Mesoproterozoic high Fe–Ti mafic magmatism in western Shandong, North China Craton: Petrogenesis and implications for the final breakup of the Columbia supercontinent

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Mesoproterozoic high Fe–Ti mafic magmatism in western Shandong, North China Craton: Petrogenesis and implications for the final breakup of the Columbia supercontinent

High Fe–Ti basic rocks (FeOt > 12 wt% and TiO2 > 2 wt%) are rare in the geological record and display a different evolutionary trend (the ‘Fenner’ trend) from the normal ‘Bowen’ trend of SiO2 enrichment. In this paper, we present geochronological, geochemical and Sr–Nd isotopic data for the Fe...

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Bibliographic Details
Main Authors:	Peng, T., Wilde, Simon, Fan, W., Peng, B., Mao, Y.
Format:	Journal Article
Published:	Elsevier BV 2013
Subjects:	High Fe–Ti basic rocks Columbia supercontinent North China Craton Western Shandong Mesoproterozoic
Online Access:	http://hdl.handle.net/20.500.11937/14996

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