Morphology and surface texture of quartz grains from ODP Site 105-645

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Autori principali: Cremer, Michel, Legigan, Philippe
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1989
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author Cremer, Michel
Legigan, Philippe
author_facet Cremer, Michel
Legigan, Philippe
collection Datos científicos de ciencias marinas y ambientales
contents The shapes and surface textures of sand-sized quartz grains from the sediments cored at Site 645 in southern Baffin Bay during ODP Leg 105 were studied to characterize the terrigenous materials and the settling processes involved in the deposition of these sediments. Here, we show a homogeneous sand fraction that results from mixing grains from various provenances. The characteristics inherited from terrestrial processes (varying degrees of wear; fluviatile, aeolian, and diagenetic features) dominate the characteristics that result from evolution in a high-energy marine environment. Thus, the influence of the last stage of sedimentation in a deep-marine environment was difficult to distinguish. However, fluctuations in the relative proportions of particular features reveal that the terrigenous material derived from sedimentary formations of Baffin Island and East Greenland or from direct abrasion of the crystalline shield, which changed through time as the dominant settling processes evolved. In particular, this study confirms the onset of major ice rafting as old as late Miocene.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_744805
institution PANGAEA
language en
publishDate 1989
publisher PANGAEA
record_format pangaea
spellingShingle Morphology and surface texture of quartz grains from ODP Site 105-645
Cremer, Michel
Legigan, Philippe
105-645; 105-645B; 105-645D; 105-645E; Baffin Bay; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg105; Ocean Drilling Program; ODP
The shapes and surface textures of sand-sized quartz grains from the sediments cored at Site 645 in southern Baffin Bay during ODP Leg 105 were studied to characterize the terrigenous materials and the settling processes involved in the deposition of these sediments. Here, we show a homogeneous sand fraction that results from mixing grains from various provenances. The characteristics inherited from terrestrial processes (varying degrees of wear; fluviatile, aeolian, and diagenetic features) dominate the characteristics that result from evolution in a high-energy marine environment. Thus, the influence of the last stage of sedimentation in a deep-marine environment was difficult to distinguish. However, fluctuations in the relative proportions of particular features reveal that the terrigenous material derived from sedimentary formations of Baffin Island and East Greenland or from direct abrasion of the crystalline shield, which changed through time as the dominant settling processes evolved. In particular, this study confirms the onset of major ice rafting as old as late Miocene.
title Morphology and surface texture of quartz grains from ODP Site 105-645
topic 105-645; 105-645B; 105-645D; 105-645E; Baffin Bay; COMPCORE; Composite Core; DRILL; Drilling/drill rig; Joides Resolution; Leg105; Ocean Drilling Program; ODP
url https://doi.org/10.1594/PANGAEA.744805