Termination time of peak decratonization in North China: Geochemical evidence from mafic igneous rocks
点击次数:
影响因子:3.39
DOI码:10.1016/j.lithos.2015.11.014
发表刊物:LITHOS
第一作者:戴立群
通讯作者:戴立群
论文编号:000372383600019
卷号:240
页面范围:327-336
ISSN号:0024-4937
是否译文:否
发表时间:2015-12-31
收录刊物:SCI
上一条: Source and magma mixing processes in continental subduction factory: Geochemical evidence from postcollisional mafic igneous rocks in the Dabie orogen
下一条: Tectonic development from oceanic subduction to continental collision: Geochemical evidence from postcollisional mafic rocks in the Hong'an-Dabie orogens
