Wang, Yuejun, Fan, Weiming, Zhang, Yanhua, Guo, Feng, Zhang, Hongfu, Peng, Touping (2004) Geochemical, 40Ar/39Ar geochronological and Sr–Nd isotopic constraints on the origin of Paleoproterozoic mafic dikes from the southern Taihang Mountains and implications for the ca. 1800Ma event of the North China Craton. Precambrian Research, 135 (1) 55-77 doi:10.1016/j.precamres.2004.07.005

Reference Type | Journal (article/letter/editorial) | ||
---|---|---|---|
Title | Geochemical, 40Ar/39Ar geochronological and Sr–Nd isotopic constraints on the origin of Paleoproterozoic mafic dikes from the southern Taihang Mountains and implications for the ca. 1800Ma event of the North China Craton | ||
Journal | Precambrian Research | ||
Authors | Wang, Yuejun | Author | |
Fan, Weiming | Author | ||
Zhang, Yanhua | Author | ||
Guo, Feng | Author | ||
Zhang, Hongfu | Author | ||
Peng, Touping | Author | ||
Year | 2004 (November) | Volume | 135 |
Issue | 1 | ||
Publisher | Elsevier BV | ||
URL | |||
DOI | doi:10.1016/j.precamres.2004.07.005Search in ResearchGate | ||
Generate Citation Formats | |||
Mindat Ref. ID | 704818 | Long-form Identifier | mindat:1:5:704818:4 |
GUID | 0 | ||
Full Reference | Wang, Yuejun, Fan, Weiming, Zhang, Yanhua, Guo, Feng, Zhang, Hongfu, Peng, Touping (2004) Geochemical, 40Ar/39Ar geochronological and Sr–Nd isotopic constraints on the origin of Paleoproterozoic mafic dikes from the southern Taihang Mountains and implications for the ca. 1800Ma event of the North China Craton. Precambrian Research, 135 (1) 55-77 doi:10.1016/j.precamres.2004.07.005 | ||
Plain Text | Wang, Yuejun, Fan, Weiming, Zhang, Yanhua, Guo, Feng, Zhang, Hongfu, Peng, Touping (2004) Geochemical, 40Ar/39Ar geochronological and Sr–Nd isotopic constraints on the origin of Paleoproterozoic mafic dikes from the southern Taihang Mountains and implications for the ca. 1800Ma event of the North China Craton. Precambrian Research, 135 (1) 55-77 doi:10.1016/j.precamres.2004.07.005 | ||
In | (2004, November) Precambrian Research Vol. 135 (1) Elsevier BV |
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