Reconciliaion of late Quaternary sea levels derived from coral terraces at Huon Peninsula with deep sea oxygen isotope records-Reference-Cited by-同舟云学术

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Reconciliaion of late Quaternary sea levels derived from coral terraces at Huon Peninsula with deep sea oxygen isotope records

Published:1996-06 Issue:1-4 Volume:141 Page:227-236
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Chappell John,Omura Akio,Esat Tezer,McCulloch Malcolm,Pandolfi John,Ota Yoko,Pillans Brad

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference29 articles.

1. Oxygen isotopes and sea level;Chappell;Nature,1986

2. Oxygen isotopes, sea level changes and the temperature history of a coral reef environment in New Guinea over the last 150,000 years;Aharon;Palaeogeogr. Palaeoclimatol. Palaeoecol.,1986

3. Quaternary sea level fluctuations on a tectonic coast; new 230Th234U dates from the Huon Peninsula, New Guinea;Bloom;Quat. Res.,1974

4. Late Quaternary tectonic movements and sea-level changes at Timor and and Atauro Island;Chappell;Bull. Geol. Soc. Am.,1978

5. Pleistocene sea levels from raised coral reefs of Haiti;Dodge;Science,1983

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