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      深海
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  deep marine
     The basin experienced early deep marine semi deep marine flysch sedimentation and later continental molasses sedimentation and was subjected to three periods of tectonic deformations during its evolution. These were early solid plastic deformation, middle stage regional fold and sliding deformation and later complex deformation under thrust nappe and shearing mechanism
     该盆地经历了早期的深海—半深海复理石沉积和晚期的陆相磨拉石沉积 ,其演化过程中主要遭受了三期构造变形 ,即 :早期固态塑性变形 ,中期区域褶皱及走滑变形和晚期逆冲推覆、剪切机制下的复杂变形
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  “深海—”译为未确定词的双语例句
     and the Limestone Formation of the Upper Shujiaba Group formed in a bathyal to abyssal basin at the north margin of the West Qinling microplate in the Devonian.
     舒家坝群上部灰岩组形成于西秦岭微板块北缘半深海—深海盆地环境。
短句来源
     ⑤ abyssal- bathyal sediments composed of radiolarian siliceous rocks,turbidite and limestone.
     ⑤深海—半深海沉积,岩性为放射虫硅质岩、浊积岩、灰岩等。
短句来源
     The analysis of the characteristics of the profile, petrology, sedimentology and geochemistry show that the gravel came from the shallow water carbonate platform and was transported to the slope or bathyal zone as carbonate debris flow along the slope of margin of carbonate platform.
     剖面特征 ,岩石学、沉积学和地球化学特征的分析结果 ,显示了石灰砾岩的砾石来源于浅海碳酸盐台地 ,它们作为碳酸盐岩碎屑流的产物 ,沿着台地边缘的斜坡 ,被搬运到半深海—斜坡处再沉积。
短句来源
     The Lixian-Minxian foreland basin undertook abyssal-bathyal flysch deposition at its earlier evolution stage and continental molasse stage at its later evolution stage.
     礼岷前陆盆地经历了早期深海—半深海的复理石沉积阶段和晚期陆相磨拉石沉积阶段。
短句来源
     Toward the Colorful Deep Sea——Aesthetic Analysis on the Concise Style of Hemingway's Prose
     走向绚丽的深海——海明威散文简洁风格的审美解析
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  相似匹配句对
     Deep Sea Dynamic Sealing
     深海动态密封
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     NEW RECORDS OF GALATHEIDAE (CRUSTACEA, ANOMURA) FROM EAST CHINA SEA
     东海深海铠甲虾类
短句来源
     Coral-The Living Treasure In Deep Ocean
     深海的活宝珊瑚
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     NATIONAL TREASURE OF PRECIOUS CORAL IN DEEP SEA OF CHINA
     中国的国宝深海贵重珊瑚
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  deep marine
Fragments of the calcareous green alga Halimeda form a large part of the sediment in the fringing reef system and adjacent deep marine environments of Grand Cayman Island, West Indies.
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These sediments likely belong to an extensive, thick, deep marine cover of the St.
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According to previous works, geological features of the rocks on top of the anomalous wedge indicate that during the Cretaceous this zone constituted a deep marine environment which underwent important crustal thinning related to rifting.
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The red colour is due to presence of hematite pigment, and indicates oxidizing conditions during early diagenesis in a relatively deep marine environment.
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Deformation involved north-vergent thrust imbrication of the basement and the emplacement of allochthonous deep marine Triassic series over the Jurassic metasediments.
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         The present paper emhodies the results of investigations on the composition of fouling organisms of Yu-lin harbour and its seasonal variation. A comparison is made of the fouling organisms of this harbour with those of Amoy harbour in the respects of their composition, biomass and seasonal fluctuation.The dormanant fouling plants of Yu-lin harbour are: Enteromorpha clathrata, E. tubulosa, Ectocapus confervoides, Giffordia spp. and Sp(?)ridia filamentosa, and the dormanant fouling animals are: Hydroldes sp.,...
            本文报导榆林港附着生物的的种类组成及其季节变化,并从种类、附着量及附着季节等方面与厦门港的附着生物作比较。 榆林港最主要的附着生物是:滸苔、管滸苔、水云、褐茸藻及笼果藻等藻类;盤管虫、螺旋虫、(?)牡蠣、(?)合草苔虫及悉尼海(?)等动物,藻类月附着量9.5克/米~2,季附着量3.1克/米~2;动物月附着量5.8克/米~2,季附着量187.1克/米~2。种类多、附着期长、附着量少是榆林港附着生物的主要特点。 榆林港与厦门港附着生物的差异,反映了热带性和亚热带性港湾附着生物的特点;也表明了深海外港与河口内港(盐度及透明度不同)在生态上的意义。
文摘来源
         Eulalia bilineata Johnston, Eteone longa (Fabricius), Eunoe oerstedi Malmgren, Goniada maculata Oersted, Nephthys ciliata (O. F. Muller), 2V. caeca (O. F. Muller), Sphaero-syllis erinaceus Claparede, Grubea clauata (Claparede), Syllis armillaris (O. F. Muller), Onuphis (Nothria) iridescens (Johnson), Spio filicornis (O. F. Muller), Flabelligera affi-nis Sars, Stylarioides plumosa (O. F. Muller), Brada villosa (Rathke), Praxillella prae-termissa (Malmgren), Mellina cristata (Sars), M. elisabethae Mclntosh, A...
            1.黄海多毛类区系包含有中国沿岸特有地方性种,黄海和日本沿岸的特有地方性种,广温性热带暖水种,寒温带冷水种和广布种等不同性质成分。 2.值得提出的是太平洋东西两岸种在黄海的发现,计有19种。这些种的分布应该考虑不仅是由于历史的成因,在某种程度上幼体也许有可能随当前自日本沿岸流向美洲沿 岸的黑潮传布过去。多毛类有些种幼虫期很长,并且能随海流分布至深海(Thorson,1950)。 3.根据与邻近海区区系的比较,黄海多毛类与日本沿岸,特别是日本本州北部金华山附近的女川湾和松岛湾一带的区系最相近似,女川湾和松岛湾一带属亲潮寒流和黑潮暖流交汇区,因之在种类组成上不仅有来自南方的暖水种,同时,还有北方的冷水种,具有混合区系特征。黄海——本州北部应属同一地理区划。 4.黄海多毛类具有十分显著的混合区系特征,与日本的情况不同,黄海的暖水种多分布在潮间带,冷水种大部分在较深水域,井与深水区终年存在的冷水团有关。 5.黄海北部和中部应属北太平洋北温带和印度西太平洋热带区之间的过渡区。
文摘来源
         What causes the earth crust to move? This is a principal theoretical problem of the earth science and has been a point at issue among the geologists. In this paper, a new hypothesis is presented in respect of this problem-the hypothesis of density equilibrium ellipsoid. In support of this hypothesis, the writer puts forward his views on a series of geological phenomena, such as the formation of the Himalaya range, San Andres fault, geosynclines, deep-sea troughs, ε-type structuses, etc.
            地壳为什么会动?这一地学领域中的基本理论问题一直成为地学工作者探讨、研宄的中心,本文作者对此提出了新观点—“密度平衡椭球体”假说。根据这一新观点,作者对喜马拉雅山的形成,圣安德列斯断层、地槽、深海沟、山字型构造的形成等一系列重要地质问题提出了新看法。
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