The mineral chemistry, trace elements and Sr-Nd isotopic geochemistry of different types of deep-seated inclusions indicate that Group Ⅰinclusions in western Shaudong could be the relicts of high degree of partial melting of the mantle-derived peridotites and then subjected to mantle metasomatism; the dunite and harzburgite in Group Ⅱ inclusions could be resulted from the metasomatism of silica-rich melts in the upper mantle; the olivine-pyroxenite and pyroxenite in Group Ⅱ and Group Ⅲ inclusions could be magmatic cumulates derived from magma underplating in the upper mantle.

不同結(jié)構(gòu)類型深源巖石包體的礦物化學(xué)日韩性色自拍视频网站在线播放、元素和同位素地球化學(xué)研究表明超碰97自慰，魯西具有變質(zhì)變形結(jié)構(gòu)特征的橄欖巖類巖石包體為巖石圈地幔橄欖巖部分熔融后的殘留體，其后又遭受了地幔交代作用的改造99re这里只有精品视频在线观看；具有變質(zhì)變形結(jié)構(gòu)麻豆精品视频在线，并疊加有礦物反應(yīng)結(jié)構(gòu)的純橄巖和方輝橄欖巖類包體為古老巖石圈地幔被富硅質(zhì)熔體改造的結(jié)果；具有殘留巖漿結(jié)晶結(jié)構(gòu)的橄欖巖人人草av在线、橄輝巖類巖石包體以及具有變晶結(jié)構(gòu)或堆晶結(jié)構(gòu)的輝石巖類包體為地幔更早期巖漿作用的在上地幔的堆積體XXXXWWW视频欧美。

Through the study of metallographic specimen and the inclusions through electrolyzation under SEM, it is indicated that the Ti-deoxidized products are globular compound inclusions with the size of 1~3μm in this experiment condition. With the technical of ion beam thinner the inner structure of these inclusions can be observed, whose core is Ti-O and outer is Mn-S. Based on EBSD the phase composition has been analyzed and it indicated that these globular compound inclusions are Ti2O3 and MnS with nucleating center Ti2O3, which can prompt to nucleate IGF.

在掃描電鏡下通過對金相試樣和電解提取的夾雜物研究表明，本實驗條件下鋼液凝固過程中析出的夾雜物是Ti-O-Mn-S形成的尺寸為1～3μm的球形復(fù)合夾雜物啊啊疼轻点视频；通過離子減薄后觀察了夾雜物的內(nèi)部結(jié)構(gòu)a视频在线，中心是Ti-O化合物，外圍是Mn-S化合物亚洲熟妇无码一区；通過電子背散射衍射對夾雜物的物相組成的分析表明了該復(fù)合夾雜物是有利于針狀鐵素體形核的Ti2O3和在凝固過程中以Ti2O3為核心形核的MnS福利小视频。

We have successfully synthesized hydrocarbonbearing inclusions in carbonate at the temperature and pressure of 150 ℃ and 40 MPa, which are near the condition of natural reservoir underground 4 kmAll synthetic hydrocarbonbearing inclusions have been analyzed by microscope and microfluorescence and fourier transform infrared spectroscopyThe results show that the synthesized hydrocarbonbearing inclusions are very similar to those in real reservoirsOur experiments give us four important insights, including:(1) immiscibility of oil and water is the main reason for hydrocarbonbearing inclusions and aqueous inclusions distributed in different fractures;(2) rapid accumulation of oil and gas can be recorded by fluid inclusions;(3) the study of synthetic hydrocarbonbearing inclusions at the temperature and pressure of real reservoir will offer references and standards for the analysis of fluid inclusions in reservoirs;(4) experiment of synthetic hydrocarbonbearing inclusions is a good method for understanding the mechanism of oilwaterrocks interreaction in reservoirs.

文中報道在實際儲層溫壓條件下(150 ℃日韩少妇无码系列视频，40 MPa，大約4 km深度)成功合成了碳酸鹽巖烴類包裹體国产老肥熟XXxX。通過對合成烴類包裹體的顯微觀察免费的一级大黄A片、熒光分析和傅里葉變換紅外光譜分析，證實合成了烴類包裹體国产高清视频在线免费观看，且與真實儲層中的包裹體具有相似特征黄色小视频网站网址免费观看，探討了油水不混溶條件下的流體包裹體捕獲機(jī)制。實驗研究給出4點重要啟示：(1)油水不混溶是造成烴類包裹體和水溶液包裹體分帶的主要原因亚洲欧美日韩中文另类；(2)油氣快速成藏過程可以被流體包裹體記錄色综合加勒比一本无码综合；(3)實際儲層溫壓條件下，合成烴類包裹體實驗研究有望為儲層包裹體分析提供依據(jù)和標(biāo)準(zhǔn)黄视频app；(4)人工合成烴類包裹體為研究含油氣條件下儲層水巖作用機(jī)理提供了一種有效手段日本一区二区三区喷水高潮。

Study using infrared microtechnique reveals three types of fluid inclusions in rutile:Ⅰ-type aqueous inclusions,Ⅱ-type CO_2-H_2O inclusions and Ⅲ-type CH_4 inclusions. Primary and pseudosecondary type Ⅰ inclusions, as well as Ⅱ-type fluid inclusions, having a range of pressure between 0.6 and 1.3 GPa, were trapped during the amphibolite-facies retrogression stageof eclogites, suggesting that fluids related to rutile mineralization originated from water released during retrograded metamorphism of eclogites.

利用紅外顯微鏡對金紅石進(jìn)行的流體包裹體研究表明，金紅石中主要存在三類流體包裹體人操人人摸人人干，即Ⅰ型H2O溶液包裹體、Ⅱ型CO2-H2O包裹體和Ⅲ型CH4包裹體激情毛片3，其中I型原生和假次生流體包裹體和Ⅱ型流體包裹體反映出的壓力范圍為0.6～1.3 GPa免费AV网站网址不卡，與榴輝巖角閃巖相退變質(zhì)作用的壓力相當(dāng)，說明與這類金紅石形成有關(guān)的變質(zhì)流體源于榴輝巖退變質(zhì)作用所釋放的水www.swag。

The influence of nonmetal inclusions on quality and performance of steels is not only dependent on total quantity of inclusions, but also on the type, shape, size, deforming behavior and distribution of the inclusions in steel.

鋼中的非金屬夾雜物對鋼質(zhì)量和性能的影響免费高清视频黄色视频频，不僅取決于夾雜物數(shù)量的多少，而且與夾雜物的類型大学生高潮一级毛片免费、形狀岛国、COM、大小、變形行為和分布情況有著密切的關(guān)系欧美xingai在线播放。

The inclusions are changed from chain shape with acute angle to spherical shape. Those are complex inclusions with the Zr containing inclusions are the nuclei for the inclusions, Al2O3 and / or MnS are located in the surface layer of the inclusions whose size is in the range of 1.0 to 3.0μm.

經(jīng)過鋯處理后在线看无码黄片，粗晶熱影響區(qū)中的夾雜物由長條的尖角狀變?yōu)閳A形或近圓形，且都是含鋯的復(fù)合夾雜物欧美黄片污，含鋯夾雜物作為形核核心亚洲无码色色，在其表層沉淀析出Al2O3和／或MnS，其尺寸在1.0~3.0μm之間亚洲精品首页。

The fluid inclusions of Shalagang antimony are composed of gas and liquidfacies. The composition of gas facies is CO2 and vapor, and the liquid facies is brinesolution. The homogeneous temperature of inclusions is between 135℃～290℃,according to the forming temperature of stibnite. And the salinity of inclusions is0.53～12.58wt%NaCl.

沙拉崗銻礦床流體包裹體以氣液兩相為主国产精品又黄又粗又大，氣相成分為CO2和水蒸氣，液相成分為鹽水溶液色呦呦在线二区；包裹體均一溫度在135℃～290℃之間国产玖玖精品视频，與輝銻礦形成溫度相吻合；包裹體鹽度變化為0.53～12.58wt%NaCl日韩激情无码一级毛片变态，總體屬低溫低鹽度包裹體嗯啊一区视频在线观看。

The simulation showed that without EMBr, the floating-up probability was nearly zero for the inclusions less than 50μm, and 6% for the inclusions larger than 200μm. With EMBr, the floating-up probability was 25% for the inclusions less than 50μm, and 38% for the inclusions larger than 200μm.

數(shù)值模擬表明2021最新三级在线观看，無電磁制動時，粒徑在50μm以下的夾雜物顆粒其上浮概率幾乎為零a片黄色视频a片，200μm夾雜物顆粒上浮概率為6%日韩a级毛片AV一区免费在线观看；有電磁制動時，粒徑在50μm以下的夾雜物顆粒的上浮概率為25%欧美性爱一二三区， 200μm夾雜物顆粒上浮概率為38%十大免费黄的色网站。

GroupⅠ, the peridotite inclusions with typical pyrolite textures (metamorphic and deformation textures);(2) GroupⅡ, the peridotite and olivine-pyroxenite inclusions with metamorphic and deformation textures and overlaid mineral reaction textures or relic magmatic crystalline textures or/and cumulate textures; and (3) GroupⅢ, the pyroxenite inclusions with crystalloblastic texture and cumulate textures.

深源巖石包體的巖相學(xué)表明，魯西深源巖石包體具有三種結(jié)構(gòu)類型：①具有典型地幔巖結(jié)構(gòu)的橄欖巖類巖石包體久热这里只精品99国产6；②具有變質(zhì)變形結(jié)構(gòu)无遮挡一级A片高清视频在线观看，并疊加有礦物反應(yīng)結(jié)構(gòu)以及殘留有巖漿結(jié)晶結(jié)構(gòu)的橄欖巖、橄輝巖類巖石包體十大免费黄色网站入口；③具有變晶結(jié)構(gòu)或堆晶結(jié)構(gòu)的輝石巖類包體国产人成。

The rutile inclusions have protogenetic and syngenetic stages. The protogenetic rutile inclusions are of fragmentation. The syngenetic rutile inclusions are mainly short column, and some are long column.

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