灰巖洞 的英文怎麼說

中文拼音 [huīyándòng]
灰巖洞 英文
limestone cave
  • 灰 : Ⅰ名詞1 （物質燃燒后剩下的粉末狀的東西） ash 2 （塵土; 某些粉末狀的東西） dust 3 （特指石灰） lime...
  • 巖 : 名詞1. （巖石） rock 2. （巖峰） cliff; crag
  • 洞 : Ⅰ名詞（物體上穿通的或凹入較深的部分; 窟窿; 洞穴） hole; cavity Ⅱ形容詞（深遠; 透徹） profound; thorough; clear
  1. Southwest is palawan, the country s last frontier with the forbidding limestone cliffs of el nido, the subterranean caverns and river of st. paul, the safari island of calauit, home to giraffes, impalas and zebras, and tubbataha reef, the most beautiful dive site this side of the world and recently declared a protected marine area

    El nido有石灰巖懸崖絕壁、地下大巖洞和地下河聖保羅河。 calauit島野生動物園棲息著長頸鹿、黑斑羚和斑馬。還有世界上最美麗的的潛水勝地tubbataha暗礁，最近被宣布為海洋保護區。
  2. Mammoth cave national park, located in the state of kentucky, has the world ' s largest network of natural caves and underground passageways, which are characteristic examples of limestone formations

    猛瑪洞穴國家公園位於肯塔基州，是世界上最大的自然洞穴群和地下長廊，也是石灰巖地貌構成的典型代表。
  3. Limestone and dolomite cover about 130 km2 which takes up about 1 / 7 areas of the national land in china. besides, it is pluviose, muggy and damp in there areas, all of these accelerate the karst caves. there are more than 100, 000 caves and holes under the earth, which consists of a karst caves kingdom in the world

    中國石灰巖和白雲巖的出露面積約為130km2 ，約佔全國總面積的1 7 ，加之雨量充沛，氣候溫熱潮濕，喀斯特較為發育，地下洞穴孔道，計有數十萬個之多，成為世界上的洞穴王國。
  4. Cenotes are created when limestone in the cave system erodes and the roof collpases, forming a water - filled sinkhole

    當洞穴系統內的石灰巖發生腐蝕而且頂部開始下沉的時候，就形成了盛滿湖水或河水的灰巖坑。
  5. A natural limestone bridge with lofty body and natural stone fences lies 10 km away from the east of shangri - la county, across which the shuodugang river is flushing from east to west through the underground cave

    處有一座天然石灰巖橋梁，故名天生橋，橋體巍峨，橋面上有天然石欄。自東向西奔流的碩都崗河，在此穿越地下溶洞，石橋形如
  6. The hydrothermal breccia and karst in the beiya area are divided into 4 types and zones, including : sedimentary tuff and breccia induced by hydrothermal explosion and sedimentation on land surface ; hydrothermal sedimentary conglomerate and gas - explosive ejecting breccia related to sedimentation in and collapsing of some shallow karst caves ; netted hydotherma1 limcstone breccia and hydrothermal explosive breccia pipe related to hydrofracturing, corrosion and explosion in the hydrothermal channels ; and yellow granular limestone formed by simmering and alteration in the deep heated water reservoir

    北衙地區熱水角礫巖和熱水巖溶可分為4種類型和層次，即地表相爆發沉積作用形成的沉積凝灰角礫巖、熱水沉積鮞狀灰巖與鈣華膠結角礫巖；與近地表洞穴沉積和垮塌作用有關的熱水沉積礫巖和汽爆射流角礫巖；與熱水通道相蝕裂和爆破角礫化作用有關的網路狀灰巖角礫巖筒和熱水隱爆角礫巖筒；深部相熱水浸煮蝕變灰巖。
  7. The favorable reservoir spaces in the carbonate rock could be divided into five types according to their origin, configuration and size, i. e., solution fissure, solution hole, cave, erosional fissure and structural fissure, which form five different reservoirs including cave - type reservoir, erosional fracture reservoir, structural fissure reservoir, and solution pore marginal beach grainstone reservoir

    而下奧陶統灰巖段儲集和生產油氣的有效儲滲空間按成因、形態及大小可劃分為溶蝕孔隙、溶蝕孔洞、大型洞穴、風化裂隙、構造裂隙等5類，構成5種性質有別的儲層，即洞穴型儲層、風化裂隙型儲層、構造裂隙型儲層、臺緣灘相顆粒灰巖溶蝕孔隙型儲層和地表殘積物裂隙孔隙（洞）型儲層。
  8. Perhaps you have seen colorful limestone cave and underground river, but the eighteen caves here are mesozoic lava land forms, which is produced by the movement, cracking and weathering of the earth ' s crust

    或許你見過絢麗多彩的石灰熔洞和地下暗河，但在這里的十八個山洞卻是中生代火山巖地貌，由於地殼運動斷裂風化形成的。
  9. Natural limestone caves are very spectacular

    天然的石灰巖洞是非常壯觀的。
  10. In the southeastern mountainside of the spring dawn in the dhyana woods, there is a lime rock cave, which is 3 meters high, 12 meters deep and 3 meters wide

    在禪林春曉東南側山腰，為一組石灰巖溶洞。洞高3米，深12米，寬3米。由外至內天然形成三進門戶洞室。
  11. Its huge variety of spectacular caves and bizarre rock formations was formed as a result of underground water erosion

    ：飛來峰毗鄰靈隱寺，由石灰巖構成，由於長期受地下水侵蝕，形成了許多奇幻多變的洞穴和怪石。
  12. The hydrothermal limestone breccia sheet presented over tertiary fluvial, lacustrive sandstone and mud in the wandongshan - wulipai area is a hydrothermal breccia landslide from the chenjiazhuang breccia pipe, and it may be a domain origin which would have obstructed the jinshajiang old channel and made the jinshajiang river to change and to form the famous valley and turns

    萬洞山五里排帶呈席狀覆蓋于第三系河湖相的砂礫巖和粘土沉積之上的灰巖質熱水角礫巖為一套從陳家莊角礫巖筒滑覆過來的熱水角礫巖滑體，其可能是造成金沙江古河道淤塞並使古金沙江改道和形成大拐彎的主要原因。
  13. Observation of drilling cores and casting - sections and the characters of pore structures and permeability of the matrix of the lower - ordovician carbonate in comparing with the lower limit of a reservoir for matrix reveal that the porosity, permeability, maximum pore diameter, saturation and median throat diameter in the matrix with undeveloped fissures, holes and solution pores are far lower than those of a reservoir limit although some micro - pores are developed in the matrix which therefore has no capacity of storing and producing oil - gas

    摘要通過鉆井巖心和鑄體薄片觀察，根據下奧陶統灰巖基質的孔滲特徵和孔隙結構特徵，並與基質作為儲層的下限對照裂隙、洞穴和溶蝕孔洞不發育的灰巖基質，發現盡管有微孔隙的發育，但其孔隙度、滲透率、最大孔喉半徑、飽和度、中值喉道半徑等參數值遠低於儲層下限值，基本不具備儲集和生產油氣的意義。
  14. The carbonate reservoir rock includes many influence factors that it is through many phases structure bursts and the ancient karst to act on jointly the formation and with which the rock karst gives first place. the complicated oil field of karst cave and crack are controlled by limestone reservoir and the crevices - cave system, which have many characteristics such as vivid and great in style, irregular distribution, the limestone cave in crack and unhomogeneity of rock etc. these kinds of reservoir belong to a world difficult and extreme problem on valuation and cognition

    它是經多期構造破裂與古風化巖溶共同作用形成的、以灰巖巖溶為主控因素、以儲集體控藏和縫洞系統控藏為主的溶洞?裂縫型復雜油氣藏，表現為其不規則形態和不均勻分佈、裂縫溶洞發育不均一、儲層非均質性極強等特點，認識和評價該類儲層屬世界性難題。
  15. The ziwei cave, including the underground river and dry passags, it developes in the lower permian qixia limestone

    摘要紫微洞發育在早二疊系棲霞組的石灰巖中，是一個干洞與地下河相結合的洞穴。
  16. In and around the town are 175 hectare botanical garden, pwe kauk and a ni - sakhan waterfalls, gokhteik viaduct and peik chin myaung caves limestone caves

    市裡和周邊分佈著一百七十五公頃的植物園，比考大瀑布和阿尼斯堪大瀑布，固泰橋和倍欽苗溶洞（石灰巖溶洞） 。
  17. Pindaya is about 45 km drive from kalaw which is 660 km from yangon. it is well - known for its extensive limestone caves, pindaya cave set deep in the hillsides

    -從距仰光市六百六十公里的克洛驅車四十五公里即可到達彬德雅，這里以深藏於山體中結構復雜的石灰巖彬德雅溶洞聞名。
  18. Abstract : this paper, giving the case history of two large - s ized docks built on complex limestones with cavities, grooves, troughsond develo ped fissures in dalian area, presents the construction techniques adopted in the construction of the docks and makes analyses and co mparison between the advantages and disadvantages of the techniques

    文摘:本文通過同在大連地區溶洞、溶溝、溶槽和裂隙發育的復雜石灰巖地質條件下所建造的兩座大型船塢的實例，介紹了所採用的不同的施工工藝，並對其優缺點進行了相對的分析和比較。
  19. D. the last day baojing gong it is a natural limestone cave which was divided into four layers with different temperatures

    寶晶宮是一個天然的石灰巖巖洞，分為四層，每一層的溫度都不一樣，非常特別。
  20. Induced porosity is typified by fracture development as found in some shales and limestones and by the rugs or solution cavities commonly found in limestones

    次生孔隙度是以某些頁巖和石灰巖的裂縫和石灰巖中的巖穴和溶洞為代表。
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