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- 更多網(wǎng)絡(luò)例句與成因的相關(guān)的網(wǎng)絡(luò)例句 [注:此內(nèi)容來源于網(wǎng)絡(luò)99pom国产熟女,僅供參考]
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Four main formations of loop bedding in Jiyang sub-basin were upper layers fall down in the process of earthquake, tautening distortion due to earthquake, the frication of earthquake-related surface of fault and the effect of redox and diffuse other formations of loop bedding comprise the effect of earthquake wave, the effect coming from circumrotate of globosity rotation, snowball function, cementation intermittent, the effect of biology, and so on.
綜合分析認為震動塌落、震動拉伸變形黄色网站日韩观看免费、地震斷裂面的摩擦作用肏丝袜屄影片、氧化還原反應(yīng)和擴散作用是環(huán)狀層理的主要成因,前三種成因的環(huán)狀層理往往與其他震成構(gòu)造伴生日韩ww频在线免费观看,可作為震積巖的良好標志二级免费黄片国产。環(huán)狀層理的其他成因還包括:地震波傳播方式的影響、地球自轉(zhuǎn)產(chǎn)生的渦旋的影響国产精品特黄特级AAAAAA片、"滾雪球"效應(yīng)一级A片岛國、間歇膠結(jié)作用以及生物成因等。
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By use of the Fischer-Tropsch reaction in a C-H-O system, we discussed the relationships between inorganic CO〓 and some physical chemistry conditions, such as Oxygen flee degree , temperature, pressure, other objects consistency and catalyzer. a when T=200K~2000K, if f〓>0, the reaction of generating CO〓 will be dominant, CH〓 hardily exists; b when T>1000K, CH〓 is not propitious to exist, carbon in system almost exists in form of CO〓; c the more pressure, the more CO〓 is propitious to exist; d the more consistency of CO, O〓 and H〓O, the more CO〓 is propitious to exist, the more consistency of H〓, the more CH〓 is propitious to exist.
依據(jù)C-H-O體系費托反應(yīng)的簡化模型,討論了氧逸度97人操人、溫度嗯好深啊用力哦啊视频、壓強、其它物質(zhì)濃度A片、Com、催化劑等物理化學條件對無機成因CO〓生成的影響手机在线免费看黄色片网站,從理論上討論了在地質(zhì)環(huán)境中,無機成因CO〓存在的物理化學條件:1在T=200K~2000K的溫度范圍內(nèi)九一国产视频精选,體系中一旦氧逸度>0亚洲视频无线观看,生成CO〓的反應(yīng)將占絕對優(yōu)勢,CH〓幾乎不可能存在色综合久久91;2T>1000K時欧美性大战久久久久久久,不利于CH〓形成,使體系中的碳主要以CO〓的形式存在亚洲免费一级免费看片;3體系壓強越大中文字幕视一区二区人妻,越有利于CO〓的形成;4反應(yīng)物CO国产精品色午夜快乐、O〓一级婬片又大又长又粗、H〓O的濃度越高,越有利與CO〓的存在欧美熟妇free性XXXX,H〓的濃度高有利于CH〓的形成。5地質(zhì)成藏作用可以經(jīng)歷很長的地質(zhì)年代国产精品资源网在线观看,這足以補償?shù)V物巖石中的Ni澳美午夜福利、Mo、Fe人人爽人人看人人硬、Co国产91视频有限公司、Ru等催化性能的降低及其它動力學條件的不足,使得費托反應(yīng)可能發(fā)生在线等免费看黄片,從而生成無機成因的CO〓和烴類www。.你懂得。
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The branch of petrology that deals with the origin of rocks, especially igneous rocks.
巖石成因說,巖石發(fā)展學研究巖石成因的巖石學的一個分支美国少妇a级,尤其是火成巖的成因
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The study on formation cause of plagioclase is closely related to formation cause of geological structure.
對斜巖成因的研究與人們對大地構(gòu)造成因的認識密切相關(guān)免费激情在线视频国产。
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The study on formation cause of plagioclase is closely related to people's knowledge on the formation cause of structure of the earth.
對斜巖成因的研究與人們對大地構(gòu)造成因密切相關(guān)。
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TOF-SIMS images show bacteriogenic pyrites are relatively rich in Cu, Zn, and Ni, suggesting that bacteria probably play an important role in the enrichment of Cu, Zn, and Ni during their formation.
TOF-SIMS 的離子像亦表明菌落成因的黃鐵礦富集 Cu 国产免费一级特黄真人视频大全、 Zn 和 Ni 亚洲国产精品日本一区二区,表明菌落在生物成因黃鐵礦的形成過程中,在改變介質(zhì)條件igao、在遷移95视频手机在线观看、活化和富集 Cu 、 Zn 等金屬元素方面做出了貢獻正在播放国产一级特黄。
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The alabandite and getchellite of hydrothermal origin, cement anatase of alkaline volcanic origin, and the high content of chlorite in coal were fist found in coals.
在西南地區(qū)晚二疊世煤中首次發(fā)現(xiàn)了熱液成因的硫錳礦和硫砷銻礦黄视频免费、堿性火山灰成因的膠態(tài)銳鈦礦和陸源碎屑成因的斜綠泥石大屌干屄视频。
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The aim of this study is to discriminate between the geogenic natural content and the anthropogenic contribution in the collected sediments.
此項研究的目的是區(qū)分在已采集的沉積物中地質(zhì)成因的自然含量和人為成因貢獻值。
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Four main formations of loop bedding in Jiyang sub-basin were upper layers fall down in the process of earthquake, tautening distortion due to earthquake, the frication of earthquake-related surface of fault and the effect of redox and diffuse other formations of loop bedding comprise the effect of earthquake wave, the effect coming from circumrotate of globosity rotation, snowball function, cementation intermittent, the effect of biology, and so on.
綜合分析認為震動塌落91精品国产兔费观看久久、震動拉伸變形青草草视频网、地震斷裂面的摩擦作用、氧化還原反應(yīng)和擴散作用是環(huán)狀層理的主要成因99er在线视频,前三種成因的環(huán)狀層理往往與其他震成構(gòu)造伴生色哟哟亚洲,可作為震積巖的良好標志。環(huán)狀層理的其他成因還包括:地震波傳播方式的影響欧美一级A片直播、地球自轉(zhuǎn)產(chǎn)生的渦旋的影響人人看黄视频、&滾雪球&效應(yīng)、間歇膠結(jié)作用以及生物成因等啪啪啪免费无码视频。
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The studies on the compositions, origins and elastic properties of the southern Tibetan lower crust include the following 4 aspects: the petrological and geochemical festures and ages of granulitic facie rocks located in Higher Himalayas; dehydration melting experiments on the biotite-plagioclase gniess collected from Higher Himalayas at high temperature and high pressure to model the formation of the granulites; measurements of wave velocities of the lower crustal rock in situ; analysis of origin of intracrust low wave velocity layers beneath southern Tibet.
以西藏南部下地殼物質(zhì)組成综合久久2019,成因及其彈性性質(zhì)為研究目標進行了4個方面的相關(guān)研究:高喜馬拉雅地區(qū)麻粒巖相巖石的巖石學,地球化學和年代學研究wwjizz国产;麻粒巖相巖石成因的高溫高壓實驗欧美激情久久;原位條件下巖石的彈性波速測量;西藏高原殼內(nèi)低速層的成因分析與模擬国产熟睡乱子乱A片。
- 更多網(wǎng)絡(luò)解釋與成因的相關(guān)的網(wǎng)絡(luò)解釋 [注:此內(nèi)容來源于網(wǎng)絡(luò)国产AV无码AV一区,僅供參考]
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morphogenetic:地貌成因的
morphogenesis 地貌成因 | morphogenetic 地貌成因的 | morphogenic phase 地貌發(fā)生幕
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morphogenetic:形態(tài)發(fā)生的 形態(tài)形成的 地貌成因的 地貌發(fā)生的
morphogenesis 地貌成因 地貌發(fā)生 形態(tài)發(fā)生 | morphogenetic 形態(tài)發(fā)生的 形態(tài)形成的 地貌成因的 地貌發(fā)生的 | morphogeneticforce 地貌發(fā)生力
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polygene:多時代的 多源的 多成因的 復(fù)成的
polygen 多價的 | polygene 多時代的 多源的 多成因的 復(fù)成的 | polygenes 多基因
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abiogenetic:非生物成因的;自然發(fā)生的
abiogenetic gas 無機成因氣 | abiogenetic 非生物成因的;自然發(fā)生的 | abiogenic gas 無機成因氣
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abiogenetic:非生物成因的;自
abiogenesis 非生物成因;自然發(fā)生 | abiogenetic gas 無機成因氣 | abiogenetic 非生物成因的;自
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aquiferous:含水的;水成成因的
aquifer 含水層 | aquiferous 含水的;水成成因的 | aquifuge 隔水層
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monogenetic:單成,單成因的,單色的,單性
monogenerock 單成巖 | monogenetic 單成 單成因的 單色的 單性 | monogeneticdye 單色染料
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polygenetic:多色的 多時代的 多源的 多成因的 復(fù)成的
polygenes 多基因 | polygenetic 多色的 多時代的 多源的 多成因的 復(fù)成的 | polygenevolcano 復(fù)成火山
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thermogenic:生熱的,熱成因的
生熱作用 thermogenesis | 生熱的,熱成因的 thermogenic | 熱成因氣 thermogenic gas
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biogenic:生物成因的
biogenic theory 油氣生物成因?qū)W說 | biogenic 生物成因的 | biogenochemical anomaly 生物地球化學異常