淺沼澤 的英文怎麼說
中文拼音 [jiānzhǎozé]
淺沼澤
英文
banados-
Based on available data, the study on regional structure, sedimentary reservoir and source rock characteristics shows that the basins in south china sea had experienced sedimentary evolution in faulting period and depression period, deposited thick cenozoic formation, upwardly developed alluvial fan facies, river - lake facies coastal swamp facies coastal facies, neritic facies and bathyal deposit system, regionally had 3 source rocks of eocene, oligocene and miocene, 3 reservoirs of pre - cenozoic basement buried bill, oligocene sandstone and miocene reef, with pliocene and pleistocene neritic facies and bathyal shale as regional caprock
摘要以現有資料為基礎，通過對區域構造、沉積儲層、烴源巖特徵等基礎石油地質條件研究，認為南海海域各盆地經歷了斷陷期和坳陷期沉積演化，沉積了巨厚的新生代地層，自下而上發育了沖積扇相、河湖相、濱岸沼澤相、濱海相、淺海相、半深海相沉積體系，區域上存在始新統、漸新統和中新統3套烴源巖，前新生代基巖潛山、漸新統砂巖、中新統生物礁3套儲層，區域蓋層為上新統和更新統淺海半深海相泥巖。Ponds, marshes, mangroves and intertidal areas at estuaries and coastal areas are good examples
魚塘，淡水沼澤森林，紅樹林，河口及淺海區域均是最好的例子。The major types include the natural and artificial wetlands such as swamp wetland, lake wetland, river wetland, estuary wetland, sea - beach wetland, shallow sea area, reservoir, ponds and rice paddy fields
主要類型有沼澤濕地、湖泊濕地、河流濕地、河口濕地、海岸灘塗、淺海水域、水庫、池塘、稻田等天然濕地和人工濕地。According to the definition in ramsar convention, wetlands include marshes, peatlands, wet meadows, lakes, rivers, floodplains, river deltas, tide flats, reservoirs, ponds, rice paddies as well as marine areas with water depths under six meters
按照《濕地公約》定義，沼澤、泥炭地、濕草甸、湖泊、河流、滯蓄洪區、河口三角洲、灘塗、水庫、池塘、水稻田以及低潮時水深淺於6米的海域地帶等均屬于濕地范疇。Wetland refers to natural or artificial, permanent or temporary marshes, peat bog and waters ( motionless or flowing, fresh water or salt water ) including sea area no deep than 6m in low tide
濕地是指天然或人工的、永久或暫時性的沼澤地、泥炭地和水域（有靜止或流動、淡水或鹹水水體） ，包括低潮時水深淺於6米的海水區。Layers of carbonate limestones, silty mudstones, quartz sand and solidified lava show that within the past 600 million years, this area was a warm, shallow sea, then a muddy swamp, then a vast desert of shimmering hot dunes, then a glacial ice sheet, then a shallow sea once again
層層的碳酸石灰巖、粉砂質泥巖、石英砂和凝固的熔巖，顯示在過去六億年間，這個區域曾經是溫暖的淺海，接著依序變成泥濘的沼澤、擁有炙熱沙丘的廣闊沙漠，然後是冰川，后來又再度成為淺海。During the dry season, soil particles and plant matter would have settled slowly to the bottom of the shallow lakes and swamps, eventually forming the blue clays and lignite
乾季時，土壤顆粒及植物緩慢沉澱到淺水湖泊及沼澤底部，最後形成藍色的黏土及褐煤。分享友人