集巖 的英文怎麼說

中文拼音 [jíyán]
集巖 英文
agglomerate
  • 集 : gatherassemblecollect
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  1. The basins in west china were downfaulted depression basins in jurassic and cretaceous, and foreland basins in cenozoic. these basins formed not only marine facies source rocks ( oil type ) and reservoirs but also continental facies source rocks ( coal type and oil type ) and reservoirs

    因此，中國類前陸盆地基本石油地質條件與國外富油氣前陸盆地相比，除海相烴源巖的質量不及後者外，其它方面並無明顯不足，且具有發育陸相烴源巖和儲集巖的優勢。
  2. The mafic dikes also formed by the partial melting of enriched mantle, include gabbro, diabase ( distributing mainly in luxi ) and lamprophyres ( camptovogesite, odinite and hornblende lamprophyres ) ( mainly in ludong ). for all the rocks, crustal contamination was absent when magma emplaced. 2

    基性脈巖主要包括輝長巖、輝綠巖（主要分佈在魯西地區）和煌斑巖（以斜閃煌斑巖為主，同時含部分拉輝煌斑巖和角閃煌斑巖） （主要分佈在魯東地區） ，都為富集巖石圈地幔部分熔融的產物。
  3. The astronaut can send out a robot which will work on the unknown plant, collecting rocks and minerals, putting up a permanent observation station or traveling far and wide

    宇航員可以派出機器人在這顆陌生的行星上工作，收集巖石和礦物；建立永久性觀察站，或向四面八方走動。
  4. Many young rock hounds grow up to be geologists

    許許多多愛好收集巖石的少年，長大后成了地質學家。
  5. And the shaly sandstone is the primary type of hydrocarbon reservoirs now. so it is the completely necessary and very significative task to study permeability of shaly sandstone reservoirs

    並且泥質砂巖儲層是當今石油的主要儲集巖石的類型，因此研究泥質砂巖儲集層的滲透率是十分必要而且非常有意義的工作。
  6. These reservoirs may develop as a result of either structural or stratigraphic causes.

    由於構造或地層方面的原因，這些儲集巖可以進一步發育。
  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、河口砂壩及三角洲平原水上分流河道微相細粒長石砂巖、粉砂巖；儲層巖石經歷了壓實，膠結，溶蝕等成巖作用，歷經早成巖機械壓實和化學壓溶孔隙縮小期、晚成巖a亞期溶蝕作用孔隙擴大期及晚成巖a亞期（ b亞期）膠結充填孔隙縮小期三個成巖-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，儲集巖排驅壓力和中值壓力較高，孔隙結構類型以細小孔-微孔隙，微細喉-微喉型為主。
  8. The rock types comprise the delta front subfacies subaqueous distributary channel, channel - mouth bar and distal bar microfacies, and delta plain subfacies subaerial distributary channel microfacies sandstones and siltstones. as for the reservoir quality, the subaqueous ( subaerial ) distributary microfacies channel sandstones are the first, the channel - mouth bar microfacies sandstones come second, the distal bar microfacies sandstones is the third, and the last one is the interdistributary bay microfacies sandstones. the intense compaction, pressure solution and late carbonate cementation are responsible for the reduction of the porosity and permeability of the reservoir rocks

    三角洲前緣水下分流河道、河口砂壩、遠砂壩及三角洲平原水上分流河道微相決定了儲集巖的發育，分佈及原始物性條件；水下（上）分流河道微相砂體厚度大、物性和孔隙結構好，次之為河口砂壩微相砂體，遠砂壩微相砂體儲集性較差，而分流伺灣微相砂體物性和孔隙結構最差。
  9. The reservoirs, which are more fractured and cataclasm, are mainly distributed in fracture belt or near it. that is, the distribution of metamorphite reservoirs is influenced by the structural fracture belts

    裂縫發育?碎裂化強烈的儲集巖主要分佈在斷裂帶及其附近，即構造斷裂帶控制著變質巖儲層的形成發育和分佈。
  10. Based on the analysis of thin sections by microscope, measurement of porosity and density, and geological setting, we tested the rock physical parameters of sandstone, siltstone, carbonate and other transitional sedimentary rocks by the mts system under formation conditions ( temperatures, pressures and pore fluid properties ). the rocks we tested are from tertiary ( including zhujiang formation, zhuhai formation, enping formation, hanjiang formation ) of zhujiangkou basin in southern china sea. according to the analysis results, we studied the main ultrasonic wave velocity characters of rocks, which are compressive and shear wave velocity and poisson ' s ratio under different formation conditions

    在對珠江口盆地第三系儲集巖進行顯微鏡薄片分析、孔隙度和密度分析，以及地質背景分析的基礎上，利用巖石物理參數測試系統（ mts ）模擬地層條件（溫度、壓力和孔隙流體狀況）測試了珠江口盆地第三系（包括珠江組、珠海組、恩平組、韓江組，以下有關討論同）砂巖、粉砂巖、碳酸鹽巖及其過渡性巖石物理性質，重點研究了不同地層條件下巖石的聲學特徵（巖石的縱橫波速度和泊松比） 。
  11. The mainly reservoirs in the middle of damintun depression of liaohe basin are the regional metamorphic rocks and the migmatites, which are more fractured and rigid by the cataclastics. the space of metamorphite is the mainly fractures, which are produced by the tectogenesis and the physical weathering

    2 、遼河大民屯中部地區主要儲集巖是太古界的區域變質巖和混合巖類，尤以裂縫發育和經過碎裂化的剛性變質巖類的儲集性能最佳。
  12. We suggest that the favorable reservoir facies within ganchaigou formation in west qaidam basin are delta front facies, fan - delta front facies, dam - and - beach facies of the littoral and shallow lake, lacustrine floor fan facies and carbonates facies

    強調了三角洲相前緣、扇三角洲相前緣、濱淺湖灘壩、湖底扇以及碳酸鹽巖沉積是西部地區乾柴溝組有利的儲集巖相帶。
  13. 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。
  14. Reservoir rock characteristics of yakela - luntai belt in talimu basin

    輪區帶儲集巖特徵
  15. It shows that oil and gas moves from source rock to reservoir rock in continuous phase

    研究認為，油氣是以連續相的形式從源巖運移到儲集巖的。
  16. 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。
  17. The conditions of source rocks, reservoir rocks, and cap rocks are favorable in the southern segment of western sag of liaohe oilfield, where several favorable reservoir - cap rock associations come into being

    摘要遼河西部凹陷南段烴源巖、儲集巖和蓋層條件十分優越，形成多套有利的儲蓋組合。
  18. In the eastern part, the paleogene infilling in the rift structure has been altered by compression and also became important reservoir rocks

    在南沙東北部充填在裂谷中的下第三系受到不同程度的積壓，是重要的儲集巖層。
  19. Visitors can manipulate the operational components of a scale model telecommunications satellite and utilize a robotic arm to fetch rock samples from a simulated martian terrain

    觀眾亦可調校通訊衛星模型的位置，領悟衛星通訊的原理或利用機械臂在模擬的火星表面上採集巖石樣本。
  20. The low - ti series show variable degrees of nb - ta depletion in primitive mantle - normalized spidergrams with slightly enriched to depleted nd isotopic compositions, whereas the transitional series exhibit similar geochemical features to emii - oib and have transitional characteristics between the high - ti and low - ti rocks. all three groups show no continuous shift in major and trace elements and cannot be regarded as different phases during magma differentiation process. on the basis of normalization to mgo = 8 %, the high - ti diabases have the lowest sig, nag and highest tig and peg

    通過詳細的巖石學和元素-同位素地球化學研究，這些巖石具有各自不同的地球化學特徵，其中高ti系列的低la nb 、 zr nb比值和虧損的nd同位素組成顯示其類似於oib的特徵，過渡ti系列則顯示出emii - oib的特徵，而低ti系列則高la nb 、 zr nb比值和變化的nd同位素組成顯示出一定比例的富集巖石圈地幔或地殼物質的參與。
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