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A. D. Albani 《Geo-Marine Letters》1981,1(3-4):163-167
The sedimentary sequence of the Pleistocene deposits of the Botany Basin were investigated using borehole samples and seismic
data. A succession of environments from marine to terrestrial, separated by erosional surfaces, were recognized and, although
absolute dating is not possible, a relative “minimum” chronology was established correlating erosional surfaces with sea-level
fluctuations. Seismic surveys and borehole material from other sites indicate that the model presented here is applicable
to other estuaries of N.S.W. 相似文献
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