Deciphering Late Cenozoic development of the western Svalbard Margin from ODP Site 986 results

No abstract is available for this paper.

• Publication year

  2000

• Venue

  Marine Geology

• Publication date

  2000-10-15

• Fields of study

  Environmental Science, Geology

• Identifiers
  DOI 10.1016/S0025-3227(00)00088-8
• External record

  Open on Semantic Scholar

• Source metadata

  Semantic Scholar

• No claims are published for this paper.

• No concepts are published for this paper.

• Proceedings of the Ocean Drilling Program, Scientific Results

  2001cited by this paper
• 17. THE DEPOSITIONAL ENVIRONMENT OF THE WESTERN SVALBARD MARGIN DURING THE LATE PLIOCENE AND THE PLEISTOCENE: SEDIMENTARY FACIES CHANGES AT SITE 986 1

  1999cited by this paper
• 6. PLIOCENE-PLEISTOCENE AND REDEPOSITED DINOFLAGELLATE CYSTS FROM THE WESTERN SVALBARD MARGIN (SITE 986): BIOSTRATIGRAPHY, PALEOENVIRONMENTS, AND SEDIMENT PROVENANCE 1

  1999cited by this paper
• THE NORWEGIAN–GREENLAND SEA CONTINENTAL MARGINS: MORPHOLOGY AND LATE QUATERNARY SEDIMENTARY PROCESSES AND ENVIRONMENT

  1998cited by this paper
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  1998cited by this paper
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  1998cited by this paper
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  1996cited by this paper
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  1996cited by this paper
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  1996cited by this paper
• Cenozoic sedimentation along the southwestern Barents Sea margin in relation to uplift and erosion of the shelf

  1996cited by this paper
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  1996cited by this paper
• 8. PLANKTONIC FORAMINIFER CENOZOIC BIOSTRATIGRAPHY OF THE ARCTIC OCEAN, FRAM STRAIT (SITES 908-909), YERMAK PLATEAU (SITES 910-912), AND EAST GREENLAND MARGIN (SITE 913)1

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  1996cited by this paper
• 10. PLIOCENE AND QUATERNARY BENTHIC FORAMINIFERS FROM SITE 910, YERMAK PLATEAU1

  1996cited by this paper
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  1996cited by this paper
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  1995cited by this paper
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