swamp lake 中文意思是什麼
swamp lake
解釋
沼澤湖-
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。 -
The time corresponding to the four parts along the section are as follows : the top lake - swamp sediments : holocene ; the uppart fine sand : later late pleistocene ; the middlepart sandy clay : middle - early late pleistocene ; the lowpart clayer silt : later - middle - pleistocene. the fossils and stone artifacts found in salawusu site should be formed during the last but one glacier, its age range is about 0. 13 - 0. 19 ma, and belongs to later middle - pleistocene
分析q曲線與氧同位素曲線的一致性以及以上研究結果，包含薩拉烏蘇地層的這套沉積物的沉積時代為：頂部湖沼相沉積物：全新世；上部具交錯層理的細砂：晚更新世晚期；中部粉砂質粘土：晚更新世中期至早期；下部粘土質粉砂：中更新世晚期。 -
And the delta genetic unit includes distributary channel, distributary bay, small lake of delta plain, swamp, distributary estuary bar, frontal delta mud and sandy density flow and so on. the fluvial system is composed of channel, channel side and flooding basin
其成因相包括分流河道、決口扇及決口河道、分流間灣、三角洲平原小型湖、沼澤、分流河口壩、前三角洲泥及砂質重力流等；該區河流體系由河道、河道邊部及泛濫盆地等沉積組合構成。 -
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。 -
Three sets of source rocks had been formed juring the steady sinking of the basin. the first source rock, being clay and calcium clay stone in tiemulike formation of permian was formed in deep lake environment ; the second source rock, being clay stone in xiaoquangou group of middle to upper triassic was formed in the offshore and the shallow lake environment ; and the third source rock, being coal beds in badaowan formation of lower jurassic was formed in the lake - swamp environment. the first one is the most potential, since it has the biggest thickness, the highest organic matter abundance, high maturity and the highest hydrogen generating capacity
在盆地穩定沉降時期，相應地形成三套烴源巖，即上二疊統鐵木里克組（ p _ （ 2t ） ）深湖、半深湖相泥巖、泥灰巖；中上三疊統小泉溝群（ t _ （ 2 - 3xq ） ）濱淺湖相泥巖及下侏羅統八道灣組（ j _ （ 1b ） ）湖沼相煤系地層。 -
Xin yu business - guang tian hotel is a star grade standard hotel. it is a multifunction commercial hotel with accommodation, repast and leisure. the hotel is located in north of the city, offering the best geographical position and convenient transportation. about ten minutes to the hangzhou north bus station and six kms to the west lake beauty spot and xixi swamp spot. it costs assets more than twenty millions. the hotel is elegantly furnished decoration and mixes with modern and classical styles
新宇商務廣田酒店是一家按星級標準建造，集住宿餐飲休閑於一體的多功能商務酒店。地處市區城北，距杭州汽車北站10分鐘路程，離西湖風景區和西溪濕地景區約6公里，地理位置優越，交通十分便利。酒店耗資兩千多萬元，裝飾華麗典雅，融現代與古典風格於一體。 -
The westward re - construction of the west lake will protect the environment while opening an ecological swamp area and adding a new highlight to tourist resorts in hangzhou
以綜合保護為宗旨的西湖西進工程，將構造江南濕地生態、創造山水有機融合，為杭州的山水城市和風景旅遊增添一大亮點。 -
And the fluvial genetic unit includes point bar, the bottom of channel, bursted fan, bursted channel, natural bank, over - bank deposits, small lake of flooding plain and swamp and so on
成因相包括點壩、河道底部沉積、決口扇及決口河道、天然堤及越岸沉積、泛濫平原小型湖及沼澤等。
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