| 1. | The velocity difference between the two layers of the lower crust is not obvious
下地壳的两构造层速度差异不明显。 |
| 2. | Tsunami : a great sea wave produced especially by submarine earth movement or volcanic eruption
海啸:由水下地壳运动或火山爆发产生的巨大波涛。 |
| 3. | ( 3 ) the mineral source was provided by both lower crust , upper mantle and upper crust , obviously from crust - mantle mixing
( 3 )矿田中的成矿物质的不仅来自于下地壳和上地幔，而且还来自于上地壳，具有壳幔混合特征。 |
| 4. | It is also found that the telluric heat flow value is stripped from south to the north and dispersed from east to the west
下地壳电性结构和速度结构明显具有纵向分层和横向分块的特点，其热流密度值具有明显的南北条带性和东西分块性。 |
| 5. | The evidence that the fluid comes from the down earth ' s crust and mantle did not found by studying fluids ( water , glued thing and natural gas ) in the basin
川西前陆盆地流体(水、胶结物和天然气)的研究，未发现来自下地壳及地幔的深部流体地球化学证据。 |
| 6. | " but at the same time , a horizontal pulling power inside the lower continental crust and mantle of the earth counteracts this upward movement , " said bian
“但同时，从下地壳一直到地幔上部在产生一种东西拉张的力量，这种拉力对喜马拉雅山的继续升高起到了阻碍作用。 ” |
| 7. | " but at the same time , a horizontal pulling power inside the lower continental crust and mantle of the earth counteracts this upward movement , " said bian
“但同时，从下地壳一直到地幔上部在产生一种东西拉张的力量，这种拉力对喜马拉雅山的继续升高起到了阻碍作用。 ” |
| 8. | According to measurements made by scientists in 2005 , the altitude of mount qomolangma is 8844 . 43 metres , 3 . 70 metres lower than the figure obtained in 1975
“但同时，从下地壳一直到地幔上部在产生一种东西拉张的力量，这种拉力对喜马拉雅山的继续升高起到了阻碍作用。 ” |
| 9. | The geochemical signatures show that the volcanic rocks in the jingzhushan formation were formed in the island - arc environment as crustal thickening - melting products in a compressional tectonic setting
地球化学特征表明，竟柱山组火山岩形成于岛弧构造环境，是挤压背景下地壳增厚熔融的产物。 |
| 10. | Due to the subduction of pacific palte under eurasian in early cretaceous , at about 140 ma , fast collapse ( delamination ) took place and the mantle plume emerged , both resulted in the large - scale crustal extension in ludong
3 、富集地幔源区( em1 )的产生是俯冲并熔融的扬子下地壳物质进入华北岩石圈地幔并与之相互交代作用形成的。 |
