麻粒巖的 的英文怎麼說
中文拼音 [málìyánde]
麻粒巖的
英文
granulitic-
Lots of information suggest that the metamorphism process of this area are from granulite facies to amphibolite facies and the retrograded metamorphic path is basically a cw nearly isothermal decompressional evolvement trend
各種信息表明本區的變質作用是由麻粒巖相退變到角閃巖相。退變質軌跡基本上是一個順時針近等溫減壓型演化趨勢。Based on the studies of petrotexture, structural deformation and the relevant metamorphism, this paper indicates that this peridotite massif is the product of ultramafic magma cumulated at the crust - mantle transtion zone and has undergone the early stage of plastic deformation under the condition of granulite facies （ 800 ） and late ductile shearing at amphibolite and greenschist facies in relevance to uplifting
本文通過巖體的結構、構造變形及相應的變質作用研究，提出了該橄欖巖體是由超基性巖漿在殼幔過渡帶結晶而成，並經歷了與圍巖一致的麻粒巖相（ 800 ）條件下的早期塑性變形以及角閃巖相和綠片巖相退化變質條件下與逆沖上升有關的韌性剪切變形。High - pressure granulite and the coexisting eclogite and coesite - bearing ultrahigh - pressure eclogite have been subsequently found in the western syntaxis since 80s " last century
自20世紀80年代以來，西構造結已經發現了高壓麻粒巖，與高壓麻粒巖共生的榴輝巖和含柯石英的超高壓榴輝巖。Since eclogite and the coexisting high - pressure granulite have been found in western syntaxis, we ' ll ask whether it is possible that eclogite also can occur in eastern syntaxis
西構造結已經發現榴輝巖和與之共生的高壓麻粒巖，東構造結是否也可能存在榴輝巖呢Lithogeochemistry and lithogenetic epoch for shaba granulite in mianning, sichuan
四川冕寧沙壩麻粒巖的巖石地球化學性質及形成時代Granulite - facies retrograde metamorphism of garnet pyroxenite in muzidian, northern dabie mountains
北大別木子店石榴輝石巖的麻粒巖相退變質作用The high pressured granulite belts in the xuanhua area of hebei province are very worthy of being studied
河北省宣化地區的高壓麻粒巖帶是非常具有研究意義的。Siziwangqi of inner mongolia is located on the north margin of north china craton, the junction of north china craton and siberia. granulite xenoliths are found there in cretaceous basalt. these xenoliths are mainly plagioclase - pyroxenite
內蒙古四子王旗地區地處華北板塊北緣，與西伯利亞板塊的接合部，其早白堊世橄欖玄武巖中發現大量下地殼麻粒巖捕虜體，並可見輝石長石捕虜晶。The lithology of c petrofabric is marble, accidental gneiss. by field attitude, rock association character, petrography and petrochemistry, we know that the protolith of a petrofabric is mainly composed of pelite, sandstone and basic to acidic volcanic, that of b petrofabric mainly a suite of pelite, sandstone ( maybe include volcanic ), and that of c petrofabric mainly limestone, impurity limestone, a few of pelite and pyroclastic rock
A巖組的巖性主要是各種角閃巖類和片麻巖類夾有片巖，偶有變粒巖、大理巖。 b巖組的巖性主要是各種片巖夾有大理巖、石英巖。 c巖組主要是一套大理巖，偶有片麻巖。Granulites are the important component of the crust and there are high - pressured granulites generated in many areas of phanerozoic erogenic belts on the earth
麻粒巖是地殼的重要組成部分。全球許多顯生宙造山帶基地有高壓麻粒巖的產出。Different rock mass on the remote sensing images were obtained, based on a comprehensive remote - structure analysis, a new acknowledge on the characteristics of regional structure in tonghuashan - yushugou area was acquired. it was suggested that tonghuashan - yushugou area underwent multi - phase structure movement, multi - phase, multi - orientation > multi - level deformed structure superimposed each other accompanied with complex deformation
通過遙感?構造的綜合解析，總結出從遙感圖像上辨識高壓麻粒地體、韌性剪切帶、疊加褶皺及不同應變帶、不同類型面理和不同巖體的圖像處理方法，並獲得榆樹溝?銅花山地區區域地質特徵的重新認識。Studies on the metamorphism and ptt path of the granulites now become to be one of the most important methods to module a structural evolvement pattern of erogenic belts
研究高壓麻粒巖的變質作用和ptt軌跡已成為建立造山帶演化構造模式的最重要途徑之一。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果表明，大別山現今出露的中基性麻粒巖不是部分熔融后形成的殘留體。Studies on the metamorphic history of the granulites on a very old platform provide us some important information of the properties, status and forming processes of the lower crust and forming mechanism of the early continent crust
古老地臺麻粒巖的變質歷史研究可以為我們深入了解下地殼性質，狀態及形成過程，探討早期大陸地殼的形成機制提供重要的信息。分享友人