Patterns of infull and basin-scale architecture : Tyee Forearc Basin, and observation from a segment of New Jersey passive margin
The well-known clinoformal geometry of a basin-fill, with an alluvial to shelf segment, deep-water slope segment, and a basin floor segment, arises from the development of a wedge-shaped body of sediment at the basin-margin that has been termed a basin-margin wedge or a shelf-slope sedimentary prism...
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| Format: | Others |
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2014
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| Online Access: | http://hdl.handle.net/2152/26478 |