Publications des scientifiques de l'IRD

Louterbach M., Roddaz Martin, Antoine P. O., Marivaux L., Adnet S., Bailleul J., Dantas E., Santos R. V., Chemale F., Baby Patrice, Sanchez C., Calderon Y. (2018). Provenance record of late Maastrichtian-late Palaeocene Andean Mountain building in the Amazonian retroarc foreland basin (Madre de Dios basin, Peru). Terra Nova, 30 (1), p. 17-23. ISSN 0954-4879.

Titre du document
Provenance record of late Maastrichtian-late Palaeocene Andean Mountain building in the Amazonian retroarc foreland basin (Madre de Dios basin, Peru)
Année de publication
2018
Type de document
Article référencé dans le Web of Science WOS:000423619700003
Auteurs
Louterbach M., Roddaz Martin, Antoine P. O., Marivaux L., Adnet S., Bailleul J., Dantas E., Santos R. V., Chemale F., Baby Patrice, Sanchez C., Calderon Y.
Source
Terra Nova, 2018, 30 (1), p. 17-23 ISSN 0954-4879
Biostratigraphic, sedimentological and provenance analyses suggest that a proto-Andean Cordillera already existed in southern Peru by late Maastrichtian-late Palaeocene times. A 270-m-thick stratigraphic section shows changes in depositional environments from shallow marine (early Maastrichtian) to non-marine (late Maastrichtian) then back to estuarine (late Palaeocene) conditions. An erosional surface separates lower Maastrichtian from upper Maastrichtian deposits. Above this surface, the late Maastrichtian unit exhibits moderately developed palaeosols and syn-sedimentary normal faults. The sedimentary evolution is accompanied by a decrease in sedimentation rate and by changes in provenance. Shallow marine lower Maastrichtian deposits have a cratonic provenance as shown by their low epsilon Nd(0) values (-15 to -16) and the presence of Precambrian inherited zircon grains. The upper Maastrichtian deposits have a mixed Andean and cratonic origin with epsilon Nd(0) values of similar to 12.6 and yield the first Cretaceous and Permo-Triassic zircon grains. Estuarine to shallow marine upper Palaeocene deposits have an Andean dominant source as attested by higher epsilon Nd(0) values (-6 to -10) and by the presence of Palaeozoic and Late Cretaceous zircon grains. The changes in depositional environments and sedimentation rates, as well as the shift in detrital provenance, are consistent with a late Maastrichtian-late Palaeocene period of Andean mountain building. In agreement with recently published studies, our data suggest that an Andean retroarc foreland basin was active by late Maastrichtian-late Palaeocene times.
Plan de classement
Géologie et formations superficielles [064]
Description Géographique
PEROU ; MADRE DE DIOS BASSIN ; ANDES
Localisation
Fonds IRD [F B010072044]
Identifiant IRD
fdi:010072044
Contact