Late Carboniferous N-MORB-type basalts in central Inner Mongolia, China: Products of hydrous melting in an intraplate setting?

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Late Carboniferous N-MORB-type basalts in central Inner Mongolia, China: Products of hydrous melting in an intraplate setting?

Petrogenesis of the ca. 310 Ma Benbatu basalts in central Inner Mongolia is crucial for constraining the evolution of the Xing'an Mongolia Orogenic Belt (XMOB), eastern segment of the Central Asian Orogenic Belt. The Benbatu basalts have low initial 87Sr/86Sr ratios (0.7042–0.7048), positive εN...

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Bibliographic Details
Main Authors:	Pang, C., Wang, Xuan-Ce, Xu, B., Zhao, J., Feng, Y., Wang, Y., Luo, Z., Liao, W.
Format:	Journal Article
Published:	Elsevier BV 2015
Online Access:	https://espace.library.uq.edu.au/view/UQ:406460 http://hdl.handle.net/20.500.11937/6456

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