垂直于小安的列斯群岛弧线俯冲的主动延伸(瓜德罗普,法属安的列斯群岛)

Nathalie Feuillet, Isabelle Manighetti, Paul Tapponnier
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引用次数: 46

摘要

活动的正断层切割了小安的列斯岛弧上的Grande-Terre和Marie-Galante隆起的礁台和Basse-Terre的火山岩。新的海洋地球物理数据表明,这种断层延伸到近海,形成了两套不同的断层。一组边界地堑垂直于弧,证明了南北延伸。另一组的“雁梯队”断层,大致沿着火山弧,容纳了左旋运动的一部分。活跃的soufri火山位于马里-加兰特地堑的西端。震级小于5.5的历史和仪器地震可能使Marie-Galante地堑边界断层破裂。
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Extension active perpendiculaire à la subduction dans l'arc des Petites Antilles (Guadeloupe, Antilles françaises)

Active normal faults cut the uplifted reef platforms of Grande-Terre and Marie-Galante and the volcanic rocks of Basse-Terre in the Lesser Antilles arc. New marine geophysical data shows that such faults extend offshore, forming two distinct sets. One set bounds graben perpendicular to the arc, attesting to ∼ north–south extension. The ‘en echelon’ faults of the other set, roughly along the volcanic arc, accommodate a component of sinistral motion. The active Soufrière volcano lies inside the western termination of the Marie-Galante graben. Historical and instrumental earthquakes with magnitude ⩾5.5 may have ruptured the Marie-Galante graben bounding faults.

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