diagenesis 中文意思是什麼
diagenesis
解釋
n. 名詞 【地質學；地理學】成巖作用，巖化作用。-
The sedimentation is the foundation, affecting the basic pattern of the reservoir, and the sedimentary facies zones beneficial to the formation and evolution of the reservoir includes platform edge bank facies, introplatform point beach facies and acclivity sedimentary facies, etc. ; the diagenesis is the key factor, determining the pattern and scope of the final distribution of the reservoir and being of great influence on reservoir structure, and the diagenesis of promoting the formation of storage rooms is mainly the dissolution occurred during hypergene stage and burial stage ; and the tectonism is the condition of influencing the connectivity among various reservoir bodies and among the storage rooms within a single reservoir body
該套儲層是在4億年左右的地質歷史中，由沉積、成巖和構造作用相互影響而形成的最終成果：其中沉積作用是基礎，影響著儲層的基本形態，有利於儲層形成與演化的沉積相為臺地邊緣灘、臺內點灘和上斜坡等沉積相帶；成巖作用是關鍵，決定了儲層的最終分佈形態和范圍，對儲層結構的影響至關重要，促進儲集空間形成的成巖作用主要有表生期和埋藏期的溶解作用；構造作用是條件，影響著各儲集體之間以及單一儲集體內部儲集空間的連通情況。 -
Spray-zone diagenesis or seepage is another variant on hypersaline brine alteration of contemporaneous carbonates.
浪花帶的成巖作用或滲濾作用是影響同生碇酸鹽的起鹽囪水變化的另一個因素。 -
Burial diagenesis can cause the kaolinite group of minerals to be neoformed, transformed or destroyed.
埋藏成巖作用能使高嶺石類礦物新生變形，轉化或消失。 -
These changes reflect the effects of burial diagenesis on the originally deposited clay mineral assemblage.
這種變化反映了埋藏成巖作用對原來沉積的粘土礦物組合的影響。 -
Scanty but growing evidence links the character of early diagenesis with specific depositional environments.
有關早期成巖作用的特徵與特定沉積環境的關系，證據雖然不多，但卻在不斷增加。 -
Burial diagenesis causes a progressive transformation of smectites, the end-products being dependent on ph and pore water chemistry.
埋藏成巖作用可使蒙脫石進一步轉化，最終產物決定於PH值及孔隙水的化學性質。 -
In terms of petroleum exploration, diagenesis is an immature stage when mostly carbon dioxide, water, and some methane and heavy hetero-compounds are generated.
在石油勘探術語中，成巖作用是一個未成熟階段，這時多半生成二氧化碳，水，一些甲烷和重質雜化合物。 -
Early diagenesis in surface soil of yellow river delta
黃河三角洲表層土壤早期成巖作用初探 -
Diagenesis and pore evolution of deep sandstones in jiyang depression
濟陽坳陷深層砂巖成巖作用及孔隙演化 -
Diagenesis and pore evolution of ordovician carbonate reservoirs in qianmiqiao buried hill
以千米橋潛山凝析氣藏為例 -
Synthetic model of sedimentation, diagenesis and pool formation of paleogene for dongying sag
成巖和油氣成藏綜合模式 -
Under the guidance of the theories of sedimentation, paleontology, stratigraphy, reservoir geology and digenesis, synthetically applying the methods of the conjunction of spot - line - surface, macro - microscopic and field - indoor, there is a comprehensive study for the upper permian series in stratum, rock, sedimentary facies and diagenesis, especial for the type and characteristics of sedimentary facies, in the paper. based on the above, the vertical evolutionary model of the sedimentary environment is explained by the study of the elevation profile and transverse profile and the regional geological characteristics
本文主要是以沉積學、古生物學、地層學、儲層地質學等相關理論為指導，運用點線面、野外與室內、宏觀與微觀相結合的方法，並藉助普通顯微鏡、陰極發光顯微鏡等手段對川西地區北部上二疊統的地層、巖石、沉積相以及成巖作用進行了研究，尤其是對沉積相的類型及特徵作了詳細的劃分與闡述。 -
At the late diagenesis phase, the dissolution of frame grains, especially the dissolution of felspar and laumontite, is the key to form secondary porosity
朵狀砂體的大小直接控制油藏的范圍及規模，靖安地區的主要油藏多沿不同的朵狀體成排分佈。 -
Three diagenesis types are help to differentiate the middle caledonian and early hercynian karst, which are stylolite, dolomitization and dedolomitization. 2 ) karst identification symbols and karst reservoir of ordovician in bores, logging, well logging and fmi have been established. karst reservoir have been identified and evaluated in the tahe oilfield
2 ）建立了奧陶系巖溶在巖芯、錄井、常規測井和成像測井上的識別標志，以及巖溶型儲層在以上方面的識別標志，並對研究區內巖溶型儲層進行了識別和評價。 -
The result is that this gas pool has simple structure, only forms a little nose - like structure at the district of fenghuangshan ; this pool belongs to delta front sub - facies sedimentary model, the underwater distributary channel and mouth bar is the better sedimentary microfacies ; the physical property of the reservoir is poor, the type of pore of the reservoir rock mostly are intergranular pore, intergranular solution hole and little are intercrystalline micropore ; the influential factors of pore structure and physical property are lithofacies, lithologic character and diagenesis ; the off - take potentia of all the testing well are deadly shortness, the wells have the worth of industrial recovery only under the condition of going through sand fracturing, and in the early of binging into production, the oil and sheath pressure drop rapidly, the production of the well drop rapidly
研究認為該氣藏構造簡單，只在鳳凰山形成了一個小型的鼻狀構造；屬於三角洲前緣亞相沉積模式，水下分流河道和河口壩是有利的沉積微相；儲層物性差，儲層巖石的孔隙類型主要有粒間孔、粒間（內）溶孔及少量晶間微孔；影響蓬萊鎮組氣藏儲層孔隙結構及儲集性的因素有巖相、巖性條件及成巖作用；所有測試井自然產能都極低，必須經加砂壓裂后才有工業開采價值，且投產初期，油套壓下降較快，氣井產量下降迅速。 -
Owing to extensive distribution of the oolite in t1f3 in west hubei and east chongqing, the oolitic beach reservoir is becoming a focus to research in the region. based on the monographic studies of depositional environment and sedimentary facies, diagenesis and pore evolvement, elementary characteristics of the reservoir, the paper endeavored to educe comprehensive appreciation and forecast to oolitic beach reservoir in t1f3 in west hubei and east chongqing
本論文即圍繞鮞灘儲層這個中心，在對沉積環境與沉積相、成巖作用與孔隙演化以及儲層基本特徵等進行專題研究的基礎上，力爭對鄂西渝東區飛三段鮞灘儲層作出綜合評價與預測。 -
A study on upper paleozoic group sandstone diagenesis in fuxian area of ordos basin
富縣地區上古生界砂巖成巖作用研究 -
This paper emphasizes the effect of the dissolution of aluminosilicate during diagenesis may provide more radiogenic strontium which would result in a high content of strontium in carbonate rocks. so we should avoid the vein of carbonate and select the samples with less terrigenous clastic, less grain content and lacking calcite cementation collected as analysis samples. the microcrystalline limestone and micro - to fine - crystalline dolomite are rather fairly whole rock samples
作者還強調了成巖過程中由長石等鋁硅酸鹽溶解提供殼源sr所造成的碳酸鹽礦物成巖蝕變可能表現為較高的sr含量；因此，在用全巖樣品進行旨在反映海水組成的各種分析時，應迴避碳酸鹽脈，選擇含陸源碎屑低、顆粒數量少、缺乏方解石膠結物的樣品，微晶灰巖或微?粉晶白雲巖是較為理想的全巖樣品。 -
Reefs are well developed in western hubei and eastern chongqing. through sedulous research, the whole acquaintance on types of reef builders, types of reef carbonatite, development and evolution of reef organisms, division of reef facies, distributing regularities of reefs and diagenesis has been concluded. according to the comprehensive studies, the following results and conclusions have been obtained
通過對鄂西渝東區上二疊統長興組生物礁造礁生物、沉積相、成巖作用的研究，認清了礁體的主要造礁生物類型、主要巖石類型、生長演化、相帶劃分、分佈規律以及成巖作用，可以得出以下結論和認識： 1生物礁主要分佈於晚二疊世碳酸鹽臺地內部和臺地邊緣，可分為三種類型。 -
Diagenesis and controlling factors of the turbidite reservoir of sub - middle of the third member of shahejie formation in niuzhuang sag
牛莊窪陷沙三中亞段濁積巖儲層成巖作用及主控因素分析
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