鮞粒 的英文怎麼說

中文拼音 [ērlì]
鮞粒 英文
oolite
  • 鮞 : Ⅰ名詞[書面語]1. （魚卵） roe2. （魚苗） fryⅡ形容詞（鮞狀的） oolitic
  • 粒 : Ⅰ名 （小圓珠形或小碎塊形物） small particles; grain; granule; pellet Ⅱ量詞（用於粒狀物）
  1. Original porosity is typified by the intergranular porosity of sandstones and the intercrystalline and oolitic porosity of some limestones

    原生孔隙度以砂巖粒問孔隙度和某些石灰石的晶體粒間和鮞狀孔隙度為代表。
  2. Oolite lime sand packs naturally with 40% porosity because the particles are essentially spheroids.

    自然堆積的灰質鮞粒砂具有40的孔隙度，因為其顆粒其本上都是球狀的。
  3. The middle part is a set of large tidal range tidal sequence including oolitic shoal fades which is made up of bedded - oolite dolomite and oolite limestone, gypsum - tidal fades in sabkha environment which consists of bedded gypsolyte, and gypsolyte - bearing gypsum - dolomite tidal facies

    中部為層狀鮞粒白雲巖、鮞粒灰巖的潮下鮞粒灘相與薩布哈環境的富層狀石膏巖的膏坪相、含石膏巖的膏雲坪相組成的大潮差蒸發潮坪層序。
  4. However, the authors discovered recently that the top and bottom surfaces of the loushanguan formation are palaeokarst unconformity interfaces, and there are a lot of interbeds of granular ( oolite, pisolite and oncolite ) dolomite and algae - mat dolomite, especially sedimentary structures such as the bird ? s eye, stromatolite, cross bedding and tepee structures

    但筆者新近研究發現，其頂、底均為古巖溶不整合面，並有大量顆粒（鮞、豆、核形石）白雲巖和藻紋層白雲巖夾層，還有許多鳥眼構造、疊層石構造、交錯層理、帳蓬構造存在。
  5. The primary rocks were sparry oolitic limestone and micrite oolitic limestone, but dolomitization destroyed the original sedimentary textures

    原生巖石為亮晶鮞粒石灰巖和泥晶鮞粒石灰巖，白雲石化作用使其巖石結構大多遭受破壞。
  6. These internal - tide deposits can be classified into four basic types according to their features, i. e., bi - directional cross - laminated fine - grained sandstone, unidirectional cross - bedded and bidirectional cross - laminated medium - grained to fine - grained sandstone, rhythmic thin alternating beds of sandstone and mudstone, and oolitic limestone

    這些內潮汐沈積進一步劃分? 4種類型：雙向交錯紋理細砂巖型、單向交錯層和雙向交錯紋理中細砂巖型、韻律性砂泥巖薄互層型和鮞粒灰巖型。
  7. Characteristics of feixianguan formation oolitic shoal reservoirs in northeast sichuan basin

    川東北飛仙關組鮞粒灘儲層特徵研究
  8. Oolitic limestones are rare and interbedded in the dark - gray mudstones and / or shales

    這些砂巖和鮞粒灰巖既可單獨成層，但更常見它們與深灰色泥頁巖組合成薄互層。
  9. Diagenesis of oolitic bank of the feixianguan formation of lower triassic in luojiazhai gas field, northeastern sichuan province

    川東北羅家寨氣田下三疊統飛仙關組鮞粒灘成巖作用
  10. According to its fades sequence features, the oolitic rocks are deposited in platform marginal oolitic bar and inner - platform oolitic bank

    蒸發臺地西緣的臺緣鮞粒壩在飛仙關期基本穩定。
  11. The feixianguan gas reservoirs in the luojiazhai gas field, northeastern sichuan province, are composed of the porous oolitic dolomites

    摘要四川東北部羅家寨氣田的儲層為下三壘統飛仙關組孔隙性鮞粒白雲巖。
  12. The reservoirs mainly exist in the oolitic bank facies in the carbonate platforms, which were deposited in high energy environment and mainly controlled by tidal action

    其沉積相屬碳酸鹽臺地的鮞粒灘相，為臺地潮下較高能環境沉積，主要受潮汐作用的控制。
  13. The paper analyzed sedimentary characteristics and depositional environment in t1f3 this region firstly, and on the grounds of establishing logical deposit pattern gave emphasis to make a study of distributing laws and spreading traits of the oolitic beach. because diagenesis is a vitally dominating factor that influenced oolitic beach reservoir nature in the region, the master diagenetic events of the reservoir in the lengthy geological history, as well as the influence to the pore abundance, was made a study of. the diagenetic stages and sequences were divided and the pore evolve pattern was established in the paper

    本論文首先分析了研究區飛三段的沉積特徵與沉積環境，在合理建立沉積相模式的基礎上重點研究了鮞粒灘（壩）的分佈規律和空間展布特點；成巖作用是影響本區鮞灘儲集性至關重要的控制因素，論文詳細研究了儲層在漫長地質歷史過程中所經歷的主要成巖事件及其對孔隙發育的影響，劃分了成巖階段與成巖演化次序，建立了孔隙演化模式並以建南構造為例進行了成巖相展布研究的嘗試；最後還在鮞灘儲層基本特徵研究的基礎上對飛三段儲層進行綜合評價與預測。
  14. Based on the principles of palaeobiology, stratigraphic geology, sedimentology, diagenesis and reservoir geology, taken field profile and drilling cores as research object, and combined with achievement of predecessors, the sedimentary facies, diagenesis essential characteristics of reservoir and controlling factors for reservoir of feixianguang formation in northwest sichuan have been comprehensively studied. both classic and mordern methods have been used in this research. the main confents includes : stratigraphic classification and correlation of feixianguan formation in lower triassic, the rock fexture characteristics, type and forming conditions of rock ; determining dirtributary law of the sedimentary facies in vertical and horizontal direction and distribution in plane and the essetial contronling factors through correlation of sedimentary facies transverse profile and regionnal geologic characteristics ; establishing plane stereoscopic modle of sedimentary of oolitics beach by studying diagenesis

    主要內容包括：對川西北地區下三疊統飛仙關組地層進行了劃分與對比，研究了飛仙關組地層的巖石結構組分特徵、類型和形成條件；通過沉積相橫向剖面的對比，並結合區域地質特徵，深入研究了沉積相在縱、橫向上的變化規律，確定了沉積相在平面上的分佈及主要控制因素，分析了沉積相的縱向演化過程和建立了沉積相的平面立體模式；詳細研究了該套地層所經歷的成巖作用類型、特徵及對儲集空間的影響，建立了鮞粒灘相儲層的形成與演化模式；最後，從沉積相、成巖作用的角度，分析了區內飛仙關組地層的生油潛力、儲層的分佈規律和發育區塊。
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