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Proceedings of the Ocean Drilling Program, 166 Scientific Results
The oxygen isotopic composition of interstitial waters: evidence for fluid flow and recrystallization in the margin of Great Bahama Bank
monograph
Author(s):
P.K. Swart
Publication date
(Online):
May 2000
Publisher:
Ocean Drilling Program
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Scientific Ocean Drilling Expedition Research Results
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Book Chapter
Publication date (Online):
May 2000
DOI:
10.2973/odp.proc.sr.166.130.2000
SO-VID:
79081337-8011-47b8-a6d7-aeb9b352ba9b
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Book chapters
The oxygen isotopic composition of interstitial waters: evidence for fluid flow and recrystallization in the margin of Great Bahama Bank
The record of Neogene sea-level changes in the prograding carbonates along the Bahamas Transect—Leg 166 Synthesis
Overview of interstitial fluid and sediment geochemistry, Sites 1003-1007 (Bahamas Transect)
Turbidite frequency and composition in the distal part of the Bahamas Transect
Data Report: Geochemistry and mineralogy of periplatform carbonate sediments: Sites 1006, 1008, and 1009
Data Report: Geochemistry of Miocene sediments, Sites 1006 and 1007, Leeward Margin, Great Bahama Bank
Coupled early Pliocene-middle Miocene bio-cyclostratigraphy of Site 1006 reveals orbitally induced cyclicity patterns of Great Bahama Bank carbonate production
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