摘要
国际大洋钻探计划（ＯＤＰ）自 １９８３年以来，已成功地实施了 ６６个航次的深 海钻探作业，获取钻探岩芯逾 １００ ０００ｍ。在关于大陆边缘的构造演化，海洋地壳的形 成与发展，地壳流体循环和壳幔相互作用，海洋沉积结构和古海洋学，地球大气圈、水 圈、冰圈、生物圈的长期变化等众多研究领域取得了一系列重大科研成果。对世界地 球科学的发展具有重要的导向作用。 中国已决定从１９９６年起加入国际ＯＤＰ组织，中国海域深海钻探可望成为现实。 ＯＤＰ涉及固体地球科学各个领域，必将对中国地球科学的发展起到巨大的推动作 用。
Over the past 11 a, the Ocean Drilling Program has completed 66 internationally staffed expeditions. JOIDES Resolution, the scientific drill ship of ODP, has travelled in the Pacific, Atlantic and Indian Ocean. Significant results of ODP drilling during this time have been obtained by investigating the tectonic evolution of passive and active continental margins, origin and evolution of oceanic crust, origin and evolution of marine sedimentary sequences, and cause of long-term changes in Earth's atmosphere, oceans, cryosphere, biosphere and magnetic field. China has divided to be a member country since 1996. The first drilling hole will be coming in the sea area off China. Based on the drilling data of ODP. Chinese solid earth science will make great progress very quickly.
出处
《海洋科学》
CAS
CSCD
北大核心
1996年第3期3-14,共12页
Marine Sciences
基金
中科院院长基金
