火成巖系 的英文怎麼說

中文拼音 [huǒchéngyán]
火成巖系 英文
igneous rock series
  • : fire
  • : Ⅰ動詞1 (完成; 成功) accomplish; succeed 2 (成為; 變為) become; turn into 3 (成全) help comp...
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  • : 系動詞(打結; 扣) tie; fasten; do up; button up
  1. Calc - alkalic series

    鈣鹼火成巖系
  2. The study shows that cretaceous volcanics mainly consist of medium acidic volcanic lava and volcanoclastic rocks, with locally developed basic lava ; medium acidic volcanics mainly consists of calc - alkalic series, was formed in compressive orogenic environment, and has good reservoir property, while cretaceous basis lava mainly consists of alkalic series, was formed in rift environment, and has poor reservoir property

    結果認為,白堊紀以中酸性山熔山碎屑為主,局部發育基性熔;中酸性以鈣堿性列為主,形於擠壓造山環境,儲集性能較好,而白堊紀基性熔以堿性列為主,形於裂谷環境,儲集性能較差。
  3. On the basis of the study on the petrology, trace element, and isotopic geochemistry, the primary magma of volcanic rocks can be divided into two series according to their originated rocks and degree of partial melting. one is the basanite - alkaline basalt - olivine tholeiite magma series, which are generated by partial melting from spinel iherzolite ; the other is nephelinite magma - alkaline picritic basalt magma, which are generated by partial melting of the garnet iherzolite

    石化學、微量元素、同位素地球化學證據都表明,華北、華南地區的根據源和局部熔融程度的不同,可以分為兩個原生漿列:一個是源為尖晶石二輝橄欖,隨著局部熔融程度的增加,形的碧玄漿-堿性玄武漿-橄欖拉斑玄武漿;另一個是源為石榴石二輝橄欖,隨著局部熔融程度的增加形的霞石漿-堿性苦橄玄武列。
  4. Distant effect of jurassic collisions of qiangtang terrane, lasa terrane and paleo - pacific land onto the eurasian land made east qinling - dabie mountains in a compressional circumstance for a long time, and suppressed its orogenic extension ; whereas, cretaceous late - collisional extension and appearance of west pacific trench - arc - basin system relieved east qinling - dabie mountains of external compression, instantly result in violent orogenic lithosphere delamination - extension and depressurized - calefactive melting, and consequently, led to the formation of large scale early cretaceous granitoids and intermediate - acidic volcanic rocks

    羌塘地體拉薩地體和西太平洋古陸在侏羅紀與歐亞大陸拼貼碰撞的遠距離效應使東秦嶺大別造山帶長期處于擠壓環境,伸展作用被抑制白堊紀的碰撞晚期伸展和西太平洋溝弧盆體的遠距離效應使東秦嶺大別地區的外部擠壓消失,導致造山帶石圈迅速強烈拆沉伸展和減壓增溫熔融,從而形大規模早白堊世花崗類和中酸性
  5. The intrusion sequence for igneous rocks is indicated by crosscutting and inclusion relationships.

    的歸入順序由切割和包含關來表示。
  6. The most common intrusive in the order of igneous rocks is granite.

    火成巖系列中最常見的侵入體是花崗
  7. Xiongcun copper - gold ore deposit is located in gangdese metallogenetic belt with a large scale. the ore body mainly exists in the second lithoid unit ' s tuffs and the third lithoid unit ' s dacite tufa of the cretaceous volcanic stratum, which are not only mother rock but also mineralized body

    雄村銅金礦床處于岡底斯礦帶,礦床規模巨大,礦體主要賦存於白堊地層第二性單元的黃鐵絹英化硅化凝灰和第三性單元英安質疑灰中,上述石既是賦礦圍又是礦化體。
  8. The upper cretaceous jingzhushan formation in the biru basin, xizang consists of a succession of coarse - grained elastic rocks in the alluvial fan - fan delta depositional system, intercalated with intermediate - acidic volcanic rocks including dacite, andesite, quartz trachyandesite and rhyolite

    摘要上白堊統競柱山組為一套沖積扇扇三角洲沉積體的粗碎屑,間夾由英安、安山、石英粗安和流紋的中酸性
  9. The reservoirs in permian is consist of carbonate rock, tuff, clastic rock and volcanic rock

    二疊儲集層主要由碳酸鹽、沉凝灰、碎屑
  10. These deposits, which can be obviously divided into basic and acid volcanic types, are present in the carboniferous bi - model volcanic series and occur along two horizons, i. e., the lower carboniferous mafic volcanic rock and the upper carboniferous felsic volcanic rock

    這些礦床產在石炭雙峰式之內,沿著下石炭統基性和上石炭統酸性兩個層位產出,分別以玄武和流紋為容礦主,可以明顯地分基性型和酸性型兩種類型。
  11. After the volcanic eruption of multi - phrase cycle - deformation, filling of basin, crustal uplifting event being studied, this dissertation tries constructing the different degree rhythm of magma activity corresponding with crust - mantle dynamic system, studying the crust - mantle deep processes. based on the studies on the characteristics of volcanic rhythm, igneous rocks assemblages, temporal and spatial distribution of igneous rocks, tectonic deformation, the author has util ized the methods of petrology, geochemistry, isotopic geology et al. to do research on the above - mentioned geological problems

    通過多次幕式山噴發-構造變形-盆地充填-地殼隆升事件序列的釐定,從山活動節律特徵、構造組合類型、時空分佈及其演化和構造變形的歷史記錄,利用石學、地球化學、同位素地質學等方法,反演深部過程與淺部響應等來闡明造山過程,建立與不同級別漿活動節律對應的殼幔動力學統,追索殼幔深部過程,已為當今地球動力學研究的前沿課題之一。
  12. The topic of this paper is structure, firstly analyse the earth structure setting of tarim basin and tectonic evolution of tazhong area in silurian - devonian, and give silurian - devonian stratum control and effect, then study the relationship of the development of tazhong uplift, fracture unconformity igneous rock and and oil - gas, at last, on the base of the analyse about history of reservoirs formation, forecast reservoirs pattern, point out favored oil and gas bearing structure and the target. and obtain some important conclusion. 1

    本文以構造研究為主題,詳細的分析了塔里木盆地誌留泥盆沉積時的大地構造背景和塔中地區的構造發展,以及它們對研究區志留?泥盆地層的控制和影響,同時在研究了塔中隆起的形發展演化、斷裂、不整合以及等構造特徵的基礎上,分析了它們與油氣的關,結合志留泥盆突破井的藏史分析,預測了藏模式,最後指出有利含油氣構造,並進行了簡單的目標預測。
  13. The paper gathered deep layers well logging materiak record well materiak core and cutting material of 27 wells in the daqing district, recognized the different type of igneous rock according to their log response feature, and made a large number of cross plot, then carefully chose several of them which works better igneous rock lithology recognition. made pattern recognition procedure using computer to recognize lithology, synthetical many logging parameter to identify igneous rock lithology. and then on the basis of recognizing lithology, the paper analyzed the lithofacies recognition law in this district

    文中採集了大慶地區27口井的深層測井資料、錄井資料、心和屑資料,根據的測井響應特徵識別不同類型的,並做了大量交會圖,精選了幾種識別性效果較好的交匯圖版,編制計算機識別性的模式識別程序,綜合多個測井參數識別性,並在識別性的基礎上,進一步分析本地區相的識別規律,最後結合試油資料,分析本地區儲集空間的特點及油氣與性和相的關
  14. In my article, we first have made a conclusion by reservoir - forming chronology that the forming - age of reservoir is 108. 27 ?. 57ma, of which, the source rock came from carboniferous - permian strata ; we have perfected our basin - modeling software, so it can calculate quantificationally the contribution radio to hydrocarbon - generating caused by igneous intrusion as a technical problem, in which we have a daring trail

    本文首次在文安斜坡應用藏年代學精確地測得了以石炭?二疊紀煤為源的油氣藏藏年齡為108 . 274 1 . 57ma ;進一步完善了盆地模擬軟體,首次定量地模擬計算了侵入對生烴的貢獻這一技術難題,在這一方向上我們作了大膽的嘗試。
  15. The carrying system in the area, dominated by the vertical carrying system, especially type i and type ii carrying faults, linking to every other types of carrying systems each other, composed a three - dimensional network carrying system

    並指出本區油氣輸導統是一個以垂向輸導統為主,以、類主輸導斷層為骨幹,與各類垂向輸導斷層、油源輸導層、不整合以及體等輸導統相溝通的復雜的三維油氣輸導網路統。
  16. The second gas generation starts at the beginning of tertiary and it continues till present. the vertical carrying system and lateral carrying system have been thoroughly investigated for the first time in the study area. their characteristics and evolution history are studied integratedly, synthetically, dynamically, and quantitatively from both bulk properties and micro - features

    整體、統、動態、定量以及宏觀與微觀相結合,首次深入地研究了本區的垂向輸導統(包括斷層垂向輸導統、輸導統等)和側向輸導統(包括具孔滲性能的自源輸導層、它源輸導層等)的特點及其形和演化。
  17. Abstract : based on the isotopic dating data of volcanics and recent research achievements of age boundary between jurassic and cretaceous systems, it is suggested that the volcanic series in shengyuan basin must be attributed to lower cretaceous

    文摘:本文根據盛源盆地同位素年齡數據和侏羅-白堊界線年齡的最新研究果,認為盛源盆地的地層時代應屬早白堊世。
  18. The results of well - to - seismic calibration are effective by selecting permian igneous rock and carboniferous double - peak limestone as the reference layers, adjusting appropriately acoustic velocity and choosing the most suitable wavelet

    利用上述方法,以哈得四油田二疊及石炭雙峰灰為參考層,選取與研究區地震數據吻合性最好的子波,合理地調整聲波速度,對哈得四油田的主要儲層東河砂進行井震標定,獲得了較為理想的效果。
  19. Based on geological environment, bi - model volcanic series, sedimentary formation and geochemical features of volcanic rocks, it is held that the deposits were most probably formed in the carboniferous back arc rifted environment

    根據礦床產出地質環境、雙峰式、沈積建造以及地球化學特徵,推斷昆侖式型塊狀硫化物銅礦床最可能形於泥盆紀石炭紀弧后拉張構造環境。
  20. This paper particularly focuses on the theory and implementation of how to inverse underground structure by comparing incident wave and scattering wave, and recording the spare time of the waves, and forward calculations for igneous, metamorphic and sedimentary rocks are carried out to verify the feasibility

    著重論述了利用慢衰減電磁波的入射波和散射波的振幅關,以及電磁波的走時關反演地下介質參數的基本原理及方法,同時,針對、變質和沉積,通過正演理論計算,說明了慢衰減電磁波測深的可行性。
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