海侵 的英文怎麼說

中文拼音 [hǎiqīn]
海侵 英文
[地質學] advance of sea; transgression （of sea）
  • 侵 : Ⅰ動詞（侵入） invade; intrude into; infringe upon Ⅱ形容詞（接近） approaching Ⅲ名詞（姓氏） a surname
  1. During the upper paleozoic in huabei there were 3 main times of sea level eustacy which caused different deposits in research area

    華北晚古生代經歷了3次大的海平面升降旋迴，不同海侵事件在研究區內留下了不同的沉積紀錄。
  2. The persistent sea invasion pressed wu - lao - keng tribe gave up the resources of seacoast and chosed burned - cultivation instead and took up their residence in the higher area of plain

    反覆的海侵，迫使武?坑系統放棄海岸資源，選擇以燒墾的方式居住在平原較高處。
  3. A study on the holocene transgression and the xigang ancient seabar in the yancheng area

    全新世海侵與鹽城市西岡古砂堤研究
  4. Through synthetically study, some achievements are made as follows : 1. based on the application of sequence stratigraphy, for the first time the characteristics of sequence stratigraphy in the xicheng concentrated mineralization area are discussed systematically and 13 three graded imperfect sequences of devonian stratum are recognized. the result shows that hydrothermal sedimentary mineralized type and hydrothermal sedimentary - rebuilded mineralized type ore deposits occur in intergrade between two sequence, as well as occur in intergrade between highstand systems tract and transgressive systems tract

    通過對該區礦床成礦作用的綜合分析研究，取得了如下一些成果和認識： 1 ）應用層序地層學理論，首次系統論述了該區泥盆系層序地層的特徵，識別出13個不完整的三級層序，並進行了區域對比。層序地層分析發現海底熱水沉積型礦床和海底熱水沉積-改造型礦床的賦礦部位是兩個層序的過渡部位，既高水位體系域向海侵體系域過渡。
  5. Transgression of late paleozoic era in ordos area

    鄂爾多斯地區晚古生代的海侵
  6. The sea makes depredations on the land

    海對陸地作了掠奪海侵蝕了陸地。
  7. The results indicate that these parameters in profile change closely with geotectonic cycles as follows : sulfur, colloid and asphaltene contents keep the lowest values in devonian, triassic, jurassic and tertiary ; they are in accordance with regressive geotectonic phases, of which the maximum values appear to be correspond to the largest - scale marine transgressions occurred in caledonian cycle, hercynian cycle and middle phase of alpine cycle

    指出，這些石油參數在剖面上的變化與大地構造旋迴有密切關系：硫，膠質和瀝青質的含量在泥盆紀、三疊紀、侏羅紀和新近紀為最低值，它們與海退構造階段相一致；石油化學成分最大值與加里東旋迴、海西旋迴和阿爾卑斯旋迴中期的最大海侵相一致。
  8. In the interim from highstand systems tract to transgressive systems tract, faulting is violent in the basin, different kind of fluids coming from dissimilar position of lithosphere enter into synsedimentary faults served as a place fluids mixed to form ore - bearing hydrocarbon alkali - fluids

    在從高水位體系域向海侵體系域的盆地相迅速轉化時，盆地內斷裂構造活動強烈，斷裂溝通不同部位的熱水流體，使成礦烴堿流體沿斷裂上升，在海底沉積成礦。
  9. By that time the choices of settlements for jiu - she type and kavalan were influenced by river system but not sea invasion

    舊社類型與噶瑪蘭族聚落位址的選擇不再受到海侵的影響，轉以河系分佈作為考量的因素。
  10. The areas of transgression are indicated by wide spacing of the thickness contours.

    稀疏的等厚線代表海侵區。
  11. Studying marine transgression of early tertiary in dongpu depression from paleontologic and geochemical marks

    從古生物和地球化學標志看東濮凹陷早第三紀的海侵事件
  12. The question whether transgression happened in paleogene of bohai bay basin has been discussed for more than 20 years, yet it was not resolved

    摘要有關渤海灣盆地古近紀是否發生過海侵的問題爭論了二十多年，至今尚無定論。
  13. In studied areas, reefs of western areas grew bigger in dimensions than those of the eastern, and the strata in which caning reefs became upper

    鄂西渝東區生物礁從西往東逐漸增大，發育層位逐漸抬升，與由東向西的海侵有關。
  14. In the late permian and triassic, the basin underwent once again a large - scale transgression, and the depositional environment was shelf sea with delta locally

    晚二疊世三疊紀盆地又經歷了一次大的海侵， ?淺海陸棚環境，局部?海陸過渡三角洲相。
  15. The top sediment above 1. 8m depth was referred to be the deposit under the cold water mass since 9. 7kabp. in the middle southern yellow sea. q - mode factor analysis was employed on 98 samples and 33 benthic foraminiferous species with relative abundance of more than 2 % in at least 3 samples and 5 varimax factors had been recognized as follows : factor 1 ( ammonia beccarii vars

    南黃海中部泥質區的ey02 - 2孔共揭示了氧同位素6期以來的海侵海退序列，該孔浮遊有孔蟲匱乏，說明黃海暖流對鉆孔所處南黃海中部冷渦泥質沉積區影響一直很弱，底棲有孔蟲中玻璃質殼占絕對優勢，比例為93 . 87 100 。
  16. The scholars insisting on transgression provided many markers such as mineralogy, lithology, paleoecology and geochemistry, but these makers are not completely the same as normal marine makers, moreover, the passageway and obviously increased makers of transgression have not been discovered, so " marine flooding ", " tsunami " and " terrestrial facies " appear, these viewpoints have coexisted for a long time

    盡管「海侵」論者提供了礦物學、巖石學、古生態學以及地球化學等多種標志，但是因為這些標志與標準海相標志比較，都有一定差別，而且至今沒有發現確實可靠的海侵通道和明顯的海相性遞增現象，所以又出現了「海泛」論、 「海嘯」論和「陸相」論。
  17. 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。
  18. Besides the aridity climate, the reason caused the high salinity of the lake water possibly was the frequent transgression in the early and middle permian

    造成湖泊水鹽度較高的原因，除了乾旱的氣候外，認為主要是由於早、中二疊世三塘湖地區頻繁的海侵作用造成的。
  19. Moreover, the system tracts in sequence are characterized by dualistic structure, namely transgressive - highstand system tracts, and tst > hst. the parasequences are divided into three types, which is respectively dominated by sandstones, mudstones, and shallowing - upward tidal flat system. and prograding sequence and retrograding sequence are composed of stacking parasequence set

    層序中體系域具有二元結構特徵，即海侵?高水位體系域，且tst hst ，準層序類型有三種，分別是以砂巖為主的準層序、以泥巖為主的準層序和以潮坪體系向上變淺的準層序。
  20. Penman considers that the question can be solved by 4 ways : the structural setting of bohai bay basin should be studied thoroughly to conclude possibility of the transgression ' s passageway. reliability of marine makers provided should be newly considered. new and exclusive evidences are required. similar sediment traps in correlative strata abroad are collected to research contrastively

    幾種觀點長期並存，筆者認為要解決這一問題，可以從四方面入手：深入研究渤海灣盆地的構造背景，推斷海侵通道存在的可能性；進一步釐定已有的海相標志的準確性；尋求新的、唯一的能區分海陸相成因的證據；搜集國外在相關層位元有類似沉積的地區，進行對比研究，並探索其成因。
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