Cenozoic calcareous nannofossils from the Lesser Antilles Forearc Region

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Auteur principal: Clark, Murlene W
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 1990
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author Clark, Murlene W
author_facet Clark, Murlene W
collection Datos científicos de ciencias marinas y ambientales
contents During Leg 110 of the Ocean Drilling Program, sediment was recovered from six sites in the vicinity of the Lesser Antilles Forearc. Hole 671B, drilled near the toe of the Barbados deformation front, was the first-ever penetration of the decollement between the underthrusting Atlantic Plate and the off scraped Barbados accretionary prism. Stratigraphic repetitions in sequence associated with tectonic movement along the decollement zone, first observed on DSDP Leg 78A, were further documented at four ODP Leg 110 sites. A significant biostratigraphic inversion is present at Site 671 at 128 mbsf in which upper Miocene sediments rest atop lower Pleistocene strata. Smaller repetitions in sequence are recorded at Sites 671, 673, 674, and 676. Leg 110 sediments range from middle Eocene to early Pleistocene in age. Pliocene/Pleistocene assemblages are generally well preserved; however, Miocene assemblages have undergone extensive dissolution at all Leg 110 sites. Paleogene sediments are sometimes recrystallized and the nannofossils contained within exhibit a range in preservation from poor to good.
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institution PANGAEA
language en
publishDate 1990
publisher PANGAEA
record_format pangaea
spellingShingle Cenozoic calcareous nannofossils from the Lesser Antilles Forearc Region
Clark, Murlene W
110-671B; 110-672A; 110-673B; 110-674A; 110-676A; DRILL; Drilling/drill rig; Joides Resolution; Leg110; North Atlantic Ocean; Ocean Drilling Program; ODP
During Leg 110 of the Ocean Drilling Program, sediment was recovered from six sites in the vicinity of the Lesser Antilles Forearc. Hole 671B, drilled near the toe of the Barbados deformation front, was the first-ever penetration of the decollement between the underthrusting Atlantic Plate and the off scraped Barbados accretionary prism. Stratigraphic repetitions in sequence associated with tectonic movement along the decollement zone, first observed on DSDP Leg 78A, were further documented at four ODP Leg 110 sites. A significant biostratigraphic inversion is present at Site 671 at 128 mbsf in which upper Miocene sediments rest atop lower Pleistocene strata. Smaller repetitions in sequence are recorded at Sites 671, 673, 674, and 676. Leg 110 sediments range from middle Eocene to early Pleistocene in age. Pliocene/Pleistocene assemblages are generally well preserved; however, Miocene assemblages have undergone extensive dissolution at all Leg 110 sites. Paleogene sediments are sometimes recrystallized and the nannofossils contained within exhibit a range in preservation from poor to good.
title Cenozoic calcareous nannofossils from the Lesser Antilles Forearc Region
topic 110-671B; 110-672A; 110-673B; 110-674A; 110-676A; DRILL; Drilling/drill rig; Joides Resolution; Leg110; North Atlantic Ocean; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.755088