泥沉積帶 的英文怎麼說

中文拼音 [chéndài]
泥沉積帶 英文
mud belt
  • : 泥名詞1 (含水的半固體狀的土) mud; mire 2 (像泥的東西) any paste like matter; mashed vegetable...
  • : 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...
  • 沉積 : [地] deposit; sedimentation; deposition; precipitation
  1. " it could be acidic water, it could be briny water, it could carry lots of sediment or be slushy, but [ it appears that ] water is involved, " edgett added

    「那可能是酸水,可能是鹽水,可能攜有很多物,也可能是濘的,但看上去跟水肯定有關系。 」
  2. Benthic foraminifer fauna, ams14c dating and acoustic sub - bottom profile was analyzed in the core ey02 - 2 and ey02 - 1 drilled from the muddy deposit in the middle southern yellow sea and the mid - shelf of north east china sea. considering the results of core qc2 ? dz4 and the standard oxygen isotope curves, we discussed the late - quaterenary paleo - environment evolution, benthic foraminifer fauna, paleo - climate, the climate events and water mass in postglacial period, average sedimentation rates, paleo - water depth, origin of sediments, average sea level rise rate in the shelf of south yellow sea and east china sea. at last we discussed the condition of sea level rise in the east china, green house effect and the protection of coastal zone

    本文根據南黃海中部質區和東海中陸架的兩個鉆孔巖芯的古生物、 ams ~ ( 14 ) c測年、淺地層剖面等,參考qc _ 2 、 dz _ 4成果及標準氧同位素曲線探討了黃東海陸架晚第四紀古環境演化、底棲動物群特徵、古氣候、冰後期以來氣候事件、古水團、速率、古水深、物源、海平面平均上升率,討論目前中國東部海平面上升的狀況、溫室效應及海岸保護。
  3. The paper divided turbidite fan in deep water from long source into braided channel microfacies, inter - braided channel microfacies, medium fan over - belt microfacies, and external fan subfacies, and divided slump turbidite which related with delta into medium fan subfacies and external fan subfacies, and summed up 15 kinds of marking of subfacies and microfacies classification. at the same time, it formed a series of effective technology of analyzing turbidite source at the base of studying region geological which combined with analyzing the content change of terrigenous debris, with the found of logging facies, and with the ancient terrestrial magnetism test and other technology means under the guidance of three - dimensional model of turbidite which has been founded already and the flat surface feature of microfacies

    將遠源深水濁扇劃分為辮狀水道微相、辮狀水道間微相、中扇過渡微相和外扇亞相;將與三角洲有關的滑塌濁扇劃分為中扇和外扇兩個亞相,並總結了濁劃分各種亞相、微相類型的十四種標志,分別為:巖石類型、層理類型、砂巖單層厚度、粒度結構特徵(粒度中值、分選性、概率曲線) 、生物化石、儲層物性(孔隙度、滲透率) 、巖隔層特徵(巖單層厚度、層數、顏色) 、鮑瑪層序組合和自然電位曲線特徵。
  4. Terrestrial sediments consist mainly of fluvial and lacustrine facies have the following characteristics : lacustrine basins have undergone a long continuous and fast subsidence and contain many terrestrial source rock sequences ; sedimentary facies of terrestrial basins are deposited in a ring formation. the best source beds are the continental source beds which contain dark shale

    陸相以河流湖泊相為主,其基本特徵有:長期快速降的湖相盆地是陸相生油的發育區;陸相湖盆的大都是環狀分佈,暗色巖是最佳生油層。
  5. On the base of fully utilizing the available data about tectonic maps and structural elements, the present paper has made synthesized research that used the ways of stratigraphic sequence edge unconformity analysis and stratigraphic thickness correlation analysis, and combined seismic - data interpretation, review of paleo - structure and ancient landform and research of tectonic evolution and petroleum system, and combined region and location, plane and profile and time and spatial. by the synthesis analysis on tectonic evolution of hetian paleo - uplift in tarim basin, the results indicate that : ( 1 ) hetian paleo - uplift is a sedimental and erosional paleo - uplift. the formation and evolution of the hetian paleo - uplift experienced three stages, that is, the uplifting and eroding stage of the caledonian period, the depositional stage of the hercynian period and the destroying stage of the himalayan period, and evolved from paleo - lift to inclining strap at last

    本文採用地質和地球物理相結合的研究思路,運用多種技術手段和方法;在充分利用已有構造圖資料和構造要素資料的基礎上,運用地層層序邊界不整合分析法、地層厚度對比分析法,結合地震資料的精細解釋、古構造和古地貌的恢復、構造演化史研究、含油氣系統的研究,和區域和局部、平面和剖面、時間和空間的結合研究,對塔里木盆地和田古隆起構造演化及油氣關系進行了綜合分析,認為: ( 1 )和田古隆起為一?剝蝕性古隆起;形成於志留-盆紀;其構造演化可分為三個階段,即加里東期的抬升剝蝕階段、海西期的階段和喜山期的破壞階段,最終由古隆起演變為一斜坡
  6. Since the past 5000 years, it is the most serious period that salt lake withered. ( 2 ) from 1989 to 1999, the deposit zonations have changed. the width including borax mud dust has increased nearly 260m. the area which is rich in boron lithium potassium has increased nearly 2. 8km2

    ( 2 )從1989 ? 1999年的十年間,扎布耶鹽湖鹽的發生了變化,含硼砂寬度增加了近260m ,硼鋰鉀富集區增大,面增加了近2 . 8km ~ 2 。
  7. Abstract : the nearshore around the nanhui spit is a transitional zonebetween the yangtze estuary and the hangzhou bay with complicated dynamic conditions, sediment transport, sedimentological processes and morphological evolution

    文摘:南匯咀近岸水域位於長江口和杭州灣的交匯,其動力條件、沙運移、過程和地貌演變復雜。
  8. According to the differences of sedimentary facies and environment, the source rock are divided into four types such as lime - mud reef in platform margin, platform inner sag, deep - water flat slope or continental shelf, abyssal basin, the lime - mud reef type is distributed in platform margin of upper ordovician, the remained three types are widely distributed in cambrian - ordovician system

    根據環境的不同,可將烴源巖劃分為在不同環境中的4種類型烴源巖;臺地邊緣灰丘型烴源巖、臺地內凹陷型烴源巖、深水緩坡與陸棚型烴源巖、深海盆地型烴源巖。
  9. The comprehensive geological characteristic has been fully studied in this paper. on the basis of this, closely combining production practice, the favorable gas developing regions have been determined with the methods of sedimentary facies and combination of generation, reservoir and caprock, and logging parameters interpretation maps and regression formulas have been established with logging data, as well as reprocessing, interpretation and identification of gas reservoir have been done with computer. integrating the information and results of geology, logging, testing and geophysics, the gas reservoir distribution regularity of structure of no. 1 sebei has been described and reserves in place of no. 1 ' sebei gas field have been recalculated, which have provided a basis for next step of development in research area

    在近十多年,通過提高地震資料處理精度、淡水聚合物漿的應用、數字測井技術的運用、並加強了低電阻層和差物性層的試氣及氣田擴邊鉆探,大大提高了對氣層的識別,大量增加了氣層的層數和厚度,擴大了氣田的含氣面,使氣田儲量通過多次復查核算仍在不斷增加本論文充分研究了青海澀北一號氣田天然氣地質綜合特徵,並以此為基礎緊密結合生產實踐,應用相與生儲蓋組合等方法確定氣藏有利發育區,應用測井資料建立測井參數解釋圖版並回歸公式,應用計算機重新處理、解釋和識別氣層,綜合地質、測井、試井、物探等多方面信息與成果,描述了澀北一號構造的氣層分佈規律,重新計算了澀北一號氣田的地質儲量,為研究區下一步開發提供了依據。
  10. With stromatolite but no desiccation crack, the depositional environment of middle - late cambrian in the area was intertidal zone to subtidal zone with the shallow - water features

    根據其中的疊層石和無明顯裂構造,推測為潮間局限潮下環境。
  11. Alluvial soil a type of soil formed on river floodplains and deltas, where new sediment is deposited on the land during floods

    土:在河流漫灘和三角洲地由洪水沖刷而形成的土壤類型。
  12. Based on the studies in sea - level rise and response of coastal zone by domestic and foreign researchers, integrated with the essential characteristics of jiangsu coast and the radiate sand ridges, laid emphasis on the effects of sea - level rise on the radiate sand ridges and the tiaozini sands in it ' s center region, the following case were discussed in the paper. ( 1 ) the recent relative sea - level rise in the region of the radiate sand ridges found on the structural and sedimentary features of the radiate sand ridges, the rate of regional land subsidence was calculated ( structural, balanced and compressed subsidence were considered respectively ). the latest assessment of global sea - level rise in the past century that was carried out by ipcc was cited

    本論文在總結國內外對海面上升及其對海岸影響的研究基礎上,結合江蘇海岸及輻射沙洲區的基本特徵,以相對海面上升對輻射沙洲及其中心部位的條子的影響為重點,討論了以下幾個方面的問題: ( 1 )輻射沙洲區近期的相對海面變化根據輻射沙洲區的構造和特徵,對區內地面降速率進行分項計算(包括構造降速率、均衡降速率和壓實降速率) ,並引用ipcc最近對過去100年來全球絕對海面上升速率的評估。
  13. The water channel was dredged to remove sediment and restore the proper depth of water. deep bay and mai po receive large amounts of sediments from the pearl river estuary. some of this sediment settles onto the mudflats, but a lot is brought into our

    米埔位於珠江河口,每年珠江河為后海灣及米埔來大量的沙,部份灘上,大部份則隨著基圍水閘操作流入基圍,在水道,令水道變淺。
  14. Excellent correlation exists between the distribution of bottom shear stress and that of sediment types. low shear stress occurs in the central mud area ; where only fine - grained sediment can be imported by weak tidal currents. once settled into the bed, it is difficult for set the sediment into motion

    中部區為應力低值區所在,水動力弱的中部區只能接受弱水動力來的細顆粒物質,而且這些細顆粒物質一旦下來,便難以再懸浮搬運走,說明中部區是連續細顆粒物質區。
分享友人