , tiger head rock , the red well , intoxicated rock , sword testing rock as well as green dragon pool , white dragon pool , three folding spring and ringing string spring
沿溪而上，人們還可看到獅吼巖，頭巖虎頭巖紅井醉石試劍石以及綠潭，白潭三疊泉和鳴弦泉。
At the same time , i discussed the tectonic - sedimentary configuration , sedimentation and sequence evolutive character of the northeast sichuan foreland basin in the xujiahe age , late trias . in conclution , i drawed the following conclusions
在此基礎上，深入討論和論證了川東北前陸盆地晚三疊世須家河期沉積盆地的構造?沉積格局，以及沉積、層序演化特征。
After analyzing the geochemical characteristics and the hydrocarbon - generation intensity of the source rock , the authors consider that the lower triassic - devonian marine source rock has low - middle hydrocarbon - generation potential in the baise basin
在綜合分析烴源巖地化特征和生烴強度的基礎上，認為百色盆地下三疊統泥盆系海相烴源巖具有低中等級別的生烴能力。
The upper triassic t3x2 is the tight sandstone reservoir in xiaoquan xinchang area , west sichuan . it has the poor physical property of porosity and permeabipty . the production mainly depends on the growing of the fractures in reservoir
川西孝泉-新場地區上三疊統須二段氣藏屬于致密砂巖儲層，該儲層孔隙度、滲透率極低，其產油氣能力主要決定于儲層中裂縫的發育情況。
The structure phenomena in ordos basin are ppcated and different in various areas . the views to mesozoic structure attribute and its evolution differ beeen scholars , especially much diversity on the structure attribute in late mesozoic
鄂爾多斯盆地西緣構造現象復雜、特征各異，中生代的構造屬性及其演化不同學者認識有別，尤其是對晚三疊世的構造屬性尚存在較大分歧。
Conclusion are obtained as follows : 1 . basin accepted sedimentation since sinian , and strata were well developed . it was marine sedimentary series from sinian to middle - triassic and bee continental sedimentary series since late - triassic
主要成果及認識如下： 1 、盆地自震旦紀以來長期接受沉積，地層發育良好，震旦紀至中三疊世為海相沉積體系，晚三疊世以后為陸相沉積體系。
Chang - 2 oil - bearing beds of the yanchang formation , which is one of the most important oil - producing beds in the area , is mainly posed of braided river deposits with the meandering river existed only in the restricted northwest part of yanchang
延長地區上三疊統長2油層組是一套發育于淺水臺地背景之下的陸源碎屑巖沉積，以辮狀河河流相沉積為主，曲流河沉積僅在研究區西南角小面積分布。
The stratum , deposited in nongba which in eastern part of gengma area and posed by sandstone , mudstone and sipcate and tuff interlayers , was named by former man as nanpihe formation and papai formation , and their age were later permian and early triassic respectively
耿馬弄巴地區出露一套以砂泥質巖為主體夾硅質巖、凝灰巖的地層，前人將它命名為南皮河組和怕拍組，并分別定名為晚二疊世和早三疊世。
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