R. Dalrymple

Publications142
h-index51
Citations10,353
Highly Influential Citations625
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Estuarine Facies Models: Conceptual Basis and Stratigraphic Implications: PERSPECTIVE
ABSTRACT The nature and organization of facies within incised-valley estuaries is controlled by the interplay between marine processes (waves and tides), which generally decrease in intensity… Expand
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The Stratigraphic Organization of Incised-Valley Systems Associated with Relative Sea-Level Change
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Morphologic and facies trends through the fluvial–marine transition in tide-dominated depositional systems: A schematic framework for environmental and sequence-stratigraphic interpretation
Abstract Most tide-dominated estuarine and deltaic deposits accumulate in the fluvial-to-marine transition zone, which is one of the most complicated areas on earth, because of the large number of… Expand
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Towards the standardization of sequence stratigraphy
Abstract Sequence stratigraphy emphasizes facies relationships and stratal architecture within a chronological framework. Despite its wide use, sequence stratigraphy has yet to be included in any… Expand
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Estuarine facies models; conceptual basis and stratigraphic implications; discussion and reply
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Classification of clastic coastal depositional environments
Abstract This paper proposes a new classification for clastic coastal environments which includes the full range of major depositional settings including deltas, strand plains, tidal flats, estuaries… Expand
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Sedimentology and Stratigraphy of a Tide-Dominated, Foreland-Basin Delta (Fly River, Papua New Guinea)
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Processes, Morphodynamics, and Facies of Tide-Dominated Estuaries
As defined in this chapter, an estuary forms during a shoreline transgression and then fills during a progradational phase that is transitional to a delta. The spatial distribution of processes,… Expand
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Late Quaternary Deltaic and Carbonate Sedimentation in the Gulf of Papua Foreland Basin: Response to Sea-Level Change
ABSTRACT The rivers that drain the wet, mountainous island of New Guinea discharge about 1.5 billion tonnes/yr of sediments into the adjacent seas, including the foreland basin between New Guinea and… Expand
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Dynamics and facies model of a macrotidal sand‐bar complex, Cobequid Bay—Salmon River Estuary (Bay of Fundy)
The 40-km-long, Cobequid Bay—Salmon River estuary has a maximum tidal range of 16·3 m and experiences limited wave action. Sediment, which is derived primarily from areas seaward of the estuary, is… Expand
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