Petrogenesis of Early-Middle Jurassic intrusive rocks in northern Liaoning and central Jilin provinces, northeast China: Implications for the extent of spatial-temporal overprinting of the Mongol-Okhotsk and Paleo-Pacific tectonic regimes
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- 作者：Hai-Hong Zhanga ; b ; zhh12@mails.jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Feng Wanga ; c ; jlu_wangfeng@jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; jlu-wangfeng@sohu.com" class="auth_mail" title="E-mail the corresponding author ; Wen-Liang Xua ; d ; xuwl@jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author ; Hua-Hua Caoe ; caohua9871@163.com" class="auth_mail" title="E-mail the corresponding author ; Fu-Ping Peia ; peifp@jlu.edu.cn" class="auth_mail" title="E-mail the corresponding author
- 关键词：Northeast China ; Early&ndash ; Middle Jurassic ; Intrusive rock ; Petrogenesis ; Mongol&ndash ; Okhotsk tectonic regime ; Paleo-Pacific tectonic regime
- 刊名：Lithos
- 出版年：2016
- 出版时间：July 2016
- 年：2016
- 卷：256-257
- 期：Complete
- 页码：132-147
- 全文大小：3699 K
文摘
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Jurassic intrusions are divided into J1 and J2 in northern Liaoning and central Jilin provinces.
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J1 magmatism was mainly associated with the Paleo-Pacific tectonic regime.
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The J2 magmatism was associated with the Mongol–Okhotsk tectonic regime.