熔化時期 的英文怎麼說
中文拼音 [rónghuàshíqī]
熔化時期
英文
melting-down period-
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
最後，綜合本區幔源礦物和地幔巖石的特徵以及地球物理資料，得出如下結論：本區上地幔的物質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、金雲母二輝橄欖巖、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徵，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；地質歷史時期這里可能發生過地殼俯沖並產生殼幔混合作用；玄武巖漿的起源深度73km ；從幔源重砂礦物的溫壓估算結果，可以推斷出巖石圈厚度可達204 . 9km ；綜合巖石圈物質組成特徵、巖石圈熱狀態、地幔溫壓狀態、氧逸度以及幔源巖石和幔源礦物的化學成分，認為研究區具備了金剛石成礦地幔地質條件。This part convincingly demonstrated the great importance of the development of the school image in the new era, with the respects of the school image and management, the school image and school special features and brand, the school image and school culture, the school image and team spirits. it elaborated that the development of the school image is beneficial to manage the school scientifically, reasonably and systematically and run a school with the managerial way, is conducive to create and set up the school brand and run a school with own specialty and fame, is conducive to create the cultural atmosphere, refine cultural connotation and run a school culturally, is conducive to melt the team, upgrade the spirit, construct the organization in the character of learning and run a school in a way of sustained development
理論部分在了解了學校形象概念的基礎上，側重談了建設學校形象的意義，分別從學校形象與學校管理、學校形象與學校特色和品牌、學校形象與學校文化以及學校形象與團隊精神四個視角加以分析研究，有力地闡明了新時期學校形象建設的重要性，認為建設學校形象有助於科學、系統、合理地管理學校，走管理辦學的道路；有助於創建學校特色和打造學校品牌，走個性化和品牌辦學的道路；有助於營建文化氛圍、錘煉文化內涵，走文化辦學的道路；有助於熔煉團隊、提升精神、建設學習型組織，走可持續發展的道路。The quantity melted at a single operation or in one period
融化量單一操作中熔化的量，或在一定時期內熔化的量It is presented that the hydrous fluxing as well as adiaba tic decompression plays an important role in melting of morb - like mantle beneath marina trough. compared with basalts from other back arc basins, it concludes that the magma varies from morb - like to arc - like with the evolution ; during the earlier stage of evolution, there coexist the two morb - like and arc - like lavas, it may be the nature of the magma in back arc basins ( especially in the earlier stage )
綜合馬里亞納海槽和其他弧后盆地玄武巖的研究成果發現，弧后盆地特別是早期擴張的弧后盆地，其巖漿產物均具從似島弧型到似洋中脊型玄武巖的時空演化特徵；同時存在島弧型和morb型兩種熔巖，可能是弧后盆地（特別是早期擴張弧后盆地）巖漿作用的一個共同屬性。The ancient region of veracruz in east mexico is often regarded as north america s first melting pot of african, european, and native american cultures. the son jarocho, for instance, is a genre that combines spanish flamenco, pre - columbian and african music
墨西哥東部具有深厚文化淵源的區域維拉克魯斯，被認為是北美首個匯聚非洲歐洲及美洲本土人文精神的文化熔爐，其夏洛楚頌樂son jarocho綜合了西班牙的佛蘭明高，以及前哥倫布時期和非洲音樂等多種歌舞類型。分享友人