淺海層的 的英文怎麼說
中文拼音 [jiānhǎicéngde]
淺海層的
英文
epipelagic-
They are said to be “ undersaturated. ” shallow, warm surface waters are described as “ supersaturated ” with respect to both calcite and aragonite, meaning that these minerals have no tendency to dissolve
海洋淺層的溫暖海水,對方解石和霰石則為過飽和,代表這兩種礦物不傾向溶解。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 greatest impact would be on land and very-shallow water organisms unprotected by deep water.
受影響最大的當然是陸生的和那些沒有厚層海洋水保護的淺海生物。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泥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、沉積速率、古水深、沉積物源、海平面平均上升率,討論目前中國東部海平面上升的狀況、溫室效應及海岸帶保護。Find a suitable image of the sea ; ones of shallow, frothy water work best
找到一個合適的形象,在海中;的淺層,泡沫水工作,最好的。According to the regional geology and the character of the lithofacies and well - logging facies, 4 kinds of sedimentary facies and 3 kinds of depositional system : marine system, delta system and fluvial system have been identified. the sedimentary facies of taiyuan formation is marine faceis, up to sanxi formation, the sedimentary facies is delta facies, the xiashihezi formation hel and he2 member are braided river facies, he3 member is meandering river facies. the mains types of sandstone of taiyuan formation are lithic quartzarenite and quartzarenite ; the mainly types of sandstone of sanxi formation and xiashihezi formation is litharenite
通過對20餘口井2000多米巖心的觀察和對40幾口井的測井數據解釋、對比,在研究區目的層段識別出了12種基本巖相和9種測井相類型,在區域沉積背景和單井相劃分的基礎上,根據巖相和測井相組合特徵,在太原組?下石盒子組劃分出4種沉積相和若干沉積微相,並進一步劃分為3類沉積體系:濱淺海沉積體系、三角洲沉積體系和河流沉積體系。Research results indicate that, with the thermocline intensity of standard 0. 05 / m as a measure, there are shallow thermocline and deep thermocline all the year round in scs
研究結果表明:以0 . 05 / m強度標準衡量,南海四季都存在上界小於50米的淺躍層和大於50米的深躍層。Beneath the relic sand of the outer shelf there is high grade of valuable heavy mineral sand ( for example ilmenite ) reaching the ii anomaly order of marine placers and it is of potential resource prospects
通過碎屑礦物判斷,原巖應是中酸性巖漿巖和淺變質巖類。鈦鐵礦等有用礦物在細砂層位中出現較厚的砂礦異常,顯示一定的淺海砂礦資源潛力。By comparing with the strata of " holocene series of the coastal plain of laizhou bay " and combining 14c age measurement, the strata position and features of the lagoon ? hallow sea ? each sedimentary facies are confirmed. the stratigraphic division of upper marine facies of holocene is done and the sedimentary environment of every stratum is affirmed
通過與「萊州灣濱海平原全新統」進行地層對比並結合~ ( 14 ) c測年數據,確定了該沉積區全新世瀉湖?淺海?海灘相沉積層的層位和特徵,並對該層及其以上地層進行地層劃分,判斷出各層的沉積環境。The effects of sediment parameters on the multi - path structure in shallow water are investigated in detail. a method of dividing the multi - path arrival time differences into groups is presented. theoretical analysis for the method is given
詳細研究了沉積層聲速、密度和衰減系數變化對淺海多途到達結構的影響,提出了對多途到達時延差進行分組的研究方法,從理論上對該方法進行了研究。The sediments of the incised valleys show an upward - fining succession, and can be grouped into four sedimentary fades : gravel lag - deposit of in - channel to partly over bank sediments of a meandering river, flood plain - estuary, estuary - shallow marine, and estuary sand bar, based on lithology, paleontology, and sedimentary textures and structures
根據巖石學、沉積結構和沉積構造特徵,本區下切河谷充填沉積物具有向上變細的沉積層序,可以劃分為4個沉積相類型:河床滯留沉積物到部分曲流河沉積體系的邊灘沉積、河漫灘河口灣沉積、河口灣淺海沉積和河口灣砂壩沉積。The effects of sound field by sediment in shallow water
關于淺海沉積層對聲場影響的討論And a thesis is exactly that the author presses close to poet ' s haizi and poet ' s posthumous work tightly by way of analysing that compares with , sum up , amplify expanding and found and ask solving synthetically, is it to strike earth , support inner world and spiritual manor , poet of haizi direct to bow with high up in the air posture ( namely the following spiritual homes ) , attempt to melt with poet ' s haizi altogether , in order to achieve deeper purpose to understand posthumous works of poet and poet , reach and understand and step forward it close to the subject deeply , is even as big as the original intention of the way to simply analyse poem that a poet believed in in life
而本論文正是筆者通過分析對比、綜合概述、引申推展以及創設求解的方式緊緊貼近詩人海子以及詩人遺作,以凌空姿勢俯向沖擊大地,直抵詩人海子的內心世界和精神領地(即以下的精神家園) ,企圖與詩人海子共融,以達到更深層次解讀詩人以及詩人遺作的目的,企及深刻解讀進一步靠近題旨,大到淺析詩人于生活中所信奉的詩歌之道的初衷。The gas chimney can be applied in hydrocarbon exploration in terms of ranking prospects, detecting migration pathways, distinguishing sealing or non - sealing faults, identifying potential over - pressured zone and drilling ( shallow gas ) hazards as well as assessing the sea floor stability for platform design and drilling
氣煙囪在油氣勘探工作中有其獨特的作用,可以有效地預測勘探方向、揭示天然氣的運移路徑、預測斷層的封閉性,同時利用氣煙囪還可以預測超壓和海底構造穩定性,降低淺層氣鉆探風險。Jacket is the most widely used offshore platform structural style. first of all, the paper summarizes the present achievements of dynamic analysis for offshore platform, and studies both the vibration isolation system for jacket and vibration - suppressed effectiveness. considering the style and character of jacket, and in order to make best use of dampers to reduce vibration, a damping isolation scheme, in which the damping layer is laid between the jacket cap and deck is put forward
本文在總結國內外對海洋平臺結構動力分析研究現狀的基礎上,針對淺海導管架式海洋平臺的型式與結構特點,研究了導管架式海洋平臺結構阻尼隔振體系及其減振效果,為了充分發揮阻尼器的耗能減振作用,提出了在平臺結構導管架端帽和甲板之間設置柔性阻尼層的新型阻尼隔振方案。The palaeogeographic research indicate that the palaeogeographic outline of the study area recorded the evolution from a sedimentary basin in which the shallow - water carbonate platform sediments and deep - water terrigenous clastic submarine fan developed from southeast to northwest and northeast during the late triassic through a submarine sheet - like model composed of deep - water sandy turbidite and fine - grained turbidite during the early jurassic to a terrigenous clastic barrier coast during the middle and late jurassic and finally to the coal - bearing delta sediments during the late cretaceous
古地理分析表明,研究區晚三疊世古地理輪廓是一個從東南向西北和東北方向由淺水碳酸鹽臺地及深水陸層海底扇沉積共同發育的沉積盆地;早中侏羅世,演變成為一個由深水砂質濁積巖和細屑濁積巖組成的水下席狀體沉積;進入中晚侏羅世,其古地理表現為一個陸屑淺海有障壁海岸;到了晚白堊世,研究區表現為以含煤沉積為特徵的三角洲相沉積。Typical depositional structures of tempestite, such as radically arrangement of plate - like micrite gravel, hummocky lamination, load structure, grading bedding and ripple bedding are presented in the succession, indicating its accumulation in an offshore environment
該風暴沉積的底面侵蝕構造清楚,板片狀泥晶灰巖礫石呈菊花狀排列,發育丘狀交錯層理、負載構造、遞變層理和小波紋層理等沉積構造,為典型的淺海風暴巖。A perturbative shallow water tomography scheme based on the modal wave number inversion technique is considered in this paper. and it could estimate the bottom sound speed and density
論文提出了一種基於簡正波波數的擾動反演淺海聲層析方法,該方法能夠反演海底聲速和密度。Analyses of grain size and mineral components of surface sediments in the offshore area of the northeastern shandong peninsula were carried out to reveal the sediment source and the relationship between the characteristics of grain size distribution and sedimentary dynamic conditions in the littoral zone off the northeastern shandong peninsula
摘要對山東半島東北部濱淺海區海底表層沉積物的粒度和礦物組分進行了分析,探討了其物源及其粒度分佈特徵與沉積動力條件的關系。To get the stability of shallow structure foundation and adjacent seabed in cheng dao shallow sea area, we have made an investigation on high resolution echo depth side sonar and shallow strata section etc. and made use of experiment analysis of core, in situ, indoor to compute, analyze and assess the stability on new computing method
為了得到埕島海域淺水區構築物地基及周邊底床穩定性,本文通過高解析度的回聲測深、旁側聲納及淺地層剖面等聲學儀器勘查,並結合鉆孔、現場和室內的實驗分析,採用新的計算方法,對埕島海域淺水區人工構築物地基及周邊底床穩定性進行了計算、分析和評價。分享友人