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- Through the low stress subduction of oceanic plate, crustal extension has dominated in Southeastern China. 晚白垩世以来大洋板块属于低应力型俯冲,拉张是东南部主构造。
- The results indicate that the tectonic forces from the subduction of the Pacific Ocean plate underneath the Eurasian plate control the stress field in the region from North China to the northern part of the North- South Seismic Belt. 其结果表明;来自太平洋板块相对欧亚板块的俯冲所形成的构造力;控制了从华北地区到南北地震带北段的应力场.
- Please tell me the mechanics of how the Pacific Ocean plate moves. 请你告诉我太平洋板块怎么运动的机制。
- Subduction of Paleo-Asian Ocean plate 古亚洲洋板块俯冲
- Tsai, Y.-B.(1979) Plate subduction and the Plio-Pleistocene orogeny in Taiwan. Petroleum Geology of Taiwan, 15, 1-10. 蔡义本(1978)台湾地区板块隐没作用与蓬莱造山运动之关系。台湾石油地质,第15号,第1-10页。
- Forming of the force of center uplifting and lateral compressing depends on the size of dip angle of plate subduction. 中央隆升力和侧向挤压力的形成取决于板块俯冲倾角的大小。
- First, the Indian plate subduction to Asia, resulting in rapid uplift of the Qinghai-Tibet Plateau. 一是印度板块向亚洲板块俯冲,造成青藏高原快速隆升。
- The eruption of Mount St. Helens in 1980 was the direct result of plate subduction. 圣海伦火山在1980年的喷发是板块沉降的直接结果。
- The tectonism of North China platform had the multistage plate subduction and collision which form a favourable condition for gold mineralization. 华北地台区构造作用具有多期次板块俯冲和碰撞,是金矿形成的有利条件。
- The Pacific Ocean plate , Eurasian plate , Indian Ocean plate , Africa plate , America plate and Antarctica plate. 太平洋板块、欧亚板块、印度洋板块、非洲板块、美洲板块和南极洲板块。
- Theoretically it is to locate in continent plate and ocean plate intersectant place . 理论上属位于大陆板块和大洋板块交汇处。
- At late Eocene, the Pacific Plate subduction direction were changed from NNW to WNW, and the development of Eocene fault depressions in the eastern part of the basin were controlled by dextral stresses. 始新世晚期;太平洋板块俯冲方向由NNW转为WNW;右旋应力场控制了盆地东部始新世断拗的发育.
- The early sanukite has only been found in Late Archaean (<3.0 Ga), probably indicating that the modern style plate tectonics was initiated at that time and that plate subduction came to be an important geological process only after 3.0 Ga. 赞岐岩集中出现在晚太古代 (<3.;0Ga);表明板块消减作用可能在 3
- Any hypothetical force postulated to either push or pull oceanic plates would be quickly dissipated overcoming the friction of sliding over a static fluid mantle beneath. 任何假设的能推动或拉动大洋板块的力,会很快因克服在其下静态的热体地幔上滑动的摩擦力而被消散。
- The formation and distribution of gold mineral deposits in Hunan and Guizhou are restrained by the old plate subduction zone developing on the active continental margin in the middle of Sichuan Oldland of mid-lat Proterozoic. 湘黔地区内生金矿的形成和时空分布,受中晚元古代以来发育于川中古陆东南活动边缘古板块俯冲带制约。
- Thus,while the upper surface of an oceanic plate is a crystalline solid ,the underside exhibits a gradual phase change,from solid to plastic to viscous liquid as the temperatures and pressures increase with depth. 因此,虽然一个洋壳的上部是晶体,下面却显示了逐步的变化,即当温度和压力随深度增加时,便从固体到可塑体再到粘滞的液体。
- South China Sea, which locates within the Pacific-Oeanic Plate, the India Plate and Eurasia Plate, is the result of Pacific-Oceanic Plate subduction and the collision of India Plate and Eurasia Plate. 摘要南海处于欧亚、太平洋、印-澳三大板块的交汇处,是在太平洋板块俯冲和印度板块与欧亚板块碰撞共同作用下经过扩张形成的。
- Volcanic rocks in Nadigangri formation could be nothing to do with plate subduction,but it was formed in extensional environment near continental margin which might be similar to rift. 那底岗日组火山岩应是与板块消减作用无关的,类似于拉张环境的靠近大陆边缘的类似于裂谷的环境中。
- Thus while the upper surface of an oceanic plate is a crystalline solid, the underside exhibits a gradual phase change, from solid to plastic to viscous liquid as the temperatures and pressures increase with depth. 因此虽然一个洋壳的上部是晶体,下面却显示了逐步的变化,即当温度和压力随深度增加时,便从固体到可塑体再到粘滞的液体。
- Thus while the upper surface of an oceanic plate is a crystalline solid , the underside exhibits a gradual phase change, from solid to plastic to viscous liquid as the temperatures and pressures increase with depth. 因此虽然一个洋壳的上部是晶体,下面却显示了逐步的变化,即当温度和压力随深度增加时,便从固体到可塑体再到粘滞的液体。