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TitleRegional stratigraphic understanding of the Labrador-Baffin Seaway
 
AuthorDafoe, L TORCID logo; Williams, G L; Dickie, K; Gregersen, U; Knutz, P C; Dam, G; Pedersen, G K; Nohr-Hansen, H; Haggart, J W; DesRoches, K
SourceGeological Society of America, Abstracts With Programs vol. 52, no. 6, 2020., https://doi.org/10.1130/abs/2020AM-355218 Open Access
logo Open Access
LinksOnline - En ligne
Year2020
Alt SeriesNatural Resources Canada, Contribution Series 20200616
PublisherGeological Society of America
MeetingEvolution, Structure and Landscapes of the North Atlantic-Arctic Realm; October 29, 2020
Documentserial
Lang.English
Mediapaper
ProvinceNewfoundland and Labrador; Eastern offshore region
Subjectsenvironmental geology; general geology; geochronology; geophysics; marine geology; Nature and Environment; stratigraphy; tectonics; Lower Cretaceous; stratigraphic analyses; geophysical interpretations; lithology; paleoenvironment; unconformities; Labrador Sea; Davis Strait; Baffin Bay Basin; Cretaceous; Cenozoic
ProgramGEM2: Geo-mapping for Energy and Minerals, Baffin Region
Released2020 10 29
AbstractThe Labrador-Baffin Seaway which includes the Labrador Sea, Davis Strait, and Baffin Bay began forming during Early Cretaceous rifting between the paleo-North American and Greenland plates. Regional geophysical and stratigraphic studies of the resultant offshore and associated onshore basins have been undertaken for decades, but our understanding of the tectonostratigraphic evolution and relationship of the two margins of the seaway is somewhat uncertain. To resolve this, we integrated interpretations from the conjugate margins and divided the stratigraphy into Cretaceous, lower Cenozoic, and upper Cenozoic intervals, with relationships illustrated in conjugate margin profiles and distribution maps. We correlated the lithology, ages, paleoenvironments, and unconformities and integrated seismic stratigraphic frameworks from each margin. During the Early Cretaceous, localized basins formed and were infilled with nonmarine and shallow marine strata, succeeded by a transgressive, Upper Cretaceous marine mudstone and localized sandstone succession as rifting continued and widespread subsidence ensued. Seafloor spreading began in the central Labrador Sea in the Maastrichtian, but propagated regionally by the Early Paleocene along with significant volcanism centered in the Davis Strait. At about the same time, regional regression took place, with a localized middle Paleocene unconformity developed along the western margin of the seaway, but significant missing section to the east. The overlying lower Cenozoic interval is middle Paleocene to Middle Miocene and includes a period of basin inversion starting in the late Paleocene, due to strike-slip motion related to a regional change in the seafloor spreading direction. Initial shallow marine and nonmarine strata are succeeded by a Lower Eocene transgressive phase. Spreading finally ceased in the Late Eocene, but the top of the lower Cenozoic interval is marked by missing section at the base of major clinothems developed within the upper Cenozoic interval. Progradation during this latest interval built parts of the shelf and blanketed the deep water. Our regional correlations help to construct a more complete understanding of the tectonostratigraphic evolution of the region, as well as highlight margin-specific and localized events.
Summary(Plain Language Summary, not published)
This work outlines the integrated stratigraphic framework for the Labrador Sea, Davis Strait and Baffin Bay region, which is related to the opening of the ocean and related sedimentary basins. Basins are infilled with primarily sedimentary rocks as old as Lower Cretaceous, with the youngest rocks of Cenozoic age blanketing much of the seafloor. Both offshore and localized onshore basins were integrated in terms of the stratigraphy and seismic framework to provide regional comparisons and an improved understanding of the tectonostratigraphic history. Seismic sections and distribution maps are used to illustrate these relationships.
GEOSCAN ID327880

 
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