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New evidence for the breakup of the Columbia supercontinent from the northeastern margin of Tarim Craton: rock geochemistry, zircon U-Pb geochronology and Hf-O isotopic compositions of the ca. 1.55 Ga diabase sills in the Kuruktag area.
ZHANG Jian,LI Huaikun,ZHANG Chuanlin,TIAN Hui,ZHONG Yan,YE Xiantao
Earth Science Frontiers . 2018, (
6
): 106 -123 . DOI: 10.13745/j.esf.sf.2018.11.15