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The Maritimes Basin is a Mid-Devonian to Early Permian sedimentary basin that underlies parts of the northeastern United States and Atlantic Canada. It is a composite basin, meaning that it consists of many sub-basins, such as the Windsor-Kennetcook Basin 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: *Windsor-Kennetcook Basin *Debert-Kemptown Basin *Shubenacadie Basin *Musquodoboit Basin *Cumberland Basin *Stellarton Basin *St. Mary's Basin *Antigonish Basin *Western Cape Breton Basin *Central Cape Breton Basin *Sydney Basin 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:〔Bianco, E. (2013). Seismic Interpretation of the Windsor-Kennetcook Basin. Geological survey of Canada Open File 7452. . (Available online. )〕 Image:Sedimentary basins in Nova Scotia.png|thumb|center|800px|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. poly 208 743 206 756 216 757 227 759 220 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Maritimes Basin」の詳細全文を読む スポンサード リンク
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