1) double-subduction zone
双俯冲带
1.
Before Upper Cretaceous, the Paleo-Minzhe-the Paleo--Korea trench--arc system and the Ryukyu trench-arc system constitute the old double-subduction zone.
前晚白垩世，闽浙-朝鲜二古沟-弧系和琉球沟-弧系组成古双俯冲带，东海微板块的构造运动受制于双俯冲带的作用。
2) subduction belt
俯冲带
1.
Both of them have effect on lithosphere and subduction belts simultaneously.
为了揭示地幔柱构造与板块构造的内在关系 ,针对地幔柱独特的地球物理和地球化学特征 ,通过与板块构造的对比 :阐明了两者虽然在许多方面存在着矛盾 ,但在诠释岩石圈的解体和俯冲带的演化过程中都发挥着重要的作用 ;拆沉的冷板片聚集产生了超级冷地幔柱 ,由此导致了超级热地幔柱 ,冷热两个超级地幔柱的活动又控制了板块的运动和发展。
3) Subduction zone
俯冲带
1.
Progresses of the researches and the causing mechanisms on the double seimic zones within the subduction zones around the pacific ocean;
环太平洋俯冲带内双地震带及其成因机制研究进展
2.
Relationship between dehydration of serpentine and intermediate-focus earthquakes in oceanic subduction zones.;
蛇纹石脱水与大洋俯冲带中源地震(70~300km)的关系
3.
Since the middle and late Caledonian, the two basins beg3n opening and closins,and three subduction zones, two collision zones andseven island arc belts were formed.
从加里东中晚期开始，两个洋盆边拉张达消减，形成３条俯冲带、２个对接带和７个岛弧带，最后于华力西中期沿克拉表里、康古尔塔格两个对接带闭合。
4) A-subduction zone
A-型俯冲带
5) supra subduction zone
上俯冲带
6) Paleo subduction zone
古俯冲带
补充资料：2,2-双氯甲基-三亚甲基-双[双(2-氯乙基)磷酸脂]
CAS：38051-10-4
分子式：C13H24Cl6O8P2
中文名称：2,2-双氯甲基-三亚甲基-双[双(2-氯乙基)磷酸脂]
英文名称：2,2- bis(chloromethyl)-trimethylene bis[bis(2-chloroethyl)phosphate]
phosphoric acid, 2,2-bis(chloromethyl)-1,3-propanediyl tetrakis(2-chloroethyl)
2,2-bis(chloromethyl)trimethylene bis(bis(2-chloroethyl)phosphate)
2,2-bis(chloromethyl)-1,3-propanediyltetrakis(2-chloroethyl)phosphate
分子式：C13H24Cl6O8P2
中文名称：2,2-双氯甲基-三亚甲基-双[双(2-氯乙基)磷酸脂]
英文名称：2,2- bis(chloromethyl)-trimethylene bis[bis(2-chloroethyl)phosphate]
phosphoric acid, 2,2-bis(chloromethyl)-1,3-propanediyl tetrakis(2-chloroethyl)
2,2-bis(chloromethyl)trimethylene bis(bis(2-chloroethyl)phosphate)
2,2-bis(chloromethyl)-1,3-propanediyltetrakis(2-chloroethyl)phosphate
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条