積雲期 的英文怎麼說
中文拼音 [jīyúnqī]
積雲期
英文
cumulus stage-
Liihe palynological data indicate a vertical paleovegetational landscape : evergreen broad - leaved forest dominated by castanopsis, lithocarpus, cycobalanopsis and anacardiaceae etc occurred on the slopes near the deposit site ; mixed coniferous / broad - leaved forest and coniferous forest occurred on the area of high elevation, and main elements were tsuga, podocarpus, pinus, picea and abies etc. seven paleoclimatic parameters of liihe area estimated include mat ( 13. 3 - 20. 9c ), wmt ( 22. 5 - 27. 5c ), cmt ( 2. 5 - 12. 6c ), dt ( 12. 1 - 24. 8c ), map ( 803. 6 - 1254. 7mm ), mmap ( 179. 4 - 281. 9mm ) and mmip ( 10. 2 - l8. 5mm ). yangyi palynoflora comprises of 52 palynomorphs belonging to 32 families. the percentage of angiosperms is 61. 5 %, gymnosperms 9. 6 %, pteridophytes 25. 0 %, algae 3. 9 %
呂合孢粉植物群的組成反映該地區在沉積時期植被具有垂直分帶特徵,沉積地附近分佈有常綠闊葉林,包括殼斗科的青岡屬、栲屬、石櫟屬和漆樹科等植物,以及多種亞熱帶和溫帶闊葉成分;林中混生少量針葉樹(如松屬和杉科等) ;林內蕨類植物較少;距沉積地較遠的海拔較高的地區分佈由鐵杉屬、冷杉屬、雪松屬和雲杉屬組成的針闊混交林或針葉林。There are rich water cultures existing in the ethnic minorities of yunnan, which have benefited the subsistence and development of the ethnic minorities of yunnan for long, and have protected the ecologic environments of ynnnan actually
摘要雲南少數民族中存在著豐富的水文化,對于各民族長期的生存與發展有著積極的作用,同時也保護了雲南的生態環境。1rosenberg sa, lotze mt, muul lm, et al. observationsthe systemic administrations of autologous lymphokineactivated killer cells and recombinant interleukin2 to patientswith metastatic cancer j. n engl j med, 1985, 313 : 1485
茅國新,高志蘭,王前雲,等.基因重組白細胞介素2聯合殺傷細胞治療晚期肺癌癌性胸腔積液j .中華結核和呼吸雜志, 1995 , 4 ( 18 ) : 2Algae - rich carbonate of cambrian is typical sediment of foreslope facies in sandu and danzhai, eastern guizhou province. after sediment, it experiences many changes of diagenetic environment, and takes place much diagenetic altercation, among which the biggest is salt water dolomilization, and then is compaction, recrystallization, pressure solution, organic dissolution, burial dolomilization, cementation and silicification
貴州省東部三都丹寨地區中上寒武統富藻碳酸鹽巖是典型的斜坡沉積,其在沉積后漫長的地質歷史時期內,經受了諸多成巖環境的改造,發生了極大的成巖變化,最大的成巖變化為鹹水雲化,其他的成巖作用有壓實作用重結晶作用壓溶作用有機溶解作用埋藏雲化作用膠結作用及硅化作用等。Alkali basite, which came from upper mantle or lower crust, invaded through those structure, which not only bring cu et al mineralizing elements, but also the most important is that thermal energy. it cycled the formation water ( yinmin fonnation and luoxue formation ), and form alkali - rich, middle - high temperature and salinity fluid mixed with alkali - rich magmatic water. there were high rate of percolation and well voidage in the contact zone between yinmin purple stratum and yinmin rubblerocks, which is in favor of the transposition and mineralization of minerogenetic fluids
因此,總結東川稀礦山式銅礦成礦模式為沉積( fe 、 cu ) ?熱液疊加( cu )改造:晉寧-澄江期,小江深大斷裂發生走滑運動,在東川礦區造成右行旋扭及其派生構造,形成「 z 」字形落因破碎帶,同時來自深源(下地殼或上地幔)堿基性巖漿侵入,不僅帶來了大量cu等成礦物質,更重要的是提供了熱源,促使地層水(落雪組白雲巖和因民組紫色層)循環,與富堿( na和k )巖漿水混合,形成富堿中高溫高鹽度流體。Now it is thought that two formations were formed in the same period from early cambrian to early ordovician and were deposited in different parts of sea basin on the northern edge of the north china platform, based on the acritarchs contained in these formations
通過對以上兩個組中疑源類化石進行研究,認為阿牙登組應從白雲鄂博群中分出,與腮林忽洞組一同劃歸早寒武世至早奧陶世的地層中,阿牙登組與腮林忽洞組為同一時期不同局限海盆的沉積,是早古生代華北地臺最北部邊緣的沉積產物。If the cumulus continues to grow, its top will become very bright in the late stage, looking like a cabbage and reaching a height beyond 10, 000 m. by then it is called cumulonimbus
若雲塊進一步繼續發展,到了後期,雲的頂部發白炫目,外觀如椰菜花,高度可達一萬米以上,便成為積雨雲。The drum dance culture, a folk traditional culture, developing from the spring and autumn periods, tang and song dynasties, to ming and qing dynasties, originates from the family life of miao people and plays an important part in it
苗族鼓舞歷經春秋戰國、唐宋時期的文化累積,到明清時期完整形成,清代以來苗族農閑時舉辦的五種典型鼓舞彰顯了苗區閑暇文化生活形態,其象形動作在描繪苗民農耕生活情景同時又反映了農耕民族的生活規律,展示了雲貴高原及周邊山地民族豐富的農耕文化內涵。The dolostones have experienced several types of post - depositional diagenetic modifications, of which dolomitization, dissolution, recrystallization and tectonic stress processes have exerted an important effect on porosity and permeability
認為該白雲巖在沉積期后變化中經歷了多種成巖作用改造,其中影響白雲巖儲集性的作用主要有白雲石化作用、溶蝕作用、重結晶作用和構造應力作用,對白雲巖孔滲改善起了積極作用。The results demonstrate that the pingba red residua is a typical in situ chemical weathering crust, and the material sources of the profile are derived from underlying triassic dolomites, the chemical weathering of dolomite can be divided into two stages : " leaching - accumulating trend " and weathering trend ", the stable teconic and whole weathering of dolomite should be the main reason for the development of thick and consecutive red weathering crust overlying dolomite rock in central guizhou
結果顯示該剖面是下伏基巖白雲巖風化成土並累積的結果,無其他外來物源,是原位風化殼;成土過程具有兩階段模式特徵,即白雲石、方解石的溶蝕酸不溶物累積和酸不溶物進一步風化兩個階段;長時期的構造穩定和白雲巖整體溶蝕作用是黔中地區白雲巖風化殼土層厚度大、分佈連續的主要制約因素。Relying on the international 4d - class baitabu airport, the demonstration work of airport logistics park that occupied an area of 10 - 15 sq km is done by jinhai investment company
依託輻射蘇北魯南地域的國際4d級連雲港白塔埠機場,面積達10 - 15平方公里的空港物流園區正由金海投資先期規劃論證運作。Cumulus clouds may not bring rain in their early stage, but if they are to develop further, rain will fall sooner or later
初期的積雲不會帶來雨水,但若繼續發展,到某一程度便會下雨。Three passages of vapor transfer are related to the regional precipitation, especially the one carrying water from the bay of bengal. mixed cold and warm cloud portions are favorable for " catalysis - water supply ". the duration and rainfall - hit area are about half the lifecycle and rainbelt size, respectively
;降水天氣的主要水汽輸送路徑有三條,以來自孟加拉灣的西南水汽輸送帶對降水最為有利;雲系以冷暖混合雲體為主,具有發生「播撒-供應」機制有利的宏觀雲體條件;雲系降水的時段和面積一般只有雲系生命期和面積的一半。We have optimized the development intensity on a number of selected sites, including tin shui wai area 103, choi wan road site 1 phases 1 and 2, sau mau ping estate phases 13 and 14 and lam tin estate phases 7 and 8
我們在個別公屋地盤已因應其獨特情況善用地積比率,包括天水圍第一零三區,彩雲道第一號地盤第一二期,秀茂坪第十三十四期及藍田第七八期。分享友人