GIG OpenIR  > 中科院广州地化所(-2008)
徐海军; 金振民; 欧新功
中国大陆科学钻探主孔100~2000m岩石心的磁化率各向异性及其地质意义
Source Publication岩石学报
ISSN1000-0569
2006
Volume22Issue:7Pages:2081-2088
Indexed Bysci
Language中文
Document Type期刊论文
Identifierhttp://ir.gig.ac.cn/handle/344008/13265
Collection中科院广州地化所(-2008)
Recommended Citation
GB/T 7714
徐海军,金振民,欧新功. 中国大陆科学钻探主孔100~2000m岩石心的磁化率各向异性及其地质意义[J]. 岩石学报,2006,22(7):2081-2088.
APA 徐海军,金振民,&欧新功.(2006).中国大陆科学钻探主孔100~2000m岩石心的磁化率各向异性及其地质意义.岩石学报,22(7),2081-2088.
MLA 徐海军,et al."中国大陆科学钻探主孔100~2000m岩石心的磁化率各向异性及其地质意义".岩石学报 22.7(2006):2081-2088.
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