海槽 的英文怎麼說
中文拼音 [hǎicáo]-
The three - dimensional topography figures of major typical hydrothermal regions are drawn on the basis of field - measured bathymetric data of the okinawa trough and collecting a large number of data on bathymetry, multibeam and seismic profiles of other major typical hydrothermal regions
在沖繩海槽熱液活動區實測水深資料的基礎上，廣泛收集了其他典型熱液活動區的水深、多波束、地震剖面等資料，據此繪制出主要典型熱液活動區的三維地形圖。From the late middle ordovician to the end of ordovician, the cephalopods, gastropods and corals in the erlangping trough, and the conodonts, coral, brachiopods, cephalopods as well as trilobites in the xichuan shelf were from the north china province
在中奧陶世晚期至奧陶紀末，二郎坪海槽的腹足類、頭足類和珊瑚與浙川陸棚的牙形石、珊瑚、腕足類、頭足類和三葉蟲均屬華北生物省。From the middle devonian to the early carboniferous, the spores of the shishuyuan trough in the northern part of eqm and those of the nanwan trough in the southern part of eqm belonged to the south china province, and the late devonian corals, brachiopods, plants, and the early carboniferous fusulinids of the xichuan shelf were from the south china province
在中泥盆世至早石炭世，東秦嶺北部柿樹園海槽與東秦嶺南部南灣海槽的孢子及浙川陸棚的晚泥盆世珊瑚、腕足類和古植物及早石炭世（蟲? ）屬華南生物省。From the cambrian to the early middle ordovician, the cambrian radiolaria and the early ordovician conodonts of the erlangping trough in the northern part of eqm, and the cambrian trilobites and early ordovician conodonts as well as cephalopods of the northern xichuan shelf in the southern part of eqm belonged to the south china province, while the cambrian trilobites and the early ordovician conodonts of the southern xichuan shelf belonged to the south china province with some elements of the north china province
在寒武紀至中奧陶世早期，東秦嶺北部二郎坪海槽的寒武紀放射蟲和早奧陶世牙形石與東秦嶺南部浙川陸棚北部的寒武紀三葉蟲、早奧陶世牙形石和頭足類屬華南生物省，而浙川陸棚南部的寒武紀三葉蟲和早奧陶世牙形石屬于華南生物省，兼有華北生物省分子。Holocene tephra deposits in the northern okinawa trough
沖繩海槽北部的全新世火山碎屑沉積Grain - size variations of terrigenous sediment sequences in the south okinawa trough
沖繩海槽南部沉積層序的粒度特徵Many research such as clay minerals, suspend in the sea, the grain size trend analysis of surface sediment, poc 6 cu and 8 c13 in bottom sediments etc. showed that : the yellow sea warm current divided the south yellow sea into two, the terrestrial material of modern sediment on the west shelf plain mainly came from the modem yellow river suspend carried by the alongshore current, and the sediment difference between the west and east side of yellow sea trough was represented by the sedimentation thickness in postglacial period, sedimentation stratum, and oxygen isotope record
粘土礦物、碳酸鹽、粗碎屑、海域懸浮體、表層沉積物粒度趨勢分析、 poc c ~ （ 13 ）及底質沉積物的c ~ （ 13 ）等多方面研究表明：以黃海暖流為主導，南黃海堆積陸架平原西側現代沉積物陸源物質主要源於黃海沿岸流攜帶的現代黃河懸移物質，黃海槽東西兩側的沉積差異主要表現在冰消期以來沉積厚度、沉積層序、氧同位素記錄上。The oceans have life at all depths, even in the deepest trenches.
在海洋各種深度都有生命，連最深最深的海槽里都還有呢。The water from the west of cheju island approximately contributes 13 % of total transport of tsushima warm current through korea strait
渤海黃海的特徵像一個淺的湖泊，黃海暖流通過深海槽影響該區的環流。The provenance of the sediment in middle okinawa trough during the last glacial maximum is the shelf of the east china sea. the characteristics of elemental geochemistry ascertain that the sediment was derived from the paleo - changjiang river
末次盛冰期沖繩海槽中部陸源物質來源於東海陸架，元素地球化學特徵顯示這些沉積物主要來源於古長江的入海物質。During the early silurian, the corals of the erlangping trough and the graptolites of the xichuan shelf belonged to the south china province
在早志留世，二郎坪海槽的珊瑚與浙川陸棚的筆石屬華南生物省。Elemental geochemical records of modern seafloor hydrothermal activities in sediments from the central okinawa trough
沖繩海槽中部現代海底熱液活動在沉積物中的元素地球化學記錄The mariana trough is an actively opening back arc basin that lies at the eastern edge of the philippine sea plate, and in the transition time from rift to sea floor spreading
位於菲律賓板塊和太平洋板塊之間的馬里亞納海槽，處于弧后張裂向海底擴張的過渡階段，是深入研究板塊運動與弧后擴張動力學過程的理想地區。From the late carboniferous to the end of permian, the spores of the shishuyuan trough were from the north china province, and the marine sediments were absent in the southern part of eqm
晚石炭世至二疊紀末，柿樹園海槽的孢子見于華北生物省，東秦嶺南部缺乏海相沉積。The new network has detected some shallow earthquakes along the trough.
新臺網已記錄到一些沿海槽發生的淺源地震。The marine hydrocarbon source rock is generally carbonate rock of isolated platforms and interplatform troughs in the baise basin
摘要百色盆地海相烴源巖主要為孤立臺地和臺間海槽碳酸鹽巖。Target drilling sites include areas where the mantle has been brought closest to the surface by tectonic action or where the crust is relatively thin, such as the nankai trough off japan ' s pacific coast
鉆探的目標包括了某些因板塊運動而使地函接近地表的區域，或是地殼相對較薄的地方，例如日本太平洋海岸外的南海海槽。The characteristics of the sediment from the okinawa trough are controlled by provenance. some major and trace elements vs. al scatter plots show clearly the evolution stage of the sedimentary supply to okinawa trough
沖繩海槽沉積物的化學特徵受控於物質來源，用元素對al的散點圖可以明顯顯示沖繩海槽物源供應具有階段性變化的特點。According to the topography and geomorphology, the abnormality of gravitation and magnetic field, characteristics of crust structure and the environment of lithospheric dynamics in the northwestern of the south china sea, the seismic profiles were explained across the yinggehai basin and xisha trough
摘要本文根據南海西北部殼體的地形地貌、重磁場異常和地殼結構特徵和巖石圈動力學環境，對穿過鶯歌海盆地和西沙海槽的地震剖面進行解釋。Concentrations of total suspended matter ( ctsm ) is unanimous with observational data and other scholars " researching results. the distribution of ctsm is higher along coast than other areas there is a tongue - like zone with high ctsm from north to southeast. the transport simulation result reveals that sm can spread to the okinawa trough for enough sea water mixing in winter. but in summer. sm can not traverse the big water barrier of kushino for different circulation character. this difference is probably related to the shifting n - s monsoon
懸浮體輸送表明，在冬季，懸浮體除了在陸架上發生擴散外，由於海水的強烈混合作用和環流的季節性變化，部分中、底層懸浮體可擴散至沖繩海槽甚至西太平洋;在夏季，由於海水層化及夏季環流特徵，懸浮體基本不能穿越黑潮這一水障，這一差異可能是由於季風和不同環流特徵所引起的。分享友人