Charte Stratigraphique et Héritage Tectonique
VI. SYNTHESE STRATIGRAPHIQUE
La compilation bibliographique, complétée par quelques travaux de terrain, de l’étude
des formations des unités morpho-structurales du transect permet de mettre en évidence les
grandes périodes de sédimentation et d’érosion des cordillères de la zone. La synthèse des
évènements tectoniques ayant affecté le nord du continent sud-américain montre également
qu’il existe un héritage structural et paléogéographique important : orogènes Gondwanien, Jurua, Névadien ; rift Mitú, individualisation des bassins, bassin pull-appart Chicama.
1. Le système pré-andin est une succession complexe constituant l’héritage tectonique à prendre en compte pour le reste de l’étude.
2. La période de rifting permo-triasique Mitú présente de la Cordillère Orientale
jusqu’au bassin Marañón individualise les bassins ouest et est.
3. Le bassin ouest péruvien est un remplissage du Jurassique au Paléocène dont la
surface d’érosion occidentale est progressive d’ouest en est et discontinue sur sa
partie orientale.
4. La base albienne du Crétacé en zone Subandine marque la discordance basale du
bassin d’avant-pays subandin.
5. Les bassins subandins Huallaga et Marañón enregistrent le remplissage associés à la propagation du prisme orogénique depuis le Santonien.
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