oceanic island 中文意思是什麼
oceanic island
解釋
大洋島-
Flabellifera is one of the most important suborders of isopoda, and the commonest isopods of predominant marine provenance. the materials examined were obtained mainly by national oceanic investigations such as " the comprehensive oceanographic survey ( 1958 - 1960 ) ", " china vietnam comprehensive survey to beibu gulf ( golf of tonkin ) ( 1959 - 1960, 1962 ) " and " china germany marine biological expedition to hainan island " ( 1990, 1992 )
中國科學院海洋研究所從50年代以來進行了若干次海洋生物考察，如「全國海洋綜合調查（ 1958 ? 1960年） 」 、 「中越北部灣海洋綜合調查（ 1959 - 1960 ， 1962年） 」及「中德海南島生物聯合調查（ 1960 ， 1962年） 」等，獲得了大量的等足類標本。 -
The early tertiary alkali basalts from yangyuan which contain abundant mantle xenoliths exhibit very homogeneous sr - nd isotopes with snd = 5. 5. their pb isotopes are similar to those of the depleted mantle ( dm ) and their trace element characteristics resemble those of oceanic island basalts ( oib )
含幔源包體的陽原早第三紀堿性玄武巖具有均一的sr - nd同位素組成（ nd 5 . 5 ） ，其pb同位素組成與虧損地幔（ dm ）相似。 -
Establish and genesis of oceanic island basic volcanic rock early carboniferous in northern of daxing ' anling
大興安嶺北段早石炭世洋島型玄武巖的確立及成因意義 -
In the light of tectonic evolution stage and metallogenesis, these metallogenic system ( assemblage ) could be classified as follows : ( 1 ) the pre - divergent metallogenic system in the southwest margin of north china paleocontinent in the archean - meso proterozoic : dongdashan iron, jinchuan nickel - copper. ( 2 ) the divergent metallogenic system in the northern margin of the qaidam paleoplate in the middle - late proterozoic : huashugou - liugouxia iron. ( 3 ) the metallogenic system in the active margin in the early paleozoic : the metallogenic assemblage in the island arc - rift in the early stage ( baiyinchang - qingshuigou copper - polymetallic ) ; the metallogenic assemblage in island arc in the middle - late stage ( honggou - jiaolongzhang copper - polymetallic ) ; the back - arc extensional basin ( zhuzhuiyaba - jiugequan - shijuli copper ) ; the metallogenic assemblage in connection with subduction and magmatic - hydatogenesis ( taergou - xiaoliugou wolfram ; huashugou - liugouxia copper ; dadonggou - diaodaban lead - zinc ) ; the metallogenic assemblage is related to the oceanic crustal shards ( dadaoerji chromite ; yushigou chromite ). ( 4 ) the metallogenic system has something to do with collision - type orogeny : the metallogenic assemblage in foreland basin ( tianlu copper ) ; the metallogenic assemblage with the intracontinental orogeny and ductile shear ( hanshan - yingzhuishan gold )
根據構造發展階段和成礦作用特點，確定本區成礦系統及組合如下： （ 1 ）華北板塊西南邊緣太古宙中元古代裂解期前成礦系統：東大山鐵成礦組合，金川鎳銅成礦組合； （ 2 ）柴達木板塊北緣中、新元古代裂解成礦系統：樺樹溝柳溝峽鐵成礦組合； （ 3 ）加里東期活動大陸邊緣成礦系統：早期島弧裂谷成礦組合（白銀廠清水溝銅及多金屬成礦組合） ，中、晚期島弧成礦組合（紅溝蛟龍掌銅及多金屬成礦組合） ，弧后擴張盆地成礦組合（豬咀啞巴九個泉石居里銅及多金屬成礦組合） ，與俯沖作用有關的巖漿熱液成礦組合（塔爾溝小柳溝鎢成礦組合，樺樹溝柳溝峽銅成礦組合，大東溝吊大坂鉛鋅成礦組合） ，洋殼殘片成礦組合（大道爾吉鉻成礦組合，玉石溝鉻成礦組合） ； （ 4 ）碰撞造山成礦系統：前陸盆地成礦組合（天鹿銅成礦組合） ，陸內造山韌性剪切成礦組合（寒山鷹咀山金成礦組合） 。 -
At the beginning of season 1, a plane crash strands the surviving passengers of oceanic flight 815 on a seemingly deserted tropical island, forcing the group of strangers to work together to stay alive
第一季伊始，一次墜機事故將815號跨洋航班中生還下來的乘客滯留在了一座看似荒棄的熱帶島嶼上，迫使這群陌生人為了生存並肩作戰。 -
What makes this island special is that it is the only oceanic island not connected to the continental shelf in malaysia rising 2, 000 feet 600 meters on a limestone pinnacle that mushrooms out near the surface. pulau sipadan have the largest variety of soft corals in the world. turtles swim and frolic freely in the waters around sipadan and divers will find lobster, barracudas, beautiful coral fishes and sometimes even sharks swimming by
其蘑菇形石柱島，深入海底1000米，露出地面的淺水處，各式鹹水魚成群，不諳泳術只玩浮潛，也夠大開眼界深諳潛水者，當然是到深海峭壁探險，在水深30米跟成群大海鐵頭魚鯊魚及東星斑等來個大合照。 -
The internal mineral separates and whole - rock sm - nd isochron age for gabbro dikes from the dangqiong ophiolite is 373 ? 8ma, inferring a magmatic activity during late devonian, which end ( t ) = + 3. 3 suggests that its tectonic setting was probably oceanic island
其nd （ t ） = + 3 . 3 ，認為其時形成環境為洋島，可能代表了新特提斯蛇綠巖形成時所攜帶的古老洋殼。 -
Its petrochemical characteristics show that the volcanics was formed in oceanic island tectonic environment
巖石化學特徵表明火山巖形成於洋島構造環境。
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