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Comment on “The Mesozoic Margin of the Maghrebian Tethys in the Rif Belt (Morocco): Evidence for Polyphase Rifting and Related Magmatic Activity” by Gimeno‐Vives et al.
Tectonics ( IF 3.3 ) Pub Date : 2020-04-06 , DOI: 10.1029/2019tc006004 A. Michard 1 , O. Saddiqi 2 , A. Chalouan 3 , M.C. Chabou 4 , P. Lach 5 , P. Rossi 6 , H. Bertrand 7 , N. Youbi 8, 9
中文翻译:
Gimeno-Vives等人评论了“里夫带马格里布特提斯的中生代边缘(摩洛哥):多相裂谷和相关岩浆活动的证据”。
更新日期:2020-04-06
Tectonics ( IF 3.3 ) Pub Date : 2020-04-06 , DOI: 10.1029/2019tc006004 A. Michard 1 , O. Saddiqi 2 , A. Chalouan 3 , M.C. Chabou 4 , P. Lach 5 , P. Rossi 6 , H. Bertrand 7 , N. Youbi 8, 9
Affiliation
- The main Mesorif gabbros emplaced in a Liassic oceanic domain and do not belong to the Central Atlantic Magmatic Province (CAMP)
- CAMP dolerites may occur separately next to the oceanic gabbros in the structurally complex Mesorif zone
- The prerift/synrift cover of the distal margin could have emplaced by gravity sliding onto the Mesorif oceanic crust
中文翻译:
Gimeno-Vives等人评论了“里夫带马格里布特提斯的中生代边缘(摩洛哥):多相裂谷和相关岩浆活动的证据”。
- 主要的Mesorif长颈鹿被放置在一个拉西洋海域中,不属于中大西洋岩浆省(CAMP)
- CAMP白云岩可能在结构复杂的Mesorif区域中的海洋辉长岩旁单独出现
- 远端边缘的预裂/合缝盖可能已因重力滑入Mesorif大洋地壳而被置入