細砂巖 的英文怎麼說

中文拼音 [shāyán]
細砂巖 英文
fine sand block
  • : 形容詞1 (條狀物橫剖面小) thin; slender 2 (顆粒小) in small particles; fine 3 (音量小) thin ...
  • : 名詞(沙子) sand; grit
  • : 名詞1. (巖石) rock 2. (巖峰) cliff; crag
  1. According to rock and mineral analysis, the formation consists dominantly of detrital feldspathic fine - sandstone with medium and silt sandstone secondly. lithologically, the content quartz is lower than those of feldspar and detritus, and the cement is dominated by clay, which gives the feature of low compositional maturity and low textural maturity

    館上段儲層性以屑質長石細砂巖為主,其次為中細砂巖和粉石中石英含量低,而長石、屑含量高,膠結物以泥質為主,表現出低成分成熟度和低結構成熟度的特點。
  2. After analyzing of the whole situation, granularity is smaller. the lithology of chang 6 oil - bearing is a set of felspar sandstone. little of them are rock - scraps felspar sandstone

    通過研究發現延長組6段儲層為一套中?粒長石及少量粉,油層組遠離物源區,成分單一,表明其物源穩定。
  3. The investigation of a lot of parameters about treated sandstone, brick materials and earthen materials with fluorited polymers has been carried out, such as the formation of polymer, the penetration depth, porosity, capillary absorption and penetration coefficient, water uptake, compressive strength, drilling resistance, absorption isotherms of water vapor, water vapor diffusion, color changes as well as resistance to desegregation of water, frizzing - throwing cycles, worming - cooling cycles, and so on. in addition, the influence of salt crystallization, acid and base, and uv aging have also been assessed in order to better understand the protection effects and utilization possibility of two fluorinated polymers, mainly according to astm standard and the combination of international methods together with general technological

    分別以國家級文物保護單位的土質、和磚材文物樣品為對象,依據astm標準及國際通用文物保護研究方法與評估準則相結合,通過膠化物形成周期、滲透深度、孔隙度、毛吸水和滲透系數、持水量、抗壓強度、抗鉆強度、吸附水蒸氣的能力、透氣性、外觀顏色等系列參數的測定,及凍融、冷熱循環、酸堿腐蝕后抗壓強度的衰減、可溶鹽對保護效果的影響、酸堿及光照對表面保護效果的影響,對兩種含氟聚合物及其與有機硅的共混物在文物加固保護和表面防護中的可行性和保護效果給予了系統研究。
  4. The dominant storage space is the solution micropores, the honeycomb - like solution pores and the kaolinitic intercrystalline pores. the pore throat is small to very small. the main characteristics of the reservoirs are low porosity and low permeability

    的儲集空間以粒內溶孔、粒間溶孔、高嶺石晶間隙等次生微孔隙為主,具有孔徑小喉道的特點。
  5. Ping chau is made up of finely layered siltstone and mudstone

    平洲由小的粉及泥組成。
  6. So although there are better oiliness in peng ii, peng iii, peng iv gas pool and there are industrial off - take potentia after compressive fracture, this gas pool belongs to lower permeability, convention sand - density sand, little to middle throat - punctate pore, sealing elasticity gas drive, partly poor water drive, normal pressure, net gas, lithologic trap to nose - like structure - lithology compounding trap model

    所以,雖然新都氣田蓬萊鎮組蓬二、蓬三、蓬四段有良好的含油氣性,且經過測試均獲得工業產能。但總體上該氣藏隸屬低滲常規?緻密,小及中喉?孔孔隙型,定容封閉彈性氣驅,部分弱水驅,常壓,干氣,性圈閉及鼻狀構造?性復合型圈閉氣藏類型。
  7. The variations in trace element contents and ratios may hold up a mirror to the lake - level fluctuations and climatic changes, which, in turn, have exerted a direct and important effect on the sequence stratigraphic development. collectively, the reservoir rocks from the yanchang formation consist dominantly of the delta front subfacies subaqueous distributary channel and channel - mouth bar microfacies and delta plain subfacies subaerial distributary channel microfacies fine - grained feldspar sandstones and siltstones. the reservoir rocks have been subjected to three stages of diagenetic and porosity evolution : ( 1 ) the porosity reduction by the mechanical compaction and chemical pressure solution during the early diagenetic stage ; ( 2 ) the porosity increase by the dissolution during the a substage of the late diagenetic stage, and ( 3 ) the porosity reduction by the cementation and filling during the b substage of the late diagenetic stage

    系統的儲層特徵研究表明,該區延長組儲層成因類型主要為三角洲前緣水下分流河道、河口壩及三角洲平原水上分流河道微相粒長石、粉;儲層石經歷了壓實,膠結,溶蝕等成作用,歷經早成機械壓實和化學壓溶孔隙縮小期、晚成a亞期溶蝕作用孔隙擴大期及晚成a亞期( b亞期)膠結充填孔隙縮小期三個成-孔隙演化階段;儲層物性總體上具有較低孔滲、低孔滲的特點,孔隙類型主要為粒間溶孔、殘余粒間孔隙、粒內溶孔、晶間孔及晶間溶孔,裂縫不發育,儲集排驅壓力和中值壓力較高,孔隙結構類型以小孔-微孔隙,微喉-微喉型為主。
  8. Grain gradation, from coarser below to finer above in repeated, truncated sequences within the ellerslie sandstone is also evident.

    在埃勒斯萊層段內,重復出現的截頂層序中,自下而上,由粗變的粒級遞變也是明顯的。
  9. Directed by new theories and approaches of sedimentology, diagenesis and reservoir evaluation, focused on marine clastic reservoir of donghe sandstone member, in tarim basin, strata and depositional system of donghe sandstone member are classified ; typical depositional facies types, depositional model and horizontal distribution have been studied through depositional facies analysis of 17 single wells, combined with seismic data. major diagenetic events, stages and " four history " collaboration have been systematically analysesed, furthermore, the relation between reservoir diagenesis and porosity evolution has been built ; thorough studies on reservoir lithology, physical property and pore structure, reservoir development related to depositional envoironment, diagenesis and tectonic has been discussed ; reservoir has been evaluated and predicted by five influential parameters drawn from the results of the study on depositional facies, diagenesis and reservoir characteristic. in the end, favourable reservoir body distribution has been pointed out

    本論文以沉積學、沉積石學、沉積成作用與儲層地質學、儲層評價技術的新理論新方法為指導,以塔里木盆地巴楚組東河段海相碎屑儲層為主要研究對象,通過17口典型井的單井地層沉積相分析和成作用分析,結合地震資料,對東河段地層和沉積體系進行了詳劃分,研究了東河段分佈區的典型沉積相類型、沉積模式及其平面展布特徵;系統分析了東河段碎屑儲層的主要成事件、成期次及其四史配置關系,指出了儲層成與孔隙演化的關系;深入研究了東河段碎屑儲層的石學特徵、物性分佈、孔隙結構等特徵,著重討論研究了沉積環境、成作用和構造作用對儲層發育的影響;運用「權重」評價法結合地層沉積相、成演化和儲層特徵研究的結果,選取了五個對儲層發育有重要影響的參數對儲層進行了整體的評價和預測,指出了塔里木盆地東河段儲層有利儲集體的分佈狀況。
  10. The dark - gray traction current deposits belong to internal - tide deposits, it develops sandstones and siltsands, and charactered with lenticular, wave, flaser bedding, bimodal cross - bedding and ripple mark

    深水牽引流沉積為內潮汐沉積類型,性為細砂巖、粉,以發育透鏡狀、波狀、脈狀層理、雙向交錯層理、波痕等沉積構造為特徵。
  11. 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、韻律性薄互層型和鮞粒灰型。
  12. Beneath the relic sand of the outer shelf there is high grade of valuable heavy mineral sand ( for example ilmenite ) reaching the ii anomaly order of marine placers and it is of potential resource prospects

    通過碎屑礦物判斷,原應是中酸性漿和淺變質類。鈦鐵礦等有用礦物在層位中出現較厚的礦異常,顯示一定的淺海礦資源潛力。
  13. The test results show that the drawing interval of 1. 5 m is helpful for controlling dead - unconsolidated thin sandstone of coal seam roof and reduce sand ratio of drawn top - coal

    試驗結果表明,放煤步距採用三采一放有利於控制頂板極鬆散細砂巖,降低放出頂煤的含率。
  14. The thermal cracking threshold of fine sandstone is determined primarily

    實驗初步確定了細砂巖的熱破裂閾值及其熱破裂規律。
  15. Fine - grained feldspar sandstone is the main oil - bearing rock and chlorite is the dominant kind of clay minerals

    研究結果表明,長2油藏含油粒長石為主,粘土礦物中綠泥石含量較高。
  16. Study on triaxial meso - failure mechanism and damage variables of sandstone under chemical erosion

    化學腐蝕下三軸觀損傷機理及損傷變量分析
  17. Thus it became well - known for frequent geologic - disaster and landslide in the stratum area. xigeda soft rock is made up from minute sandstone, mud siltstone, siltstone mud and mudstone. it is inland fluviolacustrine phase deposit rock with rhythm - cyclic character of depositional geology

    昔格達組極軟屬內陸靜水河湖相沉積,主要由粉細砂巖、泥質粉、粉質泥和泥組成,具有明顯的沉積韻律特徵。
  18. Fracture development and strain field around the stress induced crack area in sandstone

    細砂巖裂紋周圍變形破壞過程及應變場分佈
  19. The oil - bearing content of oilsand is close to rock lithology, and therefore high oil content occur mainly in fine - grained sandstone and fine - median grained sandstone

    含油性與性關系密切,含油率較高的油性主要是細砂巖、中細砂巖
  20. In order to optimize the parameters of running top coal under different coal and gangue fragmental size, on the basis of measuring and analyzing the distribution character of top - coal fragmental size, running top coal was studied for the coal seam with dead - unconsolidated thin sandstone roof by loose medium model experiment

    摘要為了優化不同煤矸塊度條件下的放煤工藝參數,在實測分析頂煤破斷塊度分佈特點的基礎上,採用散體模型試驗的方法對煤層頂板為極鬆散細砂巖條件下的放煤工藝進行了研究。
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