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- Through the low stress subduction of oceanic plate, crustal extension has dominated in Southeastern China. 晚白堊世以來(lái)大洋板塊屬于低應力型俯沖，拉張是東南部主構造。
- 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. 其結果表明;來(lái)自太平洋板塊相對歐亞板塊的俯沖所形成的構造力;控制了從華北地區到南北地震帶北段的應力場(chǎng).
- Please tell me the mechanics of how the Pacific Ocean plate moves. 請你告訴我太平洋板塊怎么運動(dòng)的機制。
- Subduction of Paleo-Asian Ocean plate 古亞洲洋板塊俯沖
- Tsai, Y.-B.(1979) Plate subduction and the Plio-Pleistocene orogeny in Taiwan. Petroleum Geology of Taiwan, 15, 1-10. 蔡義本(1978)臺灣地區板塊隱沒(méi)作用與蓬萊造山運動(dòng)之關(guān)系。臺灣石油地質(zhì)，第15號，第1-10頁(yè)。
- Forming of the force of center uplifting and lateral compressing depends on the size of dip angle of plate subduction. 中央隆升力和側向擠壓力的形成取決于板塊俯沖傾角的大小。
- First, the Indian plate subduction to Asia, resulting in rapid uplift of the Qinghai-Tibet Plateau. 一是印度板塊向亞洲板塊俯沖，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. 圣海倫火山在1980年的噴發(fā)是板塊沉降的直接結果。
- The tectonism of North China platform had the multistage plate subduction and collision which form a favourable condition for gold mineralization. 華北地臺區構造作用具有多期次板塊俯沖和碰撞，是金礦形成的有利條件。
- The Pacific Ocean plate , Eurasian plate , Indian Ocean plate , Africa plate , America plate and Antarctica plate. 太平洋板塊、歐亞板塊、印度洋板塊、非洲板塊、美洲板塊和南極洲板塊。
- Theoretically it is to locate in continent plate and ocean plate intersectant place . 理論上屬位于大陸板塊和大洋板塊交匯處。
- 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;太平洋板塊俯沖方向由NNW轉為WNW;右旋應力場(chǎng)控制了盆地東部始新世斷拗的發(fā)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. 贊岐巖集中出現在晚太古代 (<3.;0Ga);表明板塊消減作用可能在 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. 任何假設的能推動(dòng)或拉動(dòng)大洋板塊的力，會(huì )很快因克服在其下靜態(tài)的熱體地幔上滑動(dòng)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. 湘黔地區內生金礦的形成和時(shí)空分布,受中晚元古代以來(lái)發(fā)育于川中古陸東南活動(dòng)邊緣古板塊俯沖帶制約。
- 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，雖然一個(gè)洋殼的上部是晶體，下面卻顯示了逐步的變化，即當溫度和壓力隨深度增加時(shí)，便從固體到可塑體再到粘滯的液體。
- 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. 摘要南海處于歐亞、太平洋、印-澳三大板塊的交匯處，是在太平洋板塊俯沖和印度板塊與歐亞板塊碰撞共同作用下經(jīng)過(guò)擴張形成的。
- 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. 那底崗日組火山巖應是與板塊消減作用無(wú)關(guān)的,類(lèi)似于拉張環(huán)境的靠近大陸邊緣的類(lèi)似于裂谷的環(huán)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. 因此雖然一個(gè)洋殼的上部是晶體，下面卻顯示了逐步的變化，即當溫度和壓力隨深度增加時(shí)，便從固體到可塑體再到粘滯的液體。
- 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. 因此雖然一個(gè)洋殼的上部是晶體，下面卻顯示了逐步的變化，即當溫度和壓力隨深度增加時(shí)，便從固體到可塑體再到粘滯的液體。
