锥峰和塔峰溶丘地貌的表层喀斯特带径流溶蚀形成机制

	锥峰和塔峰溶丘地貌的表层喀斯特带径流溶蚀形成机制
	张信宝; 刘再华; 王世杰; 陈喜
	2012
Source Publication	山地学报
Volume	29 Issue:5 Pages:529-533
Document Type	期刊论文
Identifier	http://ir.gyig.ac.cn/handle/352002/4626
Collection	环境地球化学国家重点实验室_环境地球化学国家重点实验室_期刊论文
Recommended Citation GB/T 7714	张信宝,刘再华,王世杰,等. 锥峰和塔峰溶丘地貌的表层喀斯特带径流溶蚀形成机制[J]. 山地学报,2012,29(5):529-533.
APA	张信宝,刘再华,王世杰,&陈喜.(2012).锥峰和塔峰溶丘地貌的表层喀斯特带径流溶蚀形成机制.山地学报,29(5),529-533.
MLA	张信宝,et al."锥峰和塔峰溶丘地貌的表层喀斯特带径流溶蚀形成机制".山地学报 29.5(2012):529-533.

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