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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
Mineralogy and sedimentology of the Pleistocene to Holocene on the Leeward Margin of Great Bahama Bank
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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