灵山岛中生代沉积岩是深水远源浊积岩、还是陆内三角洲沉积?——与吕洪波教授商榷

GIG OpenIR

	钟建华
	灵山岛中生代沉积岩是深水远源浊积岩、还是陆内三角洲沉积?——与吕洪波教授商榷
Source Publication	地质论评
ISSN	0371-5736
	2012
Volume	58 Issue:6 Pages:1180-1182
Language	中文
CSCD ID	CSCD:4696412
Indexed By	CSCD
Citation statistics	Cited Times:32[CSCD] [CSCD Record]
Document Type	期刊论文
Identifier	http://ir.gig.ac.cn/handle/344008/17855
Collection	中国科学院广州地球化学研究所
Recommended Citation GB/T 7714	钟建华. 灵山岛中生代沉积岩是深水远源浊积岩、还是陆内三角洲沉积?——与吕洪波教授商榷[J]. 地质论评,2012,58(6):1180-1182.
APA	钟建华.(2012).灵山岛中生代沉积岩是深水远源浊积岩、还是陆内三角洲沉积?——与吕洪波教授商榷.地质论评,58(6),1180-1182.
MLA	钟建华."灵山岛中生代沉积岩是深水远源浊积岩、还是陆内三角洲沉积?——与吕洪波教授商榷".地质论评 58.6(2012):1180-1182.

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