dolomite reservoir 中文意思是什麼
dolomite reservoir
解釋
白雲巖儲集層-
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雲巖油層主要分佈在核二3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。 -
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雲巖油層主要分佈在核二3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。 -
Based on the ground outcrops and drilling core samples, and two - dimensional seismic data in this paper, through a comprehensive evaluation and research of the reservoir characteristics, the authors clarifies that the dolomite of the upper sinian dengying formation and the grain limestone of the lower silurian shiniulan formation are main reservoir rocks in the research area, and the sedimentary facies, karstification, and the number of cracks are the main controlling factors of the reservoir quality
以地表露頭、鉆井資料及二維地震資料為基礎，通過儲層特徵綜合評價研究，認為上震旦統燈影組白雲巖、下志留統石牛欄組顆粒灰巖為區內的主要儲集巖，沉積相、巖溶作用及裂縫發育程度為儲層發育的主控因素。 -
And the author analyses and evaluates hydrocarbon source rock, caprock and trap reserving condition of work area on the base of drilling achievements of 7 emphases structure hi work area. therefore the author draws two conclusion as follow : ( 1 ) the most favorable reservoir of the work area is the spreading region of dolomite rock of carboniferous whose remaining thickness is greater than 20m with the region from jiao 1 well - cizhu 1 well - maan 1 well to west of shizhu county seat. the secondary favorable reservoir of it is the spreading region of dolomite rock with the remaining thickness greater than 10m but less than 20m which is eastern and western region of the most favorable region and the off - lying of yangdu 1 well and yangdu 2 well
本文研究主要通過地層層序、沉積相、成巖作用和儲集條件等方面對該區石炭系黃龍組碳酸鹽巖儲層進行評價和預測，並且從該區7個重點構造的鉆探成果出發進行烴源巖、蓋層和圈閉保存條件等成藏條件的分析與評價，分別得出以下結論：工區最有利的儲層是石炭系白雲巖殘厚20m的分佈區，位於轎1井?茨竹1井?馬鞍1井?石柱縣城以西地區；較有利的儲層是石炭系白雲巖殘厚10 20m的分佈區，位於級區以東及以西的洋渡1 、 2井外圍；不利的儲層是白雲巖10m及石炭系黃龍組灰巖的分佈區，位於工區西南部和東部地區。 -
The reservoir of dolomite is mainly distributed in diagenetic dolostone. so the formation mechanism of diagenetic dolostone have directly relation with that of the reservoir pore
白雲巖儲集巖主要分佈在成巖白雲巖中，因而成巖白雲巖的形成機制便直接與儲層孔隙的形成機制相關。 -
Origin and reservoir of sanshanzi dolomite in lower paleozoic of ordos basin
鄂爾多斯盆地下古生界三山子白雲巖體成因及儲集性 -
Main diagenesis of carbonate reservoir as following : ( 1 ). there are five types of dolomitization : evaporative pumping, seepage reflux, mixing and deep buried. ordivician main type of dolomite of qianmiqiao buried hill in dagang oilfield is elogenetic micrite and microspar dolomite
5 、對碳酸鹽巖儲層的成巖作用分析認為： （ 1 ）白雲巖化作用有四種類型：蒸發泵白雲化作用、迴流滲透白雲化作用、混合水白雲化作用、深埋藏白雲化作用。 -
Technique for prediction of dolomite fractured reservoir has been quite urgent for petroleum exploration and development in biyang sag
摘要白雲巖裂縫型儲集層預測技術是目前在勘探開發中迫切需要解決的問題。
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