diagenesis n.【地質學;地理學】成巖作用,巖化作用。
n. 【地質學;地理學】成巖作用,巖化作用。 “chemical diagenesis“ 中文翻譯: 化學成巖作用“coal diagenesis“ 中文翻譯: 煤成巖酌“early diagenesis“ 中文翻譯: 早期成巖作用“initial diagenesis“ 中文翻譯: 初始成巖作用“late diagenesis“ 中文翻譯: 晚期成巖作用“middle diagenesis“ 中文翻譯: 中期成巖作用“organic diagenesis“ 中文翻譯: 有機成巖作用“peat diagenesis“ 中文翻譯: 泥炭巖化作用“retrograde diagenesis“ 中文翻譯: 退化成巖作用“diagenetic“ 中文翻譯: 成巖作用的“diageneses“ 中文翻譯: 成巖作用“diagenetic change“ 中文翻譯: 成巖變化“diagana stephane“ 中文翻譯: 迪亞加納“diagenetic deformation“ 中文翻譯: 沉積變形;原狀變形; 成巖形變作用“diagana moussa“ 中文翻譯: 迪亞賈納穆薩“diagenetic degradation“ 中文翻譯: 成巖降解作用“diagana“ 中文翻譯: 迪亞加納; 迪亞賈納“diagenetic deposit“ 中文翻譯: 成巖沉積物“diag(diagram)“ 中文翻譯: 線圖
diageotropism |
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In this research , some conclusions are followed : l ) in the tahe oilfield , multiphase tectonic movement and pleokarst were so deeply worked on the diagenesis that the types of diagenesis are various , and the relation of those are complicated 本次研究最終得出如下結論: 1 )研究區由于受到多期構造運動的影響,又受到多期古巖溶作用的疊加改造,成巖作用類型多樣,關系復雜。 |
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The diagenesis may result in the variations in pore structures of sandstone reservoirs ; the compression and cementation may lead to the decrease in valid primary porosity of sandstones , and the secondary porosity generated by solution may serve as main oil storage spaces 壓實作用和膠結作用降低了砂巖的原生孔隙度,溶解作用產生的次生孔隙成為主要的汕氣儲集空間。 |
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Pressure separation is usually controlled by the following factors , such as subsidence rate , sediment types and diagenesis during the diagenetic evolution , as a result the pressure gradient is uncontinuous 地層壓力分隔化是由于沉積物在成巖演化過程中受各種因素,如沉積速率、沉積物類型以及成巖作用的影響,使地層中的流體壓力梯度呈現出隨深度變化不連續的一種現象。 |
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These characteristics have close relation with transgression from eastern to western . 4 . reefs undermined various and complicated diagenesis , in which cementation , dolomitization and corrosion etc . play main roles in the history of reef diagenesis 4礁巖的成巖作用具多樣性和復雜性,其中泥晶化、填積、膠結、白云化和溶蝕作用最為重要。 |
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Abstract : lacustrine dolomite reservoir in the hinterland of biyang sag is mainly distributed at no . 2 and no . 3 sections of hetaoyuan & nbsp ; with its development controlled mainly by the lithology diagenesis and nose ? like structure 文摘:泌陽凹陷腹部湖相白云巖油層主要分布在核二3和核三2段,其發育程度主要受巖性、成巖作用和鼻狀構造控制。 |
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Due to the sensitivity of the clay minerals , however , any climatic influence upon the compositions of clay minerals can be easily covered up by extra - climatic events such as source rock , sedimentary environment , and diagenesis 然而,由于粘土礦物的敏感性,其氣候記錄的信息往往會被其他影響因素(如母源區、沈積環境、成巖作用等)掩蓋。 |
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The examination of the controls of the reservoir rocks indicates that the sedimentary microfacies and diagenesis are the principal geological factors controlling the development and distribution of the reservoir rocks in the study area 儲層控制因素的綜合分析認為,沉積微相和成巖作用是控制或影響該區儲層發育與展布的主要地質因素。 |
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The establishment of the quantified system on the diagenesis intensity of the clastic strata in upper paleozoic of ordos basin aimes to provide a kind of quantification investigation project for the diagenseis in this region 摘要鄂爾多斯盆地上古生界是天然氣的重點儲集地層,成巖強度定量化是地層成巖作用研究的基礎。 |
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The process of diagenesis controlled partly by sedimentation , the evolution of pores influenced by it . the affection of origin ingredient and structure in sand to sediment and solution in gooey be exhibited 長6儲層砂體中沉積作用對于成巖進程的控制,主要表現在砂巖的原始成分和結構對于膠結物的沉淀和溶蝕的影響。 |
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Lacustrine dolomite reservoir in the hinterland of biyang sag is mainly distributed at no . 2 and no . 3 sections of hetaoyuan with its development controlled mainly by the lithology diagenesis and nose ? like structure 泌陽凹陷腹部湖相白云巖油層主要分布在核二3和核三2段,其發育程度主要受巖性、成巖作用和鼻狀構造控制。 |
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In triassic and lower - middle jurassic , there is the acid diagenetic ambient , where inter - pore fluid is from the organic acid released from the coal measures during diagenesis 三迭系至中下侏羅紀煤系為酸性成巖環境,它們在成巖過程中釋放的有機酸使隙間流體呈酸性。 |
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( 2 ) the comparative study on pge geochemistry indicated that it exists multiple diagenesis and mineralization in jinchuan superlarge copper - nickel sulflde deposit ( 2 )通過鉑族元素地球化學研究,比較論證了金川超大型鎳銅硫化物礦床的多次成巖成礦作用。 |
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Reservoir properties are mainly controlled by sedimentary microfacies and diagenesis ; the effect of the tectonic movements on the reservoir is relatively limitted 研究區儲層性質主要受沉積微相和成巖作用的控制,構造運動對本區儲層性質的影響較有限。 |
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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布。 |
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Ordovician carbonate rock bed of ordovician reservoir in qianmiqiao buried hill experienced two times of karst exposure and the post plaeogene deep - buried diagenesis 摘要千米橋潛山奧陶系儲層經歷了兩次裸露巖溶及古近紀后的深埋藏成巖作用。 |
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Sedimentation - diagenesis deposits mainly formed during late sinian to cambrian period , such as bingtongshan pbzn deposits and aozigang deposits 沉積成巖型鉛鋅礦主要成礦時代屬晚震旦世~寒武紀,如冰洞山式鉛鋅礦床和凹子崗鋅礦床。 |
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Finally regional distribution of reservoir has been predicted . study suggests that feixianguan formation is essentially controlled by sedimentation and diagenesis 研究表明,飛仙關組儲層主要受沉積作用和成巖作用的控制。 |
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The diagenesis of the ed3 and es , sandstone has been evoluted to late diagenesis a and b stage , with mainly primary pores and secondary solved pores 油氣儲層的儲集空間以原生孔隙、次生溶解孔隙為主,主要為中孔中滲儲層。 |
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Chang - 2 oil - bearing beds of the yanchang formation experienced three diagenetic stages of early diagenesis , late diagenesis and epidiagenesis 研究區長2油層組經歷了早期成巖階段、晚期成巖階段和表生成巖階段三個成巖階段。 |