Early diagenesis and authigenic mineral formation in anoxic sediments of Kau Bay, Indonesia

Keyphrases

• Freshwater 100%
• Indonesia 100%
• Early Diagenesis 100%
• Authigenic Mineral Formation 100%
• Anoxic Sediments 100%
• Sill 75%
• Dolomite 75%
• Marine Sediments 50%
• Organic Carbon 50%
• Sulphidic 50%
• Bottom Water 50%
• Major Components 50%
• Water-sediment System 50%
• Pacific Ocean 50%
• Weichselian 50%
• Iron Content 50%
• Euxinic 50%
• Pore Water 50%
• Interstitial Fluid 50%
• Reactive Iron 50%
• Authigenic Minerals 50%
• Seawater 25%
• Chloride 25%
• Sulfur 25%
• Ammonium 25%
• Clay 25%
• Marine Basin 25%
• Low Oxygen 25%
• Apatite 25%
• Speciation 25%
• Phosphate 25%
• Ion Exchange 25%
• Pyrite 25%
• In the Zone 25%
• Sulfide 25%
• Carbon-rich 25%
• Alkalinity 25%
• Hydrography 25%
• Methane Oxidation 25%
• Exchangeable Cations 25%
• Deep Basin 25%
• Sulfidization 25%
• Organic Matter Decomposition 25%
• Marine Facies 25%
• Ion Exchange Reaction 25%
• Direct Precipitation 25%
• Diagenetic Reactions 25%
• Terrigenous Organic Matter 25%
• Holocene Sea-level Rise 25%
• Halmahera 25%
• Transitional Facies 25%
• Distinct Units 25%
• Precipitation from Solution 25%
• Ammonium Cation 25%
• Bay Islands 25%
• Eastern Indonesia 25%
• Organic Sulfur 25%
• Below Sea Level 25%
• Pyrite Sulfur 25%

Earth and Planetary Sciences

• Freshwater 100%
• Indonesia 100%
• Porewater 100%
• Anoxic Sediment 100%
• Diagenesis 100%
• Authigenic Mineral 100%
• Dolomite 75%
• Iron 75%
• Marine Sediment 50%
• Holocene 50%
• Sea Level 50%
• Bottom Water 50%
• Weichselian 50%
• Pacific Ocean 50%
• Organic Carbon 50%
• Ion Exchange 50%
• Salinity 25%
• Calcite 25%
• Sea Level Change 25%
• Methane 25%
• Calcium Phosphate 25%
• Clay-Water 25%
• Decomposition of Organic Matter 25%
• Organic Matter 25%
• Alkalinity 25%