And the results for two samples from Xiakangiayu, southeast of Xiaojue give an approximate age around 2.06～2.08 Ga for another episode of anatexis in the Paleo-Proterozoic time.

小覺(jué)西南下康家峪兩塊標(biāo)本的測(cè)定結(jié)果又大又粗视频，提供了該地區(qū)阜平群巖石在2.06～2.08 Ga經(jīng)歷了古元古代時(shí)期重熔作用改造的信息www.91在线。

The acid volcanic rocks of the Early Cretaceous Shangkuli Formation belong to continental crust anatexis type ones (S-type volcanic rocks) and may have formed by compression and migration of the Indian-Australia plate toward the NNE and delamination of the lower crust caused by the lithospheric extension in eastern China.

早白堊世上庫(kù)力組酸性火山巖屬陸殼重熔型火山巖，其形成可能與印度澳大利亞板塊朝北偏東方向推擠運(yùn)移欧美激情小视频、中國(guó)東部巖石圈拉張引起的下地殼拆沉作用有關(guān)国产精品国产一级国产AV。

At the stage of geosyncline, the huge thick sal geo synclinal structural layer would be formed by volcanism and weathering deposition; the Caledonion granites would be form ed by remelting or mix-melting.

地槽階段，火山作用及風(fēng)化沉積作用等形成了巨厚的硅鋁質(zhì)地槽構(gòu)造層hhzhh.com；重熔或混熔（包括混合作用和/或同化混染作用）形成了加里東花崗巖類98超碰日本人妻。

The study of ore-forming rules indicates that the shearing force came from interaction of plate-plate is the initial force, which result in remelting of deep rock. Early formed faults and later dome structures provide favourable passage-way for ore-material migrating. Finally due to complete circulate convection, ore-material experience a process of complete differentation and begin to crystal and settle in certain circumstance. In some favourable tectonic zone ore-forming material enriched to deposit.

對(duì)成礦機(jī)制的研究顯示板塊作用產(chǎn)生的剪切力是造成區(qū)內(nèi)深部巖石重熔的源動(dòng)力国产精品三级国，而早期形成的斷裂體系及后期形成穹窿構(gòu)造為礦物質(zhì)的運(yùn)移提供了有利的通道，在完善的循環(huán)對(duì)流機(jī)制配合下julia中文国产一区，成礦物質(zhì)在遷移過(guò)程中發(fā)生較為充分的分異作用农村女人一级毛片农村妇女，各類礦物質(zhì)在相應(yīng)的物化環(huán)境中結(jié)晶沉淀，并在有利的構(gòu)造部位富集成礦久久ri国产蜜臀AV。

Both the experimental results and theoretical analyses indicate that the remelting and breakup of the primary dendrites are induced by the chemical superheating of solid during recalescence rather than by the solid-liquid interface tension.

4實(shí)驗(yàn)結(jié)果和理論分析說(shuō)明黄色禁看视频，初始枝晶組織的重熔瓦解是體系再輝過(guò)程中固相的化學(xué)過(guò)熱引起的，固液界面張力作用下的重熔對(duì)組織形態(tài)的影響相對(duì)較小91无码视。

Meanwhile, the surface layer gets fine crystal grain with dispersive and homogeneous distribution of WC grains and Co binder from rapid melting and resolidification during HIPIB irradiation. Minimizing the mean free path in Co binder by decreasing the WC grain size leads to an increase in resistance to plastic deformation in the binder.

HIPIB強(qiáng)烈非平衡作用下的重熔和再結(jié)晶使WC晶粒細(xì)化且分布更均勻色综合www在线视频，同時(shí)，表層析出彌散分布的Co_3w_9C_4相日韩毛片免费高清在线视频，使Co粘結(jié)相產(chǎn)生強(qiáng)化欧美在线一级毛钱，導(dǎo)致Co粘結(jié)相的平均自由程降低，從而增強(qiáng)了Co粘結(jié)相抵抗塑性變形的能力26uuu亚洲欧美另类，提高了輻照硬質(zhì)合金的耐磨性能。

And then a local extension took place in the region of intra-Eastern Tethys when the India plate drifted to the north but suffered the resistance from the Lhasa block, contemporarily, the intra-oceanic subduction are triggered, subsequently, magmas derived from a partial melting of mantle wedge which suffered from the modification by subducted continental marginal clastics and oceanic sediments upwelled along the oceanic ridges, forming several small marginal basins during 120～128 Ma, and thus lead to the so-called SSZ-type oceanic crust.

于120～128Ma免费看黄色视频男操女视频网站，一些規(guī)模較小的邊緣洋盆形成男女插插视频，卷入陸緣碎屑和洋殼沉積的地幔楔發(fā)生熔融產(chǎn)生巖漿，沿著破裂的擴(kuò)張脊上涌產(chǎn)生了具有TNT負(fù)異常的SSZ型新洋殼日韩精品导航视频在线播放网站，期間產(chǎn)生了俯沖洋殼重熔作用欧美性爱久j草影院，標(biāo)志著年輕的熱的洋殼俯沖形成的埃達(dá)克巖侵入于仁布SSZ蛇綠巖地幔橄欖巖中。

Otherwise, the control of remelting processing parameters of the SiCp/Al composites with a amount of Si in the master matrix, using the kinetics expressions, can be suitably achieved, whereas SiCp/pure Al composites could not.

Ti對(duì)SiC/Al界面反應(yīng)有一定的抑制作用日韩性爱免费视频，但不能有效地控制多次重熔過(guò)程中SiC/Al間的界面反應(yīng)色呦呦禁止网站，其原因在于局部熔體結(jié)構(gòu)導(dǎo)致的Ti的微觀不均勻。

A series or criteria of recognizing tin-bearing granite is set up by collecting the data on related petrology, mineralogy, geochemistry, trace elements, transitional ele ments, incompatible elements and rare earth elements.

黑云母花崗巖對(duì)成礦的貢獻(xiàn)有兩個(gè)突出的方面：其一是其在重熔生成演化過(guò)程中啊灬啊灬啊灬快灬高潮了在线观看，經(jīng)高度分異作用色哟哟伊人，將原各地質(zhì)體中的錫多金屬元素分餾富集，為成礦奠定了一個(gè)良好的基礎(chǔ)a色导航在线。

The fusible plug device is a nonreclosing pressure relief device designed to function by the yielding or melting of a plug of fusible metal.

易熔塞裝置是一個(gè)非重閉減壓裝置啪啪啪免费试看，通過(guò)易熔金屬制成的塞子的變形或熔化發(fā)揮作用。

anatexis：深熔作用

深熔作用(Anatexis)引起了地殼內(nèi)部固體物質(zhì)的重溶與熔融和進(jìn)一步的初始花崗質(zhì)巖漿的形成. 本文主要從巖相學(xué)角度對(duì)河北平山阜平巖群3種主要變質(zhì)巖類中一部分巖石在薄片中所顯示的初期深熔特征進(jìn)行了報(bào)道,提出識(shí)別深熔作用發(fā)生發(fā)展初期的一些巖相學(xué)標(biāo)志,

igneous：火成巖

I型花崗巖巖漿是由火成巖(Igneous)源巖部分熔融形成. S型花崗巖巖原地花崗巖 原地花崗巖(autochthonous granite)是由原來(lái)的變質(zhì)巖就地形成的一種混合花崗巖. 關(guān)于原地花崗巖的成因主要有兩種觀點(diǎn):一種看法認(rèn)為,原地花崗巖是由重熔作用或再生

palimpsest structure：變余構(gòu)造;變質(zhì)殘留構(gòu)造

"柱磷鍶鋰礦","Palermoite" | "變余構(gòu)造;變質(zhì)殘留構(gòu)造","palimpsest structure" | "巖漿再生作用;重熔作用","palingenesis"

remelt crucible：再熔坩堝

remedy with heavy drug (具有鎮(zhèn)靜作用的方劑)重劑 | remelt crucible 再熔坩堝 | remelt iron 再熔鐵