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partial melting中文是什么意思

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  • 例句與用法
  • Paleoproterozoic ; wangjiahui granitoids ; partial melting ; recycling of islands arc and continent crustal materials ; tectonic transition ; wutai mountains
    古元古代王家會花崗巖部分熔融島弧和陸殼物質(zhì)再循環(huán)構(gòu)造轉(zhuǎn)換五臺山
  • Quantitative calculation of trace element content for the residue after partial melting suggests that intermediate - mafic granulites outcropped in the dabie orogen are not the residue of partial melting
    殘留相微量元素定量計算結(jié)果表明,大別山現(xiàn)今出露的中基性麻粒巖不是部分熔融后形成的殘留體。
  • By studying , the main conclusions have been achieved as follows : i . the volcanic rocks , as the result of the partial melting of enriched mantle , comprise calc - alkaline andesite and dacite and a few tholeiite
    通過研究,得出以下主要認識: 1 、火山巖為一套以鈣堿性安山巖為主,含少量拉斑玄武巖和英安巖。
  • Although there was a partial melting of the reactor core at tmi - 2 , the radiological release was mainly confined within the containment building and the release to the environment is minimal and insignificant
    雖然三哩島反應(yīng)堆部分堆芯已經(jīng)熔化,但輻射泄漏的范圍主要局限于安全殼廠房內(nèi),對環(huán)境的影響極其輕微。
  • Although there was a partial melting of the reactor core at tmi - 2 , the radiological release was mainly confined within the containment building and the release to the environment is minimal and insignificant
    雖然三哩島反應(yīng)堆部分堆芯已經(jīng)熔化,但輻射泄漏的范圍主要局限于安全殼廠房內(nèi),對環(huán)境的影響極其輕微。
  • Partial melting of the enriched lithospheric mantle owing to a raised geotherm caused by lithosphere thinning and following the afc process resulted in the formation of the quannan and tabei syenites in southern jiangxi
    隨著拉張作用加強,受軟流圈物質(zhì)交代過的巖石圈地幔的小比例部分熔融形成的高鉀堿性巖漿經(jīng)afc作用形成堿性雜巖(全南和塔背巖體) 。
  • The residue formed by partial melting of thickened crust due to anomalous heat supply by mantle superwelling at early cretaceous is possibly easy to detach from the crust because of its high density , leading to the remove of mountain root and large scale uplift of the orogen
    早白堊世地幔超柱事件熱擾動所引起的加厚地殼部分熔融后的殘留體可能由于比重較大而拆離進入地幔,從而發(fā)生去山根作用和造山帶的大面積隆起。
  • The mineral chemistry amd elemental variations in whole rocks can be ascribed to results of partial melting of various degrees . according to the fractional melting model , the partial melting degree for the iherzolites is less than 5 percent , and about 7 to 20 percent for harzburgites
    全巖及礦物的主量元素的成分變化主要受部分熔融程度的控制,分異熔融模型獲得的二輝橄欖巖的部分熔融程度5 ,方輝橄欖巖部分熔融程度在7 - 20之間。
  • Secondly , based on the microbeam analytical technique , on the one hand , through investigating the characteristic of major elements in the mantle minerals the author acquired the static information from mantle ; on the other hand , through multi - point analysis of a part of the minerals from mantle , the auther got dynamic information from mantle . finally , generalizating the fruits of this study and predecessors , the autor holds that the constituents of lithospheric mantle possibly includes spinel lherzolites , clinopyroxenites , websterite , dunite , harzburgites , garnet lherzite , phlogopite lherzite , eclogites , clinopyroxene megacrysts ; compared with east china and north china platform , the research field mantle shows the characteristics of higher degree of partial melting processes and more depleted mantle ; the . upper mantle beneath north hetian area is heterogeneous , with a tendency of deficit in a12o3 and lree from kaliyang in west hetian to the river basin of kalakshi river and yulongkashi river ; the subduction of the crust beneath north hetian has ever occurred in geological history and caused the mixing of mantle - crust ; the depth of the origination of basaltic magmas beneath north hetian exceeds 73km ; the thickness of the lithosphere beneath the research area amounts to 204 . 9km ; the mantle beneath north hetian has geological condtions for forming diamond deposits
    最后,綜合本區(qū)幔源礦物和地幔巖石的特征以及地球物理資料,得出如下結(jié)論:本區(qū)上地幔的物質(zhì)組成有尖晶石二輝橄欖巖、二輝巖、單斜輝石巖、純橄欖巖、方輝橄欖巖、石榴石二輝橄欖巖、金云母二輝橄欖巖、榴輝巖;與中國東部以及華北地臺上地幔相比,研究區(qū)上地幔具有富集主元素中相容元素和虧損其中的不相容元素的特征,局部熔融程度較高;上地幔存在橫向和縱向的不均一性,從西部的克里陽到喀拉喀什河和玉龍喀什河流域, al和lree富集程度呈下降趨勢,不同來源的相同礦物中主元素的含量差異較大;地質(zhì)歷史時期這里可能發(fā)生過地殼俯沖并產(chǎn)生殼幔混合作用;玄武巖漿的起源深度73km ;從幔源重砂礦物的溫壓估算結(jié)果,可以推斷出巖石圈厚度可達204 . 9km ;綜合巖石圈物質(zhì)組成特征、巖石圈熱狀態(tài)、地幔溫壓狀態(tài)、氧逸度以及幔源巖石和幔源礦物的化學成分,認為研究區(qū)具備了金剛石成礦地幔地質(zhì)條件。
  • The mafic dikes also formed by the partial melting of enriched mantle , include gabbro , diabase ( distributing mainly in luxi ) and lamprophyres ( camptovogesite , odinite and hornblende lamprophyres ) ( mainly in ludong ) . for all the rocks , crustal contamination was absent when magma emplaced . 2
    基性脈巖主要包括輝長巖、輝綠巖(主要分布在魯西地區(qū))和煌斑巖(以斜閃煌斑巖為主,同時含部分拉輝煌斑巖和角閃煌斑巖) (主要分布在魯東地區(qū)) ,都為富集巖石圈地幔部分熔融的產(chǎn)物。
  • 更多例句:  1  2  3
  • 百科解釋
Partial melting occurs when only a portion of a solid is melted. For mixed substances, such as a rock containing several different minerals or a mineral that displays solid solution, this melt can be different from the bulk composition of the solid.
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