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戴立群
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论文成果
Termination time of peak decratonization in North China: Geochemical
evidence from mafic igneous rocks
发布时间:2021-07-23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