- i型
- i: pron. (pl. we ) 〔人稱(chēng)代詞，第一人稱(chēng)，單 ...
- type: n. 1.型，類(lèi)型，(工業(yè)產(chǎn)品的)品種；風(fēng)格，型式。 2 ...
- type i and type ii errors: i型和ii型錯(cuò)誤
- collagen type i: 膠原Ⅰ型
- counter model type i: 一型計(jì)數(shù)模型
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i-type中文什么意思
- i型
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例句與用法
- Gas clothes dryers - volume i - type 1 clothes dryers
燃?xì)飧梢聶C(jī).卷1 . 1型干衣機(jī) - Genetically , they are the transition between i - type and s - type granites , formed in the tectonic environment of late orogenic epoch , directly related to the south mongolian compound orogeny
它們均形成于造山晚期構(gòu)造環(huán)境，與南蒙古復(fù)合造山作用有直接關(guān)系。 - 3 ) the uniformity and the stability of a - si : h solar cells have been studied and we discussed the influence of i - type thickness and p - type u c - si : h to the uniformity of a - si : h solar cells
3 )非晶硅太陽(yáng)電池一致性及穩(wěn)定性的研究。主要討論了i層厚度及p層微晶對(duì)電池一致性的影響和i層厚度對(duì)穩(wěn)定性的影響。 - The qiongzhong and danxian batholiths , as the largest early mesozoic syntectonic granite intrusions in hainan island , are mainly composed of porphyritic biotite two - feldspars granitoids , in which alkali - feldspar phenocrysts and dark minerals are foliated mostly in we - direction . the granites are of metaluminous i - type . major and trace elements show co - variations with sio2 , suggesting the fractional crystallization of plagioclase , hornblende , apatite and ti - fe oxides in the evolution of the granites
花崗巖的主量元素和部分微量元素成分與sio _ 2呈良好的相關(guān)關(guān)系，顯示出明顯的斜長(zhǎng)石、角閃石、磷灰石和ti - fe氧化物等的分離結(jié)晶作用，總體上它們與大陸島弧花崗巖的微量元素豐度和分布特征相似，系統(tǒng)地虧損ba 、 nb 、 sr 、 p和ti等元素。 - Comparing with the granitoid from jiaodong guojialing in mineralogy , the minerals in the granitoid in nimu - qushui granitoid crystallized in the environment of oxidization , the granitoid has a characteristic of rich volatile components and a high content of alkali , the rock - forming minerals and accessory minerals have a characteristic of i - type granite , and the granite shows a characteristic in favor of an and cu ore formation
通過(guò)與膠東郭家?guī)X地區(qū)的花崗巖類(lèi)的礦物學(xué)進(jìn)行對(duì)比，可知本區(qū)花崗巖類(lèi)礦物結(jié)晶時(shí)處于氧化狀態(tài)，具有富含揮發(fā)分的特征，堿質(zhì)含量高，造巖礦物及副礦物表現(xiàn)出型花崗巖特征，具有殼幔混源物質(zhì)，表現(xiàn)出有利于金、銅礦形成的花崗巖類(lèi)的礦物特征。