Maritimes Basin

From Wikipedia, the free encyclopedia

The Maritimes Basin is a Mid-Devonian to Early Permian sedimentary basin that underlies parts of the northeastern United States and Atlantic Canada.[1] It is a composite basin, meaning that it consists of many sub-basins, such as the of Nova Scotia. Some of these basins host important natural resources, including coal, petroleum, and minerals such as sylvite, halite, and barite. The Maritimes Basin was deposited and tectonically-modified during the final assembly of Pangea.

List of sub-basins in Nova Scotia[]

The Maritimes Basin consists of eleven sub-basins in Nova Scotia:

The region has a complex basin history in terms of syndepositional deformation and superimposition of numerous episodes of fault reactivation in the basin. As such, each basin has distinctive stratigraphy, especially within the lowermost Carboniferous section.

The eleven sub-basins are located in this clickable map:[2]

Windsor-Kennetcook BasinDebert-Kemptown BasinShubenacadie BasinMusquodoboit BasinCumberland BasinStellarton BasinSt. Mary's BasinAntigonish BasinWestern Cape Breton BasinCentral Cape Breton BasinSydney Basin
Shaded relief digital elevation model, showing the eleven sedimentary basins in Nova Scotia. The locations of petroleum exploration wells are indicated by the black dots.

References[]

  1. ^ Gibling, M.R.; Culshaw, N.; Rygel, M.C.; Pascucci, V. (2008), "Chapter 6: The Maritimes Basin of Atlantic Canada: Basin creation and destruction in the collisional zone of Pangea", in Miall, A.D. (ed.), Sedimentary Basins of the World, 5, pp. 211–244, doi:10.1016/S1874-5997(08)00006-3
  2. ^ Bianco, E. (2013). Seismic Interpretation of the Windsor-Kennetcook Basin. Geological survey of Canada Open File 7452. doi:10.4095/292763. Available online.[permanent dead link]
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