地幔熱點 的英文怎麼說
中文拼音 [demànrèdiǎn]
地幔熱點
英文
mantle hot spot-
Based on affirming mantle plume hypothesis, the authors introduce several 2d or 3d simulation experiments about ridge - plume ( hotspot ) interaction and some examples of hotspot - ridge interactions existing in the three oceans
研究洋脊熱點之間的相互作用對于揭示地幔動力學、熱點附近洋殼構造的演變以及與熱點密切相關的洋中脊處的巖漿熱液活動具有重要的意義。Hotspot is a window to understand mantle plume hypothesis and dynamics of mantle plume, and the area where ridge interactions with hotspot is the best place to directly find out relationship between plate tectonics and mantle plume
摘要地表熱點是認識地幔柱假說以及地幔柱動力學的窗口,發生在洋脊與熱點之間的相互作用則是了解地球上兩大動力系統(板塊構造和地幔柱)的直接聯系的最有利地區。Applying system theory to study mineralized belt or concentrated area has been a hot topic recently. this paper applied new theory of modern seafloor hydrothermal sedimentary minerlization, sequence stratigraphy, mantle plume or hotspot and metallogenic series to study systematacially characteristic of geology and geochemistry of seafloor hydrothermal sedimentary deposits and hydrothermal sedimentary - rebuilded deposits and gold deposits
論文應用現代海底熱水沉積成礦研究成果、層序地層學、地幔熱柱或熱點理論及礦床成礦系列理論等,對本區熱水沉積型鉛鋅(銀)礦床、熱水沉積-改造型鉛鋅(銀)礦床和金礦床進行了詳細的地質地球化學研究。Different zone block in the basin has different construction. cold and heat shells are at intervals. crust behaves as hot, light, flowing and thicker, however, mantle behaves as cold, weight, and harder, multi - phase and deep mantle
盆地不同區塊熱結構不同,為冷、熱殼相間,地殼表現為熱、輕、軟、流、厚殼,地幔表現為冷、重、硬、多相、深幔的特點。It is further pointed out that simulation experiments combined with geology, petrology, geochemistry and geophysics ( especially for high resolution seismic technique ) in studying mantle ( hotspot ) - ridge interaction will play an important role in such reseaches as plume - ridge interactions
在肯定地幔柱假說的基礎上,對洋脊地幔柱(熱點)的模擬實驗以及三大洋中不同擴張脊與熱點相互作用的最新研究作了系統的介紹和評述,指出室內模擬實驗以及地質學、巖石學、地球化學和地球物理學(特別是高解析度的地震技術)的結合研究將是本領域研究的發展趨勢。The scientists who discovered the “ hot spot ” say that the crust beneath the new ice stream is very thin, and suggest that hot magma from the earth ' s mantle came close enough to the surface to cause the ice stream to form
科學家們發現"熱點" ,指出,地殼下面的新冰流非常薄,並指出,從地球的地幔噴出的熱巖漿險些夠到地表造成冰流形成。分享友人