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Magnetostratigraphy of the Suerkuli Basin indicates Pliocene (3.2 Ma) activity of the middle Altyn Tagh Fault, northern Tibetan Plateau
Chang H (Chang, Hong); Ao H (Ao, Hong); An ZS (An, Zhisheng); Fang XM (方小敏); Song YG (Song, Yougui); Qiang XK (Qiang, Xiaoke); Chang, H (通讯作者),Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China.
Source PublicationJOURNAL OF ASIAN EARTH SCIENCES
2012
Volume44Issue:特刊: SIPages:169-175
Subject Area地质学
WOS IDWOS:000300203200013
Language英语
Indexed BySCI
KeywordResolution Magneto Stratigraphy Tectonic Uplift Qinghai Province Qaidam Basin China Deformation Growth Paleomagnetism Sedimentation Displacement
Cooperation Status国际
Department大陆碰撞与高原隆升重点实验室
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Document Type期刊论文
Identifierhttp://ir.itpcas.ac.cn/handle/131C11/2148
Collection图书馆
Corresponding AuthorChang, H (通讯作者),Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China.
Recommended Citation
GB/T 7714
Chang H ,Ao H ,An ZS ,et al. Magnetostratigraphy of the Suerkuli Basin indicates Pliocene (3.2 Ma) activity of the middle Altyn Tagh Fault, northern Tibetan Plateau[J]. JOURNAL OF ASIAN EARTH SCIENCES,2012,44(特刊: SI):169-175.
APA Chang H .,Ao H .,An ZS .,Fang XM .,Song YG .,...&Chang, H .(2012).Magnetostratigraphy of the Suerkuli Basin indicates Pliocene (3.2 Ma) activity of the middle Altyn Tagh Fault, northern Tibetan Plateau.JOURNAL OF ASIAN EARTH SCIENCES,44(特刊: SI),169-175.
MLA Chang H ,et al."Magnetostratigraphy of the Suerkuli Basin indicates Pliocene (3.2 Ma) activity of the middle Altyn Tagh Fault, northern Tibetan Plateau".JOURNAL OF ASIAN EARTH SCIENCES 44.特刊: SI(2012):169-175.
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