The petrogenesis of intrusive rocks is discussed in this paper according to the equilibrium of minerals. It is suggests that in the Shigujian pluton, the designations of plagioclases are 15 - 25, the plagioclases are all oligoclase; the biotites are Mg-biotites, and most of the amphiboles are edenitic amphiboles or edenite; paragenetic ...

結(jié)果表明：（1）石鼓尖侵入巖中αV在线视频，斜長(zhǎng)石成分較穩(wěn)定日韓在線專區，共生角門(mén)石和黑云母為巖漿平衡結(jié)晶的礦物www.99re.com；（2）天堂寨和九資河侵入巖中污色视频在线观看，部分斜長(zhǎng)石和黑云母可能為熔蝕殘留礦物欧美黄色一、二区性交，角閃石屬于火成巖區(qū)的新生礦物，可能為斜長(zhǎng)石和黑云母發(fā)生熔融反應(yīng)所形成一本在线香蕉高清在线；（3）三個(gè)侵入體的巖石均為巖漿成因中文字幕无码乱人l伦。

Myconrrhizal fungus infected the cortical cells and formed pelotons in the cells, after it penetrated the exodermal passage cells through velamen cells. It is interesting that strain AR-18 also penetrated exodermis from the cortical cell next to it, where mycelium grew vigorously and infected inner cortical cell, even a few mycelium penetrated endodermis while there was no mycelium in the fibrovascular bundles.

真菌AR-15與金釵石斛一起培養(yǎng)時(shí)，真菌菌絲與根被細(xì)胞密切接觸并侵入根被細(xì)胞泰国一级a爰片免费视频观看，也可通過(guò)侵入根毛進(jìn)入根被細(xì)胞国产网站观看，由根被繼續(xù)侵入外皮層通道細(xì)胞，進(jìn)一步向皮層細(xì)胞侵染天天干天天碰小视频免费观看；部分根被真菌危害黄色工厂AV片，根部組織內(nèi)有大量真菌孢子和菌絲。

During the inversion of the dual lateral log, The generalized inversion method is used to invert the three parameter (the radius of the invasion zone, the resistivity of the invasion zone, the resistivity of the destination formation) and eliminate the affect of invasion zone.

對(duì)于雙側(cè)向測(cè)井反演亚洲欧洲中文字幕视频在线观看，本文將廣義逆反演方法用于消除侵入影響的三參數(shù)(侵入半徑黄色视频入、侵入帶電阻率、原狀地層電阻率)反演中99久强奸久久9毛片。

For intrusion, only those hypabyssal intrusion rocks with thickness over 15 m, having effective fracture zone, and inserted in or immediately adjacent to mature source rock, and those dikes near contemporaneous fault and within buried hill fracture zone have favorable reservoir forming condition s.

在大量的侵入巖體中日韩性爱视频中文字幕，只有侵入巖厚度大于15m，具有有效裂縫帶發(fā)育另类日韩高清精品视频在线观看免费、直接嵌置或緊鄰成熟烴源巖的淺成侵入巖a级a片，以及分布在同生斷層附近的、潛山裂縫發(fā)育帶中的脈巖具備有利成藏條件国产色网站农村。

The comparative studies of lithogeochemistry for the volcano-intrusive complexes both from Jiulongzhang and from xiangshan reveal that the chemical compositions of the volcano intrusive complexes in the two areas are very close, and the trace element spidergrams and REE patterns basically coincide with each other. It is also shown that the two volcano-intrusive complexes have the same source features and the active continental margin tectonic settings. At the same time, it is found that, from early volcanic magma activities to later intrusive magma activities, the content of SiO2 and the Rb/Sr ratio decreased, on the contrary, the content of MgO and the ratios of K/Rb, Ba/Rb and LREE/HREE increased. It is shown that the hypabyssal or ultra-hypabyssal intrusives are not the products of the volcanic magmatic differentiation.

兩地區(qū)的火山－侵入雜巖的巖石化學(xué)成分及其變化特點(diǎn)極為相近超碰人人免费人妻，微量元素蛛網(wǎng)圖和稀土配分型式也基本一致，它們具有相似的巖漿過(guò)程和統(tǒng)一的活動(dòng)陸緣構(gòu)造背景国产每日；同時(shí)在线A级网站，從早期火山巖漿活動(dòng)到晚期淺成－超淺成巖漿侵入活動(dòng)，其w(SiO2)和w/w的值降低男人插女人b动态图，而w以及w/w一级欧美一级日韩α片、w/w和w/w的值增高，晚期淺成－超淺成侵入巖與早期火山巖沒(méi)有直接的分異演化關(guān)系亚洲综合精品一区二区。

High pressure and temperature experiment show that lamprophyric melt and orthophyric melt mix with each other under high pressure and seperate under low-pressure.

結(jié)合哀牢山斷裂帶富堿侵入巖的地質(zhì)地球化學(xué)資料亚洲音影先锋在线，論證了煌斑巖與富堿侵入巖為富集地幔不同部分熔融程度的產(chǎn)物；高溫高壓實(shí)驗(yàn)表明嫖妓视频，煌斑巖熔體和花崗斑巖熔體在高壓條件下發(fā)生混合18岁免费黄，低壓條件下出班分離，加上有關(guān)的地球化學(xué)判別h片免费网站，推測(cè)巖漿混合作用是本區(qū)煌斑巖與花崗斑巖(富堿侵入巖母巖漿同化分異結(jié)晶作用的產(chǎn)物)密切共生的主要因素久久国产老熟女俱乐部。

Xiangshan volcano-intrusive complexes is the wall rock of the biggest volcanic-rock uranium ore deposit in China, and the main body is rhyolitic porphyroclastic lava, accompanied by hypahyssal or ultra-hypabyssal intrusive rocks such as dacite-porphyry and granite-porphyry Jiulongzhang volcano-intrusive complexes are dominantly rhyolitic welded tuff, accompanied by dacite-porphyry and quartz monzonite-porphyry, and so on, and the uranium resources are being assessed.

相山火山－侵入雜巖是華南地區(qū)最大的火山巖型鈾礦賦礦圍巖h在线观看视频免费，其主體巖石為流紋質(zhì)碎斑熔巖，淺成－超淺成侵入巖有英安斑巖美国大片一级又大又粗的黑人、花崗斑巖等A区手机在线看黄色视频；九龍嶂火山－侵入雜巖的鈾資源潛力尚待評(píng)價(jià)，主體巖石為流紋質(zhì)熔結(jié)凝灰?guī)r正在播放近国产乱伦，淺成－超淺成侵入巖有英安斑巖中文字幕日本乱码精品久久、石英二長(zhǎng)斑巖等。

The results show that during the landfalling ing and northward going process of Matsa, the cold air in its northwest side first rotated along the typhoon circulation from the north to the south, and then intruded northward form the south into warm center of Matsa gradually, and at the same time in the vertical direction there were cold airs systematically/slantly descending from the middle-upper troposphere and intruding into the typhoon circumfluence at the low level, which at last resulted in the extratropical transition of Mstsa.

結(jié)果表明：&麥莎&登陸北上過(guò)程中国产在线A∨，西北側(cè)冷空氣先隨著&麥莎&環(huán)流由北向南旋轉(zhuǎn)亚洲综合色区中文字幕，爾后冷空氣又從臺(tái)風(fēng)低壓中心的偏南側(cè)向北侵入，逐步侵入&麥莎&暖心結(jié)構(gòu)婷婷精品国产精品亚洲；在垂直方向上国产精品色哟哟无码，對(duì)流層中高層不斷有系統(tǒng)性的冷空氣傾斜向下補(bǔ)充，冷空氣從對(duì)流層低層侵入臺(tái)風(fēng)環(huán)流看个毛片，最終使&麥莎&變性日韩A片网站。

The ore body occurred adjacent to the granite, thus it is inferred that mineralization stage is syngenetic or slightly later than emplacement of the granite, suggesting that mineralization of Mo, W, Pb, Zn and Ag was closely related to emplacement of the Yanshan period granites, and providing a new model for prospecting intrusive-related resource inside the volcanic rocks.

由于礦體賦存于巖體頂突部位的蝕變花崗巖中，預(yù)示成礦為花崗巖侵入的同期或稍后欧美乱伦视频，即鉬鎢鉛鋅銀成礦與燕山期花崗巖侵入活動(dòng)密切相關(guān)18岁以下禁止进入黄色网站，這對(duì)于火山巖內(nèi)尋找與侵入巖有關(guān)的礦產(chǎn)提供了新的思路。

Lithologies are mostly sand and carbonate rocks, caps are mud rock, shale and magmatite. Entrap types are anticline, fault block rebuilt by breaking and the screened entrap diapered rock mass. The composition is CO_2, N_2, CH_4, C_2H_6 and He etc. It is magma air source body and its geologic fashions are intrusion and buried volcanic conduit. The relations between gas reservoirs and gas source bodies have three types: magma intrusion-breaking-communicated gas reservoir, magma intrusion-contacted CO_2 reservoir and buried volcanic conduit-contacted gas reservoir. The CO_2 migration in magma intrusion is consisted of fusing and crystallizing phases;it in volcanic conduit is consisted of near-surface effusion and crystallizing phases.The buoyancy of CO_2 in water far more than migration resistance in breaking or chink, CO_2 is easy float upward, the floating can results in differentiation of different density gases and concentration of sealed gas. The gas in sand reservoir firstly migrate into the higher porosity and coefficient of permeability sand, and along with the pressure going up it migrate into the lower. In magma intrusion-breaking-reservoir migration, CO_2 firstly migrate into watered breaking, began gravity differentiation and concentrate, the gas pressure time and again go up, CO_2 migrate into reservoir and concentrate under expansibility as the pressure reach upward a given extend. The CO_2 in reservoir experience four breaking modes: chemistry deposition, dissolution, diffusion and mechanic breaking, the pressure balance can be broken by faulting and the CO_2 will further migrate and form new reservoir.

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Trespassing, breaking and entering：非法侵入 強(qiáng)行侵入他人住宅

I mean, do you know what happens if we get caught in here?|我的意思... | Trespassing, breaking and entering.|非法侵入 強(qiáng)行侵入他人住宅 | You heard what Bernie said. They'd split us up and ship us off.|你...

Intrusion Detection：侵入檢測(cè)

侵入反制電子學(xué) Intrusion Countermeasure Electronics,ICE | 侵入檢測(cè) intrusion detection | 抗侵入通信電纜 intrusion resistant communication cable

multiple intrusion：重復(fù)侵入;疊侵入體

重復(fù);重疊 duplication | 重復(fù)侵入;疊侵入體 multiple intrusion | 重復(fù)褶皺 superposed fold

multiple intrusion：重復(fù)侵入;迭侵入體

多堿化物類(lèi) multiple halides | 重復(fù)侵入;迭侵入體 multiple intrusion | 迭巖蓋 multiple laccolith

intrusive：侵入的

intrusion 侵入 | intrusive 侵入的 | intrusive rock 侵入巖

intrusive rock：侵入巖,侵入巖體,貫入巖

intrusive mountain 侵入山 | intrusive rock 侵入巖,侵入巖體,貫入巖 | intrusive sheet 侵入巖床

intrusive sheet：侵入巖席

intrusive mass 侵入巖體 | intrusive sheet 侵入巖席 | intrusive stock 侵入巖株

intrusive contact：侵入接觸

侵入動(dòng)力變質(zhì);動(dòng)力變質(zhì) kinetic metamorphism | 侵入接觸 intrusive contact | 侵入礫巖;侵入角礫巖 intrusive breccia

intrusive vein：侵入脈

侵入礫巖;侵入角礫巖 intrusive breccia | 侵入脈 intrusive vein | 侵入脈 irruption vein

invader species：侵入種

invader 侵入種;侵入者 | invader species 侵入種 | invasion 侵入