淺鹽湖 的英文怎麼說

中文拼音 [jiānyánhú]
淺鹽湖 英文
schott
  • 淺 : 形容詞1 （從上到下或從外到里的距離小） shallow 2 （淺顯） simple; easy 3 （淺薄） superficial 4 ...
  • 鹽 : 名詞1. （食鹽; 鹽類） salt 2. （姓氏） a surname
  • 湖 : 名詞1 （被陸地圍著的大片積水） lake 2 （指湖州） short for huzhou3 （指湖南、湖北） a name referr...
  1. The lacustrine carbonate rocks in the wudaoliang group consist of boundstone ( stromatolite ), micritic limestone, grainstone and micritic dolostone which were laid down in the shallow - water to bathyal, high - salinity and enclosed to semi - enclosed lake systems

    五道梁群湖相碳酸鹽巖分為生物粘結灰巖（疊層石） 、泥晶灰巖、顆粒灰巖與泥晶白雲巖四大類，反映出沉積環境為一個具有淺水半深水、高鹽度、半封閉封閉特點的綜合湖泊系統。
  2. These geomorphic units of paleogeography constitute the basic model of paleocontinent, littoral - neritic sea and carbonate plateform at that stage, and this depositional model is similar to the pattern of the east china continent and ocean, which is the result of evolution during the past long geologic age

    這些古地理地貌單元構成了湖北省泥盆紀時期古陸濱淺海和碳酸鹽巖臺地的基本沉積模式，這種沉積模式與現今中國東海大陸、海洋格局基本一致，亦是經過了漫長地質歷史時期演化，而形成現今這種格局的。
  3. The coqen basin in xizang lies between the bangong - nujiang suture zone and yarlung zangbo suture zone, and once extended northwards and southwards, respectively centred by the qiekan - goicang - asog rift zone as the center of deposition and subsidence during the middle jurassic to the early creatceous. ( 1 ) during the middle - late jurassic, the rift zone was occupied by deep - water turbidites, radiolarian siliceous rocks, shallow - water carbonate rocks, clastic rocks and basic - ultrabasic rocks, while both sides of it by littoral and shallow marine elastic rocks and carbonate rocks

    摘要位於班公湖怒江縫合帶與雅魯藏布江縫合帶之間的措勤盆地，在中侏羅世早白堊世期間具有以且坎古昌阿索裂谷帶為沉積、沉降中心向南北兩側展開的古地理格局：中晚侏羅世時期，裂谷帶內由深水濁積巖、放射蟲硅質巖和淺水碳酸鹽巖、碎屑巖巖片及基性超基性巖等組成；裂谷帶兩側由濱淺海相碎屑巖和碳酸鹽巖組成。
  4. The main sedimentary facies of the upper carboniferous on the margin of the xuefeng anicient land can be divided into submarine alluvial, foreshore siliciclastic, shallow beach carbonate, carbonate platform and backshore restrict carbonate facies

    摘要湖南沅陵雪峰古陸邊緣上石炭統主要包括下列巖相類型：沖積扇砂礫巖相、前濱海灘砂巖相、淺灘碳酸鹽相及混積巖相、潮下碳酸鹽巖相及灘后局限碳酸鹽巖相。
  5. 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。
  6. Simple introduction of the deep - water crystillization and mechanized harvesting of lake salt

    淺談湖鹽深水結晶和機械化採收
  7. Sedimentary environment in benxi stage from east to west were respectively shallow - sea muddied continental shelf, barrier island, lagoon and tidal flat. most area in taiyuan stage was distributed by shallow - sea continental shelf, but the northern and southeastern part were scattered by clastic tidal flat and carbonate tidal flat. sedimentary environment in shanxi stage, in the middle and late shihezi stage was deltas and lake

    馬5晚期研究區發育蒸發臺地相和局限臺地相；本溪期自東而西發育淺海泥質陸棚、障壁島、瀉湖及潮坪相；太原期大部分地區發育淺海陸棚沉積，北部和西南部則發育碎屑巖潮坪和碳酸鹽潮坪沉積；山西期和石盒子中晚期為三角洲和湖泊沉積環境；石盒子早期廣泛發育辮狀河三角洲和湖泊沉積。
  8. The transitional facies can also be divided as estuarine, tidal flat and lagoon ; the depositional envirnononents of clastic rock marine facies include offshore, shallow water continental shelf, deep water continental shelf, slop as well as the deep water basin ; the carbonate facies can also be divided into a carbonate platform and ramp

    海陸過渡相又分為河口灣、潮坪、瀉湖；海相碎屑巖沉積環境包括濱海、淺水陸棚、深水陸棚、斜坡以及深水盆地；碳酸鹽巖海相又可分為碳酸鹽臺地、碳酸鹽緩坡。
  9. In recently study, much mark of shallow water origin and evaporation are found, so the salt and gypsum rock is considered of evaporation origin in shallow water

    深水相泥巖與淺水成因的鹽巖或膏鹽巖頻繁互層，說明沙三段沉積時期，湖平而變化頻繁。
  10. Furthermore, sixteen sedimentary subfacies are identified. respectively, the sedimentary subfacies are delta plain, delta front, prodelta, braided delta plain, braided delta front, braided prodelta, coastal lake, saucer lake, tidal flat, barrier island, lagoon, carbonate continental shelf, muddy continental shelf, open platform, local platform and evaporate platform

    並進一步識別出16種沉積亞相，分別為：三角洲平原、三角洲前緣、前三角洲、辮狀河三角洲平原、辮狀河三角洲前緣、前辮狀河三角洲、濱湖、淺湖、潮坪、障壁島、瀉湖、碳酸鹽陸棚、泥質陸棚、開闊臺地、局限臺地和蒸發臺地。
  11. Light gray, light yellow gray carbonate rock, clastic rock, a little amount mudstone with the gypsum rock in suonahu formation, regarding carbonate rock as principle

    嗩吶湖組主要發育淺灰色、淺黃灰色碳酸鹽巖、碎屑巖，少量泥巖和石膏巖沉積，以碳酸鹽巖為主。
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