[HTML][HTML] Palaeoshorelines on the Australian continental shelf: Morphology, sea-level relationship and applications to environmental management and archaeology
Palaeoshorelines that lie submerged on stable continental shelves are relict coastal
depositional and erosional structures formed during periods of lower sea level. An analysis
of the well-dated Late Quaternary (0–128 ka) sea-level record indicates that the most
persistent (modal) lower sea levels were at 30–40 m below present, which occurred
between 97 and 116 ka and at approximately 85 ka and 10 ka. A secondary modal position
was at 70–90 m that occurred mostly during a period of fluctuating sea level between 30 and …
depositional and erosional structures formed during periods of lower sea level. An analysis
of the well-dated Late Quaternary (0–128 ka) sea-level record indicates that the most
persistent (modal) lower sea levels were at 30–40 m below present, which occurred
between 97 and 116 ka and at approximately 85 ka and 10 ka. A secondary modal position
was at 70–90 m that occurred mostly during a period of fluctuating sea level between 30 and …
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