酸式巖 的英文怎麼說

中文拼音 [suānshìyán]
酸式巖 英文
acid salt
  • 酸 : 酸構詞成分。
  • 式 : 名詞1 （樣式） type; style 2 （格式） pattern; form 3 （儀式; 典禮） ceremony; ritual 4 （自然科...
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  1. ( 4 ) based on the analysis and summary of typical orogenic belt in china, advancing the marker to distinguish the exist of delamination occurred in orogenic belt, especially giving up some new marker such as ring ultrabasic - basic - medium acid rock body, local bimodal continental rifting volcanic activity ; rapakivi granite, etc. ( 5 ) collating the main stages of south part of sanjiang orogenic belts evolution after the close of old nanchangjiang ocean, i

    較全面地提出了判別造山帶成熟拆沉作用發生的標志，特別是根據對我國典型造山帶的總結分析，提出了一些新的標志，如環狀超基性一基性一中酸性雜巖體;局部雙峰式大陸裂谷型火山活動;二長花崗巖、堿性花崗巖和奧長環斑花崗巖;地殼局部短暫下沉;等等。
  2. These geomorphic units of paleogeography constitute the basic model of paleocontinent, littoral - neritic sea and carbonate plateform at that stage, and this depositional model is similar to the pattern of the east china continent and ocean, which is the result of evolution during the past long geologic age

    這些古地理地貌單元構成了湖北省泥盆紀時期古陸濱淺海和碳酸鹽巖臺地的基本沉積模式，這種沉積模式與現今中國東海大陸、海洋格局基本一致，亦是經過了漫長地質歷史時期演化，而形成現今這種格局的。
  3. 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

    這些礦床產在石炭系雙峰式火山巖系之內，沿著下石炭統基性火山巖和上石炭統酸性火山巖兩個層位產出，分別以玄武巖和流紋巖為容礦主巖，可以明顯地分成基性火山巖型和酸性火山巖型兩種類型。
  4. In the aspect of metallogenic theories, this paper mainly presents retrospects of the research history of such problems as varied and complex submarine ore - forming processes, three huge metallogenic provinces, metallogenic models, intermediate - acid magmatic rocks and their related ore - forming processes, stratabound deposits and the application of isotopes, trace elements and fluid inclusions to metallogenic studies

    在成礦理論方面，主要就多樣復雜的海底成礦，三大巨型成礦域，成礦模式，中酸性巖漿巖及有關成礦作用，層控礦床，同位素、微量元素及氣液包裹體運用於成礦等問題的研究歷史作了回顧。
  5. Among the felsic rocks, samples from the zhangjiakou formation ( fm. ) are characterized by moderately to strongly eu anomalies, and variable negative anomaly of sr, ti and p, whereas samples from the donglingtai fm. exhibit enriched lree and flat hree patterns with nb / ta fractionation and high zr / sm ratios

    在中酸性火山巖系列中，張家口組火山巖表現出中等-強烈的eu負異常和不同程度的sr 、 ti 、 p負異常；東嶺臺組火山巖表現出富集lree和平坦的hree的稀土配分模式， nb ta分餾，高zr sm比值。
  6. The structure of activity of humic was affected by utilization and soil forming mother rock. as the human behavior frequently disturbed the soil, humic molecules weight became less ; polycondensation degree and aromatility of soil humic deceased, and its activity became intense

    利用方式和母巖都影響著土壤腐殖質胡敏酸的結構和活性，人為影響愈頻繁，土壤腐殖質胡敏酸分子量小、縮合度和芳構化度低、活性強。
  7. The results demonstrate that the pingba red residua is a typical in situ chemical weathering crust, and the material sources of the profile are derived from underlying triassic dolomites, the chemical weathering of dolomite can be divided into two stages : " leaching - accumulating trend " and weathering trend ", the stable teconic and whole weathering of dolomite should be the main reason for the development of thick and consecutive red weathering crust overlying dolomite rock in central guizhou

    結果顯示該剖面是下伏基巖白雲巖風化成土並累積的結果，無其他外來物源，是原位風化殼；成土過程具有兩階段模式特徵，即白雲石、方解石的溶蝕酸不溶物累積和酸不溶物進一步風化兩個階段；長時期的構造穩定和白雲巖整體溶蝕作用是黔中地區白雲巖風化殼土層厚度大、分佈連續的主要制約因素。
  8. All the mafic and felsic volcanic - hosted massive sulfide deposits are therefore defined as the kunlun type volcanic - hosted massive copper sulfide deposit

    這些基性火山巖型和酸性火山巖型礦床被統稱為昆侖式火山巖型塊狀硫化物銅礦床。
  9. Karst cycle ii could reconstructed the middle and upper ordorician, and the cave preservation of the karst cycle ik iii are better than the cave of the karst cycle i. 5 ) the genetic forecast mode of karst reservoir in the tahe oilfield are founded on the basis of the research of pleokarst topography, pleodrainage system and karst cycle

    巖溶旋迴可改造中上奧陶統，巖溶旋迴、的洞穴保存情況好於巖溶旋迴中的洞穴。 5 ）通過巖溶古地貌、古水系和巖溶旋迴的探討，初步建立了塔河油田奧陶系碳酸鹽巖巖溶型儲層成因預測模式。
  10. For the first time, take tarim basin as an example to establish theoretical, industrial threshold value of organic enrichment of carbonate source rocks. calculate gas quantity of generation, adsorption, dissolving in oil, dissolving in water, diffusion of unit area carbonate rocks at different geologic conditions. and then according to the material balance principle, figure out the corresponding organic carbon content when gas being started expelling from source rocks with separate phase

    分別計算了不同地質條件下單位面積碳酸鹽巖的生氣量及源巖和圍巖各種形式的殘留和耗散氣量（吸附氣量、油溶氣量、水溶氣量、擴散氣量） ，進而根據物質平衡原理計算出源巖開始以游離相有效排氣時所對應的有機碳含量，並將它作為該地質條件下氣源巖的有機質豐度理論下限值。
  11. Calculate gas quantity of generation, adsorption, dissolving in oil, dissolving in water, diffusion of unit area carbonate rocks at different geologic conditions. and then according to the material balance principle, figure out the corresponding organic carbon content when gas being started expelling from source rocks with separate phase. regard it as the theoretical threshold value ( tocmin ) of gas source rocks at that same geologic condition

    分別計算了不同地質條件下單位面積碳酸鹽巖的生氣量及源巖和圍巖各種形式的殘留和耗散氣量（吸附氣量、油溶氣量、水溶氣量、擴散氣量） ，進而根據物質平衡原理計算出氣源巖開始以游離相有效排氣時所對應的有機碳含量，並將它作為該地質條件下氣源巖的有機質豐度理論下限值。
  12. A new model for determining the weathering components in red weathering crust over dolomites

    碳酸鹽巖上覆紅色風化殼中風化組分確定的一種新模式
  13. Volcanic rock is quite different from sandstone and carbonate rock in diagenetic model, petrology and reservoir characterization

    火山巖在成巖模式、巖石學和儲集層特徵上，與砂巖、碳酸鹽巖有很大區別。
  14. The new results of which are as follows : l. paricular seven identification mark from up - shallowing to exposed surface in taphrogenic trough have been built, the first modelling of the identification mark of carbonate sequence boundary is very important in theory

    首次將碳酸鹽巖層序變化識別特徵模式化，具有重要的理論意義。 2 、提出了影響油氣聚集勘探單元劃分的新見解。
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