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      Massive siliciclastic discharge to slopes of the Great Barrier Reef Platform during sea-level transgression: constraints from sediment cores between 15°S and 16°S latitude and possible explanations

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      Sedimentary Geology
      Elsevier BV

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          Journal
          Sedimentary Geology
          Sedimentary Geology
          Elsevier BV
          00370738
          November 2003
          November 2003
          : 162
          : 1-2
          : 141-158
          Article
          10.1016/S0037-0738(03)00216-1
          3e06c43e-e5bd-47fd-9a11-0ae407ae63f4
          © 2003

          http://www.elsevier.com/tdm/userlicense/1.0/

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