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, les données existantes sont anciennes et mal naviguées, est fortement souhaitable
interprétées par l'industrie, plus spécifiquement au centre et à l'ouest du golfe, est essentielle pour améliorer notre modèle. Reconstruire l'évolution du golfe en tenant compte de la position à chaque période des continents Nord et Sud-américains sera une tâche primordiale pour mieux contraindre notre modèle. Cette étape, insuffisamment approfondie faute de temps dans cette thèse, nous permettra d'asseoir solidement les pôles de rotation obtenus dans cette thèse en contraignant l'espace existant entre les continents nord et sud-américain lors de l'éclatement de la Pangée, l'intégration de données sismiques ou de forages acquises et, dans de nombreux cas ,
, En ce qui concerne la plaque Caraïbe, la comparaison des anomalies magnétiques datée de la Période Magnétique Calme du Crétacé avec celles d'autres bassins océaniques pourrait permettre d'affiner notre interprétation et de dater plus finement les anomalies observées
, L'acquisition de données magnétiques de haute résolution, à proximité du fond, est une option qu'il convient de ne pas exclure. La comparaison des données de l'arc des Petites Antilles avec des bassins ayant une géométrie similaire, comme le bassin d'arrière-arc des Mariannes, pourrait aider à une meilleure compréhension des bassins voisins de cet arc
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