天堂国产午夜亚洲专区-少妇人妻综合久久蜜臀-国产成人户外露出视频在线-国产91传媒一区二区三区

當(dāng)前位置:主頁(yè) > 科技論文 > 地質(zhì)論文 >

高溫高壓下殼幔含水礦物電導(dǎo)率實(shí)驗(yàn)研究

發(fā)布時(shí)間:2018-06-27 18:05

  本文選題:電導(dǎo)率 + 高溫高壓實(shí)驗(yàn) ; 參考:《中國(guó)科學(xué):地球科學(xué)》2016年03期


【摘要】:含水礦物是地殼、地幔,尤其是俯沖帶內(nèi)的重要礦物.高溫高壓下殼幔含水礦物電導(dǎo)率實(shí)驗(yàn)研究是一個(gè)相對(duì)較新的研究方向.隨著實(shí)驗(yàn)技術(shù)的不斷進(jìn)步,很多高壓相含水硅酸巖礦物的電導(dǎo)率測(cè)定工作得以開展,在有效控制溫度、壓強(qiáng)和氧逸度等條件下,含水礦物的電導(dǎo)率實(shí)驗(yàn)數(shù)據(jù)可以對(duì)地球內(nèi)部水的分布提供制約.本文介紹了已有的蛇紋石、滑石、水鎂石、phase A、super hydrous phase B、phase D含水礦物在高溫高壓下的電導(dǎo)率實(shí)驗(yàn)研究,對(duì)各含水礦物電導(dǎo)率數(shù)據(jù)的有效性進(jìn)行了分析,并重點(diǎn)介紹了電導(dǎo)率測(cè)試含水礦物脫水對(duì)全巖電導(dǎo)率的影響以及壓強(qiáng)對(duì)含水礦物電導(dǎo)率的影響.在已有數(shù)據(jù)的基礎(chǔ)上,對(duì)含水礦物的導(dǎo)電機(jī)制以及俯沖帶的電結(jié)構(gòu)進(jìn)行了探討.最后對(duì)今后的研究前景及潛在的研究領(lǐng)域進(jìn)行了展望.
[Abstract]:Water-bearing minerals are important minerals in the crust and mantle, especially in subduction zones. Experimental study on conductivity of water-bearing minerals in crust and mantle under high temperature and pressure is a relatively new research direction. With the development of experimental technology, the determination of electrical conductivity of many high-pressure water-bearing silicate minerals has been carried out. Under the conditions of effectively controlling temperature, pressure and oxygen fugacity, The experimental data of conductivity of water-bearing minerals can restrict the distribution of water in the earth's interior. In this paper, the electrical conductivity of phase A super hydrous phase Bu phase D minerals of serpentine, talc and brucite at high temperature and high pressure are studied. The validity of conductivity data of these minerals is analyzed. The effect of dehydration of water-bearing minerals on the conductivity of the whole rock and the effect of pressure on the conductivity of water-bearing minerals are introduced emphatically. Based on the available data, the electrical conduction mechanism of water-bearing minerals and the electrical structure of subduction zones are discussed. Finally, the future research prospect and potential research field are prospected.
【作者單位】: 中國(guó)地質(zhì)大學(xué)地質(zhì)過(guò)程與礦產(chǎn)資源國(guó)家重點(diǎn)實(shí)驗(yàn)室;
【基金】:國(guó)家自然科學(xué)基金項(xiàng)目(批準(zhǔn)號(hào):41590623,41472040) 中央高;究蒲袠I(yè)務(wù)費(fèi)專項(xiàng)項(xiàng)目(編號(hào):CUGL150801) 地質(zhì)過(guò)程與礦產(chǎn)資源國(guó)家重點(diǎn)實(shí)驗(yàn)室自主研究課題(編號(hào):MSFGPMR201408)資助
【分類號(hào)】:P542.5

【相似文獻(xiàn)】

相關(guān)期刊論文 前2條

1 張啟新;李潔;叢穩(wěn);;地下水電導(dǎo)率與礦化度相關(guān)關(guān)系分析——以甘肅省河西走廊張掖盆地為例[J];地下水;2010年06期

2 ;[J];;年期



本文編號(hào):2074766

資料下載
論文發(fā)表

本文鏈接:http://sikaile.net/kejilunwen/diqiudizhi/2074766.html


Copyright(c)文論論文網(wǎng)All Rights Reserved | 網(wǎng)站地圖 |

版權(quán)申明:資料由用戶19e08***提供,本站僅收錄摘要或目錄,作者需要?jiǎng)h除請(qǐng)E-mail郵箱bigeng88@qq.com