鹽沉積 的英文怎麼說
中文拼音 [yánchénjī]
鹽沉積
英文
salt deposit-
The lacustrine carbonate rocks in the wudaoliang group consist of boundstone ( stromatolite ), micritic limestone, grainstone and micritic dolostone which were laid down in the shallow - water to bathyal, high - salinity and enclosed to semi - enclosed lake systems
五道梁群湖相碳酸鹽巖分為生物粘結灰巖（疊層石） 、泥晶灰巖、顆粒灰巖與泥晶白雲巖四大類，反映出沉積環境為一個具有淺水半深水、高鹽度、半封閉封閉特點的綜合湖泊系統。" it could be acidic water, it could be briny water, it could carry lots of sediment or be slushy, but [ it appears that ] water is involved, " edgett added
「那可能是酸水，可能是鹽水，可能攜帶有很多沉積物，也可能是泥濘的，但看上去跟水肯定有關系。 」The lower part formed in a littoral - epeiric environment, is a series of elastic rocks, partly contains carbonate rock and metamorphic basic volcanic rocks and the upper part formed in a bathypelagic environment is a series of sediments with chert, partly contains metamorphic basic volcanic rocks
其下部為一套濱淺相碎屑巖，局部夾碳酸鹽巖、變質基性火山巖；上部為一套深水沉積巖系夾硅質巖，局部夾變質基性火山巖。In many sedimentary basins the salinity of the formation water increases with depth or compaction.
在許多沉積盆地中，地層水的含鹽量隨深度或壓實作用而增高。Assemblage ) represented the coastal shallow - water environment ; factor 2 ( protelphidium tuberculatum assemblage ) represented the alongshore cold - water current area or cold shallow sea environment ; factor 3 ( elphidium magellanicum assemblage ) represented the sh allow sea ( < 20 - 30m depth ) deposit ; factor 4 ( ammonia ketienziensis assemblage ) represented the shallow - sea water more than 50m depth ; and factor 5 ( buccella frigida assemblage ) represented the colder - water sea environment ; and the distribution of factor load accorded with the character of benthic foraminifer community
Q型因子分析揭示ey02 - 2孔5種有孔蟲組合，分別對應濱岸鹽沼環境、黃海沿岸流冷水分佈區、高潮坪淺海沉積環境、水深大於50m的現代淺海環境及較冷的沉積環境。因子載荷的分佈與有孔蟲群落特徵吻合較好。南黃海有孔蟲含量? ?水深轉換函數關系式有一定的局限性，並不能在南黃海陸架地區推廣使用。On this surface the encroaching muskeg sea developed a carbonate bank fringed by coastal sabkhas in which gypsiferous deposits were formed.
在這個地表上，侵入的馬斯愷格海發育了一個碳酸鹽灘，其邊緣有海岸薩勃哈石膏質沉積形成。In middle and late periods of the early permian, the pre - caspian areas rose successively, the climate became dry, and the environment turned to be supratidal zone ( evaporitic environment ), resulting in the spread sedimentation of salts and the formation of the salt sediment group ( the upper part of the lower permian ) which consists mainly of halite and anhydrite
早二疊世中後期由於持續構造抬升，盆地氣候變得乾旱，海水變淺，潮上帶蒸發環境發育，以致這一時期廣泛發育鹽類沉積，形成含鹽層系，主要由鹽巖和硬石膏層構成，並形成許多大小不等的鹽丘構造。Besides, the sedimentary facies of upper ganchaigou and lower ganchaigou formation were also mapped in supersequences which are the main target strata for exploration. the high resolution sequence stratigraphic framework showed the genetic relationship between the distributions of sedimentary facies and their tectonic settings. the near - source sedimentary systems such as subaqueous alluvial fan and lake - floor fan are often deposed in rise - hemicycles in the steep slope background in the north, the coarse lithology of fan - delta prograded from north to south in fall - hemicycles, and the braided stream facies are formed in the rise - hemicycles in gentle slope background in the south, braided stream facies prograded from sorth to north in the fall - hemicycles, but the lacustrine facies and salt lake facies developed in the middle part of the area
詳細的沉積相研究發現，紅獅地區第三系發育有沖積扇、水下沖積扇、河流、三角洲、扇三角洲、湖泊和湖底扇7種主要沉積相類型，並對作為區內主要勘探目的層系的下乾柴溝組和上乾柴溝組進行了以超層序為單位的沉積相平面編圖，以較高的時間解析度揭示了區內沉積相帶的平面展布及其在不同構造背景中的分佈規律，比如在北部的凹陷陡坡背景下，上升半旋迴低水位期通常發育有水下扇、湖底扇等陡岸近源特徵的沉積體系，下降半旋迴高水位期，扇三角洲相粗碎屑巖由北向南進積;在南部的凹陷緩坡背景下，上升半旋迴主要發育辮狀河流相，下降半旋迴辮狀河三角洲相由南向北進積;而中部紅柳泉一獅子溝一帶則為湖泊相沉積和鹽類沉積。The fluids upwelled to seafloor along fault thus ore - forming metals accumulated. 2. this paper indicated the definition the hydrothermal sedimentary rocks. the definition is a group of especial sedimentary rocks forming at the temperature ranging from 70 ? to 350 ? ( or more high ) through sedimentation and synsedimentary metasomatism in the seafloor
區內的熱水沉積巖主要有硅質巖、鈉鉀長石巖、重晶石巖、透閃石巖、碳酸鹽巖、綠泥石巖和鐵白雲石斑點千枚巖，它們往往與熱水沉積礦體緊密伴生。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。Prokaryotic microbial diversity of the ancient salt deposits in the kunming salt mine, p. r. china
昆明鹽礦古老巖鹽沉積中的原核生物多樣性This japer introduces characteristic of peroxide bleaching, advantage and disadvantage of sodium silicate used for principal additive in peroxide bleaching process, mechanism of silicate precipitating, practice in control of silicate deposition in dip production
摘要本文介紹了過氧化氫漂白特點，硅酸鈉作為過氧化氫漂白的重要添加劑的優缺點，硅酸鹽沉積機理，脫墨漿生產中防止硅酸鹽垢的生產實踐。In the early sinian, clastic sediments formed by fluvial and continental glacial actions were developed, while in the late sinian, great thickness of marine carbonate rocks formed by two transgression - regression cycles were developed
早震旦世發育由河流作用與陸地冰川作用形成的陸源碎屑沉積；晚震旦世則發育由兩次臺地盆地臺地的海進海退旋迴形成的巨厚海相碳酸鹽沉積。Carbonate sediments in all environments are basically products of an ancient biochemical system.
一切環境的碳酸鹽沉積物，基本上都是古代生物化學體系的產物。With regard to the causes of formation and sources of salt, people have different point of views in different basins, and different depositional models are set up, even in one same basin there are also divergent view to exist different opinions still exist on the position of the salt bearing strata in sequence stratigraphy. it will greatly influence the exploration level of resources in salt - bearing basin if the above doublts can not be made clear. in this way, it will be of great significance to make it clear about the above issues and the relationships about salt and oil & gas
對于鹽巖的成因及鹽源在不同盆地有不同的認識，並建立了各自的沉積模式，就是同一含鹽沉積盆地或含鹽沉積凹陷人們的認識依然分歧很大，關于鹽巖在層序地層中的位置人們的認識依然不同，對這些問題的認識不清將極大的影響對人們含鹽盆地的能源勘探開發水平，因此搞清鹽巖的成因及其與油氣聚集的關系具有重要意義。An abnormal condition in which calcium salts are deposited in a part or tissue of the body
鈣質沉著鈣鹽沉積于體內某一部件或組織的不正常狀況Results : the primary cells formed a monolayer in 18th day. von - kossa staining presented mineral deposition after the cells had been cultured 30 days in calcified solution. conclusion : bmsc can be isolated and cultured easily
結果:原代細胞培養第18d細胞融合成單層，長滿整個培養皿;倒置顯微鏡下觀察，礦化條件下，細胞培養30天， von一kassa染色顯示有局灶狀鈣鹽沉積。The archaea contain many organisms of extreme environments, such as hydrothermal vents, hot springs, saline sediments, volcanic craters and boiling muds. they include methane - generating organ - isms ( methanogens ), sulfate reducers, and extremophiles
古細菌包括許多生長在極端環境中的有機體，如高熱溫泉口，高鹽沉積地區，火山噴發處，沸騰的巖漿中等的生物有機體，還包括產甲烷菌等。Reefs or bioherms are an impotant type of carbonate deposits. they are consist of numerous and all kinds of organisms, or resulted from biological action
生物礁是碳酸鹽沉積中的一種重要類型，這是由大量的、各種各樣的生物堆積而成，或是生物作用的產物。Based on the principle and methods of carbonate sedimentology and reservoir diagenesis, and guided by the theories of carbonate reservoir geology, the diagenesis, controlling factors for reservoir and distribution of reservoir of feixianguan formation in northeast sichuan have been comprehensively studied. multiple methods from different branches of geology and advanced analyze and test technology have been used in mis research. the type and characteristics of diagenesis are described in detail, burial solution model and dolomitic model established, diagenetic environment and diagenetic stage divided
本文以碳酸鹽沉積學和成巖作用原理和方法為基礎，以碳酸鹽巖儲層地質學理論為指導，採用多學科、多技術的綜合分析方法，配以先進的分析測試手段，重點對川東北地區飛仙關組碳酸鹽巖成巖特徵、儲層控制因素及儲層分佈等作了廣泛而深入的研究。分享友人