陸架盆地 的英文怎麼說
中文拼音 [liùjiàpénde]
陸架盆地
英文
shelf basin-
Pre - cenozoic groups in the shelf basin of the east china sea
東海陸架盆地的前新生界The origin and evolution of land plants was an important event in the history of earth life and has affected all other lives on the earth and global environment. during the past two decade, the new discoveries of fossil plants microfossils and megafossils from the mid - ordovician through all silurian to the lower devonian improved knowledge of the origin of land plants, provided a time framework of the basal groups for the land plants and the early evolution diversity of vascular plants. three new plant based epochs have been recognized. on the other hand, molecular sequence studies have provided insights into the phylogeny and early branches of land plants. a phylogenetic tree has been established by the joint of a study of comparative morphology and gene sequences. this paper summarizes recent advances and new knowledges, comments on the phylogenetic studies based on the cladistic analysis
陸生植物的起源和演化是地球生命中的重大事件,它影響到地球上所有的其他生命和全球環境。在過去的20年中,從中奧陶世歷經整個志留紀至早泥盆世的巖層中,化石植物微化石和大化石的新發現改變了人們對陸生植物起源的認識,並且為陸生植物和維管植物早期演化分異提供了基部類群分化的時間框架。據此人們識別出地史中的3個陸生植物的時代:始胚植物時代始維管植物時代和真維管植物時代。In east china sea shelf basin, the mesozoic relict sediments are distributed in some central - south areas, such as fuzhou sag, minjiang sag and yushan lower uplift
摘要東海陸架盆地中生界主要分佈於盆地中南部的福州凹陷、閩江凹陷和漁山低隆起地區。The topography and the physiognomy of the south china sea are very complex such as continental slop, continental shelves, seamounts, sea basin, etc. the south china sea lies between qingzang plateau, which is as the main driver of the variety of climate, and the western part of the pacific, which is called warm pool, and is influenced by some current systems, such as coastal current, kuroshi, etc. the south sea has considerable species
南海具有陸坡、陸架、海溝、海盆等復雜的地形、地貌;南海位於作為地球氣候變化的主要驅動力的青藏高原和西太平洋暖池之間;南海受到沿岸流、南海暖流水、黑潮入侵水等流系的影響;南海具有豐富的物種分佈;上述因素共同影響南海生源要素的分佈、輸送和遷移。In a study on a sedimentary basin analysis of the huanan orogenic belt, the sedimentary basin character and evolution in the southeastern passive continental margin of the yangtze plate is investigated with elaborate sedimentary environments and sedimentary character from the sinian to the triassic, and then the sedimentation sketch of this belt is established especially to be from rift, passive continental margin into foreland basin in the early paleozoic on the yangtze plate
在華南造山帶沉積盆地分析和演化研究中,對揚子大陸東南邊緣從震旦紀到三疊紀沉積環境,沉積作用特點,沉積盆地性質和演化進行研究,特別是建立了中國南方揚子板塊早古生代從裂谷,被動大陸邊緣到前陸盆地華南造山帶沉積作用格架。4. triangular diagram of the sandstone clastic compositions and the relationship diagram of major element suggest that the proto basin of the clastic rock of the yanbian group was a forearc basin, which was in an active continental margin
鹽邊群碎屑巖碎屑骨架顆粒統計分析結果和砂巖常量元素構造環境判斷圖解顯示,它們所處的構造環境為活動大陸邊緣,初步判定它們的原型盆地為弧前盆地。The sedimentary formation can be summarized as rift bay filling sequence, epicontinental sea filling sequence, offshore debris lake basin sequence and inner continental lake basin sequence. a framework of sequence stratigraphy for the upper palaeozic strata is established in the area. the helan aulacogen of upper carboniferous in the west margin of ordos can be divided into 12 sequences, and most of the upper palaeozoic strata in the area can be divided into 15 sequences
本文對研究區內上古生界進行了層序地層學探討,將本區沉積建造概括為裂陷海灣充填層序、陸表海充填層序、近岸碎屑湖盆層序和內陸湖盆層序,建立了研究區上古生界層序地層學格架,西緣賀蘭拗拉槽上石炭統劃分為12個層序,本區大部分地區上古生界可劃分出15個層序,並全面地概括了層序演化各階段的具體特徵。Controls of mesozoic and cenozoic tectonic evolution on source rock distribution in east china sea shelf basin
東海陸架盆地中新生代構造演化對烴源巖分佈的控製作用For the exploration of mesozoic remnant basin on east china sea shelf, therefore, a principle of " mesozoic - cenozoic combination " should be complied
東海陸架中生代殘餘盆地勘探應「中新(生界)結合、上下兼探」 。Based on the theory of plate tectonics and the new knowledge of continental dynamics, this paper starts mostly with tectonic analysis and then makes a comprehensive view on the characteristic of stratum composition, gold mine mineralized, magmatic activity as well as ruptures activity to discuss the yanshanian tectonic evolution of the xiaoqinling area under the regional tectonic framework of qinling orogenic belt
本文以板塊構造理論和大陸動力學研究的新認識為指導,採用以構造分析為主線,結合區內地層沉積、金礦成礦、巖漿活動以及南北兩側斷陷盆地形成演化等綜合分析,在秦嶺區域構造大框架下對小秦嶺燕山期的構造演化特徵進行探討。East china sea shelf basin, consisting of tertiary oil - bearing strata and great in thickness, is an important cenozioc oil - bearing basin in china
摘要東海陸架盆地是我國重要的新生代海上含油氣盆地,其中充填了巨厚的古新近系含油巖系。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。Through the analysis of the stratigraphy and sedimentary facies of the research areas, the description model between the stratigraphic framework and deposite environment can be set up firstly by the transition from the " three horizons sandstone with two intercalated limestone horizons ' mn yanshiping area to shale and marl in amdo - zigetang co, and to oil shale in bilong co, then by the transition of the shallow water platform facies to the deep water continental shelf, slope, and to the deep water basin
通過對研究區地層和沉積相分析,建立起一個從北向南由雁石坪地層類型「三砂夾兩灰」過渡為安多?茲格塘錯地層類型泥頁巖、泥灰巖,最後到比洛錯地層類型黑色油頁巖,由淺水臺地相過渡到深水陸棚、斜坡,最後到深水盆地相的地層格架與沉積環境解釋模式。So it had the long distance controlling effect on the sediment in the ordos. it is generally supposed that on the ramp of cratonic basin, the sequence of the epicontinental sea in the ordos is mainly composed of the transgressive system tract and the high stand system tract. this paper shows that it is possible that the incised valley of the low stand system tract can exist on the continental shelf in the basin
鄂爾多斯地區上古生界具有克拉通盆地陸表海緩坡沉積的一般特徵,層序構成一般以海侵和高位體系域為主,本次研究認為在陸表海沉積背景下,除在大陸邊緣附近,在盆地內古大陸架上也可以發育低位體系域的下切河谷充填沉積。When the research content and meaning of the orogenic - sedimentology far more is expanding, and enlarging to the global paelogeography. the evolution history in rifting - assemble of southern china continental landmass is investigated with a relationship between sedimentary basin and orogenic belt, which reflects not only a synchronizing but also asynchronies in contrast, the southern china landmass with the global paelogeography. meanwhile it is promoted that the pan cathaysian is an important part of the global paelogeography
把造山帶沉積學研究內容和內涵進一步擴展,放到全球的古地理格架中,從造山帶和沉積盆地關繫上研究中國南大陸的獨特裂聚演化史,反映出中國南大陸與全球古地理對比既有同步性也有非同步性;進而提出泛華夏陸塊群是全球古地理的一個重要組成部分。分享友人