Original paper
Geochronologic and geochemical constraints of the petrogenesis of Permian mafic dykes in the Wuding area, SW China: Implications for Fe–Ti enrichment in mafic rocks in the ELIP
Abstract
Mafic dykes are widely distributed and well preserved in the Wuding area, SW China. The dykes are composed of fine-grained diabases, which are further subdivided into two groups (Group I and Group II). The rocks from Group I have relatively higher MgO (4.95–6.16 wt%) and lower TiO 2 null (2.26–2.78 wt%) contents than those from the Group II rocks (MgO = 4.04–4.58 wt%; TiO 2 = 4.09–4.55 wt%). Two baddeleyite ages of 264 ± 3 Ma and 256 ± 5 Ma...
Paper Details
Title
Geochronologic and geochemical constraints of the petrogenesis of Permian mafic dykes in the Wuding area, SW China: Implications for Fe–Ti enrichment in mafic rocks in the ELIP
Published Date
Feb 1, 2017
Volume
331
Pages
64 - 78
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History