洞穴沉積 的英文怎麼說

中文拼音 [dòngxuéchén]
洞穴沉積 英文
cave deposits
  • : 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
  • : 名詞1 (巖洞; 窟窿) cave; cavern; grotto 2 (動物的窩) den; hole 3 (墓穴) grave4 [中醫] (穴...
  • : Ⅰ動詞1 (沉沒; 墜落) sink 2 (沉下 多指抽象事物) keep down; lower 3 [方言] (停止) rest Ⅱ形容...
  • : Ⅰ動詞(積累) amass; store up; accumulate Ⅱ形容詞(長時間積累下來的) long standing; long pending...
  • 洞穴 : cave; cavern; abri; grotto; weem; [德國] senke; pocket
  • 沉積 : [地] deposit; sedimentation; deposition; precipitation
  1. There are three genetic types of mineral deposits in the beiya ore district : cu - au polymetallic deposits related to alkaline porphyries, comprising porphyritic cu - au deposits and polymetallic skarn deposits related to quartz - albite porphyry and quartz - k - feldspar porphyry ; fe - au deposits related to gabbro or basalt magma, consisting of magmatic fe - au deposits and sedimentary polymetallic deposits formed in caves and lakes ; and palaeo - placers formed at the weathering surface, in lakes and in karsts

    北衙金礦有3種成因不同的礦床:與堿性斑巖有關的銅金多金屬礦,包括與石英鈉長斑巖和石英正長斑巖有關的斑巖型銅金礦床和矽卡巖型多金屬礦床;與輝長玄武巖漿有關的鐵金礦床,包括熔漿型鐵金礦床和噴流型多金屬礦床,後者又有和湖相環境之分;及古砂礦,有古風化殼型砂礦、河湖相古砂礦和洞穴沉積古砂礦。
  2. There are things like burrows in some of the sediments found in layers above ( after ) the impact ejecta which can ' t easily be mimicked by a flood and imply many organisms survived the meteor impact to die off about 300, 000 years later

    在一些沖擊物中有類似的東西存在於沖澱物的層面內,暗示了很多生物體經歷流水影響之後倖存到大約30萬年以後才消失。
  3. Morphological accumulation of karst cave and landform development in guizhou

    巖溶形態與貴州地貌發育
  4. And 14 species associated with tufa deposition at cave entrance, 4 travertine types of bryophytes can be distinguished : stalacitite, travertine on cave wall, floor seepage, droping - water travertine

    14種苔蘚植物參與了口鈣華形態包括鐘乳石、壁鈣華、底泉華和底滴水鈣華4種類型。
  5. The entering of the tourist and lamp - light gave much energy to furong cave and the temperature in the cave rised slowly. the different temperature between the outer and the inner as the air circulation, would make the cave wet seriously in the summer and dry in the winter. the density of co2 would go up because of piston - effect, cave depositing and the tourists " entering

    遊人的進入和燈光的使用,給芙蓉內帶來了大量的能量,致使空氣升溫;由於動內外的溫度差和空氣的流通,開放的出現夏季高濕,冬季乾燥的變化現象; co _ 2的濃度會因為活塞效應、洞穴沉積和遊人的進入而升高,但影響最大的還是遊人,當遊客量較大的時候,co _ 2的濃度會隨遊人進入的數量增加而明顯升高,內co _ 2含量峰值記錄最高出現了6200ppm的記錄。
  6. On the base of summarizing and evaluating chinese soil erosion models, this paper brings forward future developing directions that the soil erosion models should pay attention to : ( 1 ) paying attention to the theory researches of soil erosion models, consummating from erosion factors basis erosion prediction to erosion processes quantity and theory researches, studying each erosion factor and its interaction impact on erosion processes, and sediment dispersion, transportation and deposition action on complex slopeland, as well as different catchments scales ; ( 2 ) reinforcing the study of gravitation erosion and cave erosion mechanism, and big and middle scale catchments erosion models ; and ( 3 ) making the best of advanced rs and gis technology, providing plentiful datum for erosion models researches, making and for soil erosion models checkout

    在總結和評價中國土壤侵蝕模型的基礎上,提出了今後土壤侵蝕模型應該注重的發展方向: ( 1 )注重土壤侵蝕模型的理論研究,將從以侵蝕因子為基礎的侵蝕預報向侵蝕過程的量化研究和理論完善,研究各侵蝕因子及其交互作用對侵蝕過程的影響,泥沙在復雜坡面以及不同流域尺度間的分散、輸移和作用; ( 2 )加強對重力侵蝕、侵蝕機制的研究,加強對大中流域侵蝕模型的研究; ( 3 )充分利用先進的rs 、 gis技術,為侵蝕模型的研究提供大量的數據源,以利於對土壤侵蝕模型的檢驗。
  7. 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,即地表相爆發作用形成的凝灰角礫巖、熱水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。
  8. It is revealed through studying the environmental geochemical behavirous of phosphorus that the sedimentary phosphorus in sea - continental margin recorded the paleoclimatic and paleoenvironmental changes information and its critical significance of indicating past - global changes

    綜合這些研究成果,有關不同時間尺度的古氣候變化的信息主要是通過對冰芯1 3 、黃土4 、 5 、海底6 、 7 、湖物8 、樹木年輪9 、碳酸鹽10 ,以及生物遺跡11等的研究獲得的。
  9. The waters flowing over the limestone and chalk have, over thousands of years, deposited travertine barriers, creating natural dams which in turn have created a series of beautiful lakes, caves and waterfalls

    數千年來流經石灰石和白堊上的水,逐漸為石灰華屏障,構成自然的堤壩,後者又創造了一系列美麗的湖泊、和瀑布。
  10. The lefthand photo shows a classic gypsum rope formation, from a cave in the grand canyon. the righthand photo shows a more cotton - like example from a cave in tennessee

    左邊圖片顯示的是一個典型的繩狀石膏,來自大峽谷的一個。右邊的圖片是田納西一個內的棉紗狀的物樣品。
  11. The tourism resource of caves is a kind of special perspective resources under the earth. the deposit of caco3 is the main appreciating perspective in fu rong cave

    旅遊資源是一類位於地下的特殊景觀資源,巖溶中次生碳酸鈣( caco _ 3 )物是芙蓉主要觀賞景觀,它抗干擾能力較弱。
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