Keywords: wagnerite new polytype; prismatine; volatile; sillimanite; Larsemann Hills

中文關(guān)鍵詞：氟磷鎂石新多型少妇爽到呻吟的视频；柱晶石看一级在线视频；揮發(fā)分；夕線石；南極拉斯曼丘陵

The deep origin of Kangjinla podiform chromitite is suggested by: that for the Kangjinla chromitite and the mantle peridotite rocks, the compositions of the chrome spinel, olivine and clinopyroxene are rather different, which indicates that the chrome spinel in the chromitite is neither the simple concentration of that in the host rocks nor with certain genic relation with mantle peridotite. Though the chromitite might be exotic for host rocks, both of them were carried from deep mantle to the shallow place by mantle plum.

康金拉鉻鐵礦石與礦體圍巖地幔橄欖巖的鉻尖晶石人人操人人爽黄色片、橄欖石和單斜輝石等成分方面明顯不同91天堂精品一区二区在线看，認(rèn)為礦石鉻尖晶石并非是由副礦物鉻尖晶石富集而成，與地幔橄欖巖也不存在成因聯(lián)系国产一级A片不卡在线观看视频，認(rèn)為豆莢狀鉻鐵礦床對(duì)于近礦圍巖地幔橄欖巖而言為外來體日韩中文字幕无码一级毛片，但兩者可能均是由地幔深部被地幔柱帶到上部。

The complete borosilicate assemblage grandidierite-prismatine-tourmaline is determined and their formation setting are investigated. A review on the nomination confusion of kornerupine minerals has been made and a new name, boro-prismatine, is recommended for the case occurrence of the mineral at Antarctica according to the composition and structure data.

確定了完整的硅硼鎂鋁礦-硼柱晶石-電氣石硼硅酸鹽礦物組合（Gdd-Prs-Trn）欧美a片黄片大片，探討了其產(chǎn)出環(huán)境精品黄色网站在线入口；對(duì)柱晶石類礦物在國(guó)內(nèi)、外命名的混亂現(xiàn)象進(jìn)行了介紹美女被操逼网站，結(jié)合礦物成分和結(jié)構(gòu)特征国产黄片视频免费看，南極產(chǎn)出的該類礦物建議稱硼柱晶石。

The results show that formation of FeO*Cr2O3 induces wetting in reaction between the liquid ceramics and outer stainless steel pipe. The ceramics structure can be divided into three zones, i.e. pin microlite, columnar and dendritic zone.

試驗(yàn)結(jié)果表明：外層鋼管與內(nèi)襯陶瓷間因形成FeO*Cr2O3尖晶石相而產(chǎn)生反應(yīng)潤(rùn)濕99国产性爱，陶瓷層由隱針狀內(nèi)層6080午夜影院三级片、柱狀中間層和外層樹枝晶組成。

For example, alkaline elements can affect diffusion velocity of Zr, Si and O ions although these alkaline elements cannot exist in crystal structure of zircon. However, K rich media and Na rich media exert different effects on the growth of crystal form: in the K rich media, growth speed of prism faces in the vertical direction is much higher than that of pyramid faces, and {111} growth speed in the vertical direction is higher than {311},which decides the formation of bipyramids dominated by {311} pyramids; in the Na rich media, both prism and pyramid grow to a certain extent, but the former is smaller than the latter.{100} growth speed in the vertical direction is lower than {110}, while {111} growth velocity in the vertical diredtion is lower than that of {311},resulting in the growth of the crystal form characterized by {100} short prism and {111} pyramid.

例如黄黄黄片AAAAA，盡管堿性元素并不進(jìn)入鋯石晶格日本黄a网站，但它們可以影響Zr、Si网站黄色视频免费、O離子的擴(kuò)散速度经典人人操人人干人人看，但是富鉀和富鈉的介質(zhì)對(duì)鋯石晶形發(fā)育的影響是有差別的黄色片一区，表現(xiàn)為：在富鉀的介質(zhì)中色哟哟毛片网站，將導(dǎo)致柱面的法向生長(zhǎng)速度較錐面快得多，而錐面中给个免费的黄色网站，｛111｝的法向生長(zhǎng)又較｛311｝快伊人黄片啪啪啪，由此決定了形成以｛311｝錐為主的雙錐狀晶體；在富鈉的介質(zhì)中美女黄色乱轮视频，柱面和錐面都有一定程度的發(fā)育xxxx性16xx，但前者弱于后者，而柱面中欧美三级视频观看，｛100｝的法向生長(zhǎng)較｛110｝慢真实处破女www，由此決定了形成以｛100｝柱和｛111｝錐為主的短柱錐狀晶體。

axinite：方柱石 斧石

方解石 方柱石 Scapolite | 方柱石 斧石 Axinite | 斧石 柱晶石 Kounerupine

flagstone：薄層砂巖;板層砂巖

柱晶松脂石 flagstaffite | 薄層砂巖;板層砂巖 flagstone | 石片 flake

spar deck：輕甲板

spar buoy 柱形浮標(biāo) | spar deck 輕甲板 | spar 晶石

Terpin Hydrate：柱晶松脂石

柱晶松脂石 flagstaffite | 柱晶松脂石 terpin hydrate | 柱磷鋁石 metavariscite

cassiterite：柱晶石 錫石

斧石 柱晶石 Kounerupine | 柱晶石 錫石 Cassiterite | 錫石 黝簾石 坦桑石 Zoisite

kornerupine：柱晶石

koreite 壽山石 | kornerupine 柱晶石 | kornerupite 柱晶石

kornerupine; kornerupite：鈉柱晶石

等軸鉭鈣石 koppite | 鈉柱晶石 kornerupine; kornerupite | 鎂水鉛石 korteite

mordenite：絲光沸石

最近,經(jīng)X射線衍射法研究,表明柱沸石的鋁矽酸鹽格架的三維空間結(jié)構(gòu)具有與絲光沸石(mordenite)相同的特點(diǎn),絲光沸石形成各向等長(zhǎng)的晶體. 柱沸石單位晶胞 ...