| 1. | Continental plate boundary
大陆板块边界 |
| 2. | These nne and ne faults become a long transform fault system and formed a boundary between the eastern margin of china continental plate and philippine sea plate
这些北北东向和北东向断层形成一条巨长的转换断层系列，也是中国大陆板块东缘与菲律宾洋块的一条边界。 |
| 3. | This system plays an important role in the relative movement between the west pacific plate and eurasian continental plate . thus , the paleozoic structures had been modified
此断层系列对于西太平洋板块与欧亚板块之间的相对运动起重要作用，于是古生代构造带被改造。 |
| 4. | As africa was once joined to australia before the continental plates parted , similarities exist in the plants from the two continents , and many useful and drought - tolerant plants have even taken over and become pests
由于非洲与澳洲在大陆板块分开之前曾连在一起，所以这两个洲的植物在许多方面有相似之处，许多有用及耐旱的植物因为过度生长而变成了有害植物。 |
| 5. | The collision between continental plates is a key to understanding the evolution of continental dynamics . perhaps the most spectacular large - scale result of plate tectonics is the broad complicated zone of intracontinental convergence between eurasia and peninsular india following their collision at about 45 ma
大陆内部的陆-陆碰撞过程是大陆动力学的核心问题，青藏高原被视为印度板块与欧亚板块于新生代碰撞的结果，是典型的陆-陆碰撞带。 |
| 6. | In this case during paleozoic , nearly east west trending arc structures resulted from the interaction between china plate and siberian plate . in mesozoic the westward subduction of kula - pacific plate under the china continental plate resulted in the nne and ne trend structures ( duimadao fault , diaoyudao fault , okinawa fault , uplifts belts and subsidence belts ) as well as volcano - magmatic belts in eastern of china plate
本文所涉及近东西向展布的弧形构造形成于古生代时期中国板块与西伯利亚板块的碰撞带，而在中生代，中国板块下的kula - pacific板块向西俯冲导致了北北东向和北东向构造（如duimadao断层、 diaoyudao断层、 okinawa断层、隆起带和沉降带）以及位于中国板块东部的火山岩浆带。 |
