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高压下测量岩石纵波速度的反射—透射法
周文戈; 谢鸿森; 赵志丹; 刘永刚; 岳兰秀
2001
Source Publication地质科技情报
Issue3Pages:1-5
Other Abstract介绍了一种高压下测量岩石纵波速度的新方法——反射—透射法。并在室温高压 ( 0 .1~ 0 .3GPa)的条件下测量了麻粒岩和榴辉岩等样品的纵波波速 ,所获得的结果在误差范围内与前人的工作相吻合 ,而该方法能达到的实验压力更高。与透射法相比 ,反射—透射法的优点在于它适用于地幔岩石纵波速度的测量.
Keyword反射—透射法 纵波速度 高压
Subject Area地球深部物质与流体作用地球化学
Indexed ByCSCD
Language中文
CSCD IDCSCD:578176
Citation statistics
Cited Times:3[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/7351
Collection地球内部物质高温高压实验室_地球内部物质高温高压实验室_期刊论文
Recommended Citation
GB/T 7714
周文戈,谢鸿森,赵志丹,等. 高压下测量岩石纵波速度的反射—透射法[J]. 地质科技情报,2001(3):1-5.
APA 周文戈,谢鸿森,赵志丹,刘永刚,&岳兰秀.(2001).高压下测量岩石纵波速度的反射—透射法.地质科技情报(3),1-5.
MLA 周文戈,et al."高压下测量岩石纵波速度的反射—透射法".地质科技情报 .3(2001):1-5.
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