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- A Near-Annual Pacific Ocean Basin Mode. 一個(gè)接近全年的太平洋海域模型。
- This supercontinent will have a small ocean basin trapped at its center. 該超大陸將捕獲一個(gè)小洋盆居于其中心。
- Jurassic and Cretaceous, the marginal ocean basin was in the stage of ocean crust evolution and had a setting similar to mid-ocean ridge. 侏羅-白堊紀為洋盆洋殼演化期,處于類(lèi)似洋中脊的構造環(huán)境。
- They are colliding. The plate carrying the ocean basin, because it is heavier, dives beneath the plate carrying the continent. 它們碰撞了。攜帶海洋盆地的板塊,因為比較重,潛入到攜帶大陸的板塊下。
- The braided channel turbidite of middle basin floor fan is characterized by gray and green-grayish sandstone and conglomerate and graveled sandstone with grain-se... 根據預測的砂體,結合構造和生油條件,可以確定勘探巖性油氣藏的有利目標。
- General features of ocean. Movement of ocean: wave, tides and ocean current. Eros ional and depositional coast. Continental margin and ocean basin. 海洋的一般特征。海洋的運動(dòng):波浪、洋流和潮汐。侵蝕型海岸和沉積型海岸。大陸邊緣和洋盆。
- It is concluded that there is a former island arc in central Altyn Tagh and an ocean basin in the north of the old island arc before Mesoproterozoic Era. 由此表明,在中元古代以前中阿爾金地塊可能是一個(gè)古島弧,在古島弧的北側還存在有一個(gè)古大洋盆地(或古弧后盆地)。
- The mineralization is related to the ocean basin closure in the Lower Permian,the moyite of the late magmatic evolution of the post-collision high-kalium granitoid. 成礦與早二疊世洋盆閉合,后碰撞高鉀鈣堿性花崗巖類(lèi)巖漿演化晚期的鉀質(zhì)花崗巖有關(guān)。銅礦(化)體呈細脈浸染狀產(chǎn)在鉀質(zhì)花崗巖的內外接觸帶內。
- In this study, Love wave dispersion data of 117 selected wave paths crossing the Pacific ocean basin are determined by applying the MF-FTAN technique to SRO/GDSN long period data. 應用現代適配濾波頻時(shí)分析技術(shù)對SRO/GDSN長(cháng)周期面波記錄進(jìn)行處理,獲得穿過(guò)太平洋盆地的117條波路徑的勒夫波頻散數據。
- The footwall rocks are deposited near the vent of a basin that is controlled by the activity of growth fault, similarly to cherts deposited near the ridge of a modern ocean basin. 礦體底板、頂板與頂板上覆地層中硅質(zhì)巖的沉積環(huán)境不同.;礦體底板硅質(zhì)巖沉積于受同生斷裂控制的熱水噴口的附近;類(lèi)似于洋中脊附近環(huán)境下沉積的硅質(zhì)巖;
- By far the greater part of the hydrosphere, of course, is the ocean basins. 海域無(wú)疑是水圈中的最大部分。
- The difference accounts for the existence of continents and ocean basins. 這種差別解釋了大陸和海洋盆地存在的原因。
- Basin floors generated at different times will exhibit a hierarchical sequence of crustal structure and epeirogenic behaviour. 不同時(shí)期生成的盆地底板,將顯示地殼構造的等級次序和造陸性質(zhì)。
- They dropped their net to the floor of the ocean. 他們把網(wǎng)下到海底。
- This indicates that volcanism in the Yaiba Formation took place in the Middle Jurassic Bajocian Stage and proves that the early Middle Jurassic was an important stage in the formation of the Neo Tethys ocean basin. 表明葉巴組的火山活動(dòng)發(fā)生在中侏羅世巴柔期,中侏羅早期是新特提斯(Neo?Tethys)洋盆形成的重要階段。
- Don't scrape your feet on the floor. 別用腳蹭著(zhù)地板。
- The tables are firmly fixed to the floor. 桌子都牢牢地固定在地板上。
- The Yangtze landmass collided with North China landmass due to Caledoniansubduction which happened after the ocean basin closed with Paleotethys subduction atEarly Palaeozoic. At last it developed Caledonian orogeny and caused borderland basinreversing. 早古生代洋盆隨原特提斯的消亡,經(jīng)加里東期的俯沖,揚子地塊與華北地塊碰撞,最終形成加里東俯沖造山帶,由此導致陸緣盆地的反轉。
- When ocean basin closes and remanant ocean crust intrudes into continental crust by tectonics, both the remnant ocean crust and the continental crust made up the ophiolitic melange belt. 摘要當洋盆閉合洋殼殘片構造侵位于陸殼之上時(shí),共同組成蛇綠混雜巖帶。
- Oceanic subduction-type eclogite in the Lhasa block, Tibet, China:Remains of the Paleo-Tethys ocean basin? 青藏高原拉薩地塊中的大洋俯沖型榴輝巖:古特提斯洋盆的殘留?