tertiary area 中文意思是什麼
tertiary area
解釋
三級區-
The filling evolutionary process in the palaeozoic era in this area was extremely complex. during the majiagou stage of early ordovician period, the researched area went through three tertiary eustatic cycles. with negative movement in ma ; stage, deposits of evaporate platform and local platform were developed
古生代研究區經歷了十分復雜的充填演化過程，早奧陶世馬家溝期本區經歷了三個三級海平面升降旋迴，其中馬5期隨著海平面下降，發育了蒸發臺地和局限臺地沉積。 -
Speaking at the press briefing on the project after the contract signing ceremony, the director of drainage services, mr raymond cheung tat - kwing, said today ( august 27 ) that tertiary - level treatment was given to the sewage collected at ngong ping in order to protect this environmentally sensitive area and the water quality of the water gathering ground for shek pik reservoir and other receiving water bodies
渠務署署長張達?今日（八月二十七日）在簽約儀式后，向傳媒簡介工程內容時表示，為保護這環境敏感地帶和石壁水塘集水區及其他接收水域的水質，因此在昂坪收集的污水，將採用三級程度處理。 -
The characteristic of shehejie group of tertiary gritstone fan body in wangzhuang area of dongying depession
3段扇三角洲砂礫巖體沉積特徵分析 -
The study area is composed of sandstone & conglomerate reservoir of alluvial fan & fan delta, which belong to sha3 lower member and sha4 upper member of lower tertiary of yong " an town oilfield in dongying depression. the target stataum develops in the hanging wall of the synsedimentary fault in the scarp zone of dongying depression. the frequently intense movements result in the variation of sandstone and conglomerate reservoir and the evolution of the time and space of sha3 lower member and sha4 upper member in yong " an town oilfield
研究區是東營凹陷永安鎮油田沙三下段、沙四上段的沖積扇和扇三角洲砂礫巖體，目的層發育在東營凹陷陡坡帶同生斷層的下降盤，因斷層多期強烈活動，導致永安鎮油田沙三下段、沙四上段的砂礫巖體成因類型多，時空演化變化大，在扇根一帶小層對比難度大，給油田開發帶來很大的難題，在這種背景下進行流動單元研究難度更大。 -
( 4 ) the formation and growth of structural traps and stratigraphic - unconformity traps in the area is controlled by three compressive stages of silurian - devonian, late permian - tertiary and oligocene - quaternary ; non - structural and compound traps mainly grew in the early paleozoic. structural traps mostly grew in the late paleozoic and the cenozoic and mostly grew on the north and south belts ; non - structural traps mostly grew in the northern area of the hetian concave. most traps in the area formed or typed at last in the himalayan episode, dispersed on the north and south belts
（ 4 ）研究區構造與地層不整合圈閉的形成和發育受志留-泥盆紀、晚二疊世-第三紀、漸新世-第四紀三個擠壓階段的控制；早古生代主要發育非構造圈閉和復合圈閉，晚古生代和新生代則主要發育構造圈閉：構造圈閉主要發育在南北兩帶上，其次為中帶；非構造圈閉主要發育在和田凹陷以北的地區；研究區內大多數圈閉是喜山期形成或最終定型的，在南北兩帶都有分佈，而海西期圈閉主要分佈於研究區中帶瑪南構造帶處。 -
Based on the original data of tm in 1988, 1992 and 1998, then after some processing and analysis, the author have the thematic data of land - use by interpretation. on the basis of them, the author made the analysis of land - use for this area based on the spacial analysis of gis and the method of comparison between result of land - use classification as follows : the method of aggregating analysis, the analysis of urbanization, the analysis of the transformation rate of cultivated land, the analysis of the driving force of land - use change and the sustainable use of land. the conclusions may be demonstrated below : the cultivated land decreases with the patchs fragment ; road spreads radialy surround second - ring road ; the urban land expands quickly toward southwest along the major roads and be concentrative. rural land and industry increse rapidly with dispersing ; 0thers change slowly. the major driving forces of land - use change in this area are the rapid expansion of urban and rapid growth of population, foreign investment and the development of tertiary industry which was based upon the real estate. according the trendency of land - use change, the author consider that we must insist on the way of the sustainable use of land based on protecting the cultivated land
在此基礎上，應用分類結果比較法，在gis各種空間分析功能（幾何量算、統計分析、疊加分析及緩沖區分析）的支持下，對該區土地利用變化進行了如下分析：土地利用綜合分析、城市化進程分析、耕地轉化率分析、土地利用變化因素分析及土地的可持續利用分析。結果表明：該區土地利用變化主要表現為耕地大量減少，斑塊破碎化；交通用地沿二環線呈放射狀向四周擴展；城鎮用地沿交通干線向西南方向擴張迅速，用地趨于集中；農村居民點和工礦業用地增加，用地趨于分散；其它用地變化較慢。這一用地變化的主導因素是城鎮用地擴展快、人口增長迅速、外資的大量投入及以房地產為主的第三產業的快速發展。 -
Could there exist another possibility for the south boundary of the system as follow : the rainfall infiltrates in the outcrop carbonate - mountain area of western, and moves towards south and deeper along carbonate rocks, then moves upper through the overlain tertiary system ( n ) with a thickness of 400m ( instead of running off to the springs and yellow river through a long approach of least hydraulic gradient ), and then mainly transforms into the horizontal drainage in the loess layer of quaternary, finally drains in lu - botan depres sion
並且提出，關于對系統南界的認識，是否存在另一可能：即在西部碳酸鹽巖裸露區大氣降水入滲后，沿碳酸鹽巖向南向深部運動，然後，並非在極小的水力坡度驅動下長距離地向東部黃河、泉群徑流排泄，而是通過上覆厚度約400m的第三系向上運動，繼而主要在第四系黃土層中轉為向南水平排泄到鹵泊灘。 -
The decrease in cultivated average farmland mainly and the farm capital substituting function on the workforce embody agricultural repel strength. the absorbing forces in rural and urban area use one liner regression model predicting the absorbing power of the secondary industry and the tertiary industry in rural region and the urban as a whole. the shifting frictional force shows as economic cost and psychological cost mainly
農業排斥力主要通過人均耕地面積的減少和農業資本對勞動力的替代作用來體現；城鄉吸納力主要運用一元線性回歸模型分別預測了農村第二產業、第三產業和城鎮總體對農業勞動力的吸納能力；轉移摩擦力主要表現為經濟成本和心理成本。 -
Depositional feature of tertiary yanchang formation of fuxian exploratory area in ordos basin
鄂爾多斯盆地富縣探區三疊系延長組沉積特徵 -
Besides, the study of cantonese dialect is an academic subject. many members of the linguistic societies, teaching staff and students of tertiary institutions are conducting research in this area
此外，粵方言研究是一門學科，不少語文學會會員和專上院校師生都以這個課題進行學術研究工作。 -
The study area, gubei slope is situated in zhanhua depression, jiyang subbasin, bohaiwan basin, which lies between gudao uplift and gubei depression, the area is about 100km2. up to now, this area has been drilled into part of the mesozoic, shahejie formation, dongying formation, guantao formation, minghuazhen formation and pingyuan formation of the tertiary
到目前為止，該工區已鉆穿了部分中生界、沙河街組、東營組、館陶組、明化鎮組和平原組等地層，本論文研究的主要對象是下第三系沙河街組沙二、沙三段地層。 -
This difference is caused not only by maturity but also by source rock. natural gas in baimiao area is mainly derived from tertiary source rock and carboniferous permian formation in qianliyuan sag, which is near the high point on lanliao fracture belt
白廟地區天然氣主要來源於前梨園窪陷第三系烴源巖和石炭?二疊系煤系地層，靠近蘭聊斷裂帶構造高點，淺層es _ 2 ~下? es _ 3 ~ 2氣層具有較高的ar ~ （ 40 ） ar ~ （ 36 ）比值，為煤型氣及混合氣。 -
The study area is in the eastern part of linqing depression, with an area of 5910km2. it is a mesozoic - tertiary rift basin, located in the southwestern end of bohai bay basin
構造位置處于渤海灣盆地西南收斂端，為一中、新生代大陸裂谷盆地，總面積18000km ~ 2 ，研究區面積約5910km ~ 2 。 -
The hydrothermal limestone breccia sheet presented over tertiary fluvial, lacustrive sandstone and mud in the wandongshan - wulipai area is a hydrothermal breccia landslide from the chenjiazhuang breccia pipe, and it may be a domain origin which would have obstructed the jinshajiang old channel and made the jinshajiang river to change and to form the famous valley and turns
萬洞山五里排帶呈席狀覆蓋于第三系河湖相的砂礫巖和粘土沉積之上的灰巖質熱水角礫巖為一套從陳家莊角礫巖筒滑覆過來的熱水角礫巖滑體，其可能是造成金沙江古河道淤塞並使古金沙江改道和形成大拐彎的主要原因。 -
The good reservoir facies are braided stream and braided delta in alaer area, fan - delta in arhati area and lake - floor fan in shizigou - ganchaigou area. all of these areas are the main targets for oil exploration, it has discovered that there is an important unconformity between upper youshashan and lower youshashan formation of tertiary, on which there are a large amount of erosion and long time of depositional hiatues
在上述研究的基礎上，對區內油氣勘探的有利區帶進行了預測，指出阿拉爾北東辮狀河三角洲相帶、阿哈提南東扇三角洲相帶和獅子溝一乾柴溝湖底扇相帶為區內有利的儲集相帶，是今後勘探的主要目標。 -
The controlling factors of tertiary sequences in hong - shi area are tectonic, climate and their combinations
明確提出了控制紅獅地區層序發育和分佈特點的主要因素是構造、氣候及二者結合的觀點。 -
From connecting - well profiles that reflect filling characteristic of basin, combining with comprehensive analysis of seismic stratigraphic framework, the sequence stratigraphic framework of tertiary was established in hong - shi area and the distribution of sedimentary systems in time and space was deeply discussed
通過能揭示區內第三系沉積充填特徵的連井剖面，結合地震層序地層格架的綜合分析，建立起了紅獅地區第三系的層序地層格架，探討了沉積層序的時空分佈規律。 -
It is a late cretaceous to tertiary basin located on the eastern part of the continental shelf of the east china sea ; it occupies an area of 59, 000 km2
西湖凹陷是晚白堊第三紀盆地，位於中國東海大陸架的東部，面積590000km2 ，處于緯度124030 '與127000 '之間，經度28030 '與31000 '之間。 -
On the basis of a comprehensive study of the outcrop, core, well log and seismic data, taking the high resolution sequence stratigraphic theory as a direction, the tertiary sequence stratigraphic system was firstly established in hong - shi area in qaidam basin, which consists of 42 sequences, 12 supersequences, 3 supersequence sets and 1 megasequence
首次在區內第三系中建立了以三級層序為基本單元的層序地層系統，其中包括42個三級層序、 12個超層序、 3個超層序組和1個一級巨層序。 -
The second gas generation starts at the beginning of tertiary and it continues till present. the vertical carrying system and lateral carrying system have been thoroughly investigated for the first time in the study area. their characteristics and evolution history are studied integratedly, synthetically, dynamically, and quantitatively from both bulk properties and micro - features
整體、系統、動態、定量以及宏觀與微觀相結合，首次深入地研究了本區的垂向輸導系統（包括斷層垂向輸導系統、火成巖輸導系統等）和側向輸導系統（包括具孔滲性能的自源輸導層、它源輸導層等）的特點及其形成和演化。
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