冲击波动态高压技术已成为人们研究、认识地球内部物质组成、状态及其性质的重要手段和方法之一,在固体地球科学研究中发挥着重要作用。
Shock compression has become an important method to advance our understanding of the deep Earth 's interior , and has played an important role in the research of solid Earth science .