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Hong, Hanlie, Li, Zhaohui, Xue, Huijuan, Zhu, Yunhai, Zhang, Kexin, Xiang, Shuyuan (2007) Oligocene clay mineralogy of the Linxia Basin: evidence of Paleoclimatic evolution subsequent to the initial-stage uplift of the Tibetan Plateau. Clays and Clay Minerals, 55 (5) 491-503 doi:10.1346/ccmn.2007.0550504

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Reference TypeJournal (article/letter/editorial)
TitleOligocene clay mineralogy of the Linxia Basin: evidence of Paleoclimatic evolution subsequent to the initial-stage uplift of the Tibetan Plateau
JournalClays and Clay Minerals
AuthorsHong, HanlieAuthor
Li, ZhaohuiAuthor
Xue, HuijuanAuthor
Zhu, YunhaiAuthor
Zhang, KexinAuthor
Xiang, ShuyuanAuthor
Year2007 (October 1)Volume55
Page(s)491-503Issue5
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1346/ccmn.2007.0550504Search in ResearchGate
Mindat Ref. ID148161Long-form Identifiermindat:1:5:148161:1
GUID21a3e44b-0b17-42ec-886e-3e4630eed7f7
Full ReferenceHong, Hanlie, Li, Zhaohui, Xue, Huijuan, Zhu, Yunhai, Zhang, Kexin, Xiang, Shuyuan (2007) Oligocene clay mineralogy of the Linxia Basin: evidence of Paleoclimatic evolution subsequent to the initial-stage uplift of the Tibetan Plateau. Clays and Clay Minerals, 55 (5) 491-503 doi:10.1346/ccmn.2007.0550504
Plain TextHong, Hanlie, Li, Zhaohui, Xue, Huijuan, Zhu, Yunhai, Zhang, Kexin, Xiang, Shuyuan (2007) Oligocene clay mineralogy of the Linxia Basin: evidence of Paleoclimatic evolution subsequent to the initial-stage uplift of the Tibetan Plateau. Clays and Clay Minerals, 55 (5) 491-503 doi:10.1346/ccmn.2007.0550504
In(2007, October) Clays and Clay Minerals Vol. 55 (5) Springer Science and Business Media LLC


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