A porcellanite layer, probably younger than 0.6-0.4 Ma, of a nearly monomineralic composition of opal-CT was sampled on the Southwest Indian Ridge during Polarstern cruise ANT-VI/3. The intense cementation of the rock, together with recent findings by the Ocean Drilling Program (Legs 113 and 120) and the occurrence of a unique older porcellanite from Eltanin Core 47-15, provides evidence of very early silica precipitation in pure diatom oozes of the Southern Ocean. Such porcellanites occur in shallowly buried young sediments and provide a contrast to the established concepts of porcellanite formation
Deep-sea cores recovered from the N.W. Indian Ocean during Leg 23 of the Deep-Sea Drilling Project w...
Measurements of opal preservation in deep sea sediment cores have been presented in three ways: the ...
Since the 1970s, Ocean Drilling Program (ODP) and Deep Sea Drilling Program (DSDP) studies have docu...
The formation of marine opal-CT nodules or layers as early diagenetic deposits has been documented o...
From the equatorial Indian Ocean, carbonate-free portions of sediment samples of Paleocene to Miocen...
This study deals with the mineralogical variability of siliceous and zeolitic sediments, porcellanit...
The Mesoproterozoic porcellanite of the Vindhyan Super group is the oldest porcellanite deposit of ...
From the equatorial Indian Ocean, carbonate-free portions of sediment samples of Paleocene to Miocen...
Carbonate-free portions of Upper Cretaceous to Holocene sediment samples from the Kerguelen Plateau ...
A distinct porcellanite layer from the Southwest Indian Ridge intercalated in Pleistocene diatom ooz...
A single deep-sea core (MD982156) of 30.30 meters long which is obtained during the MD III-IMAGES IV...
Carbonate-free portions of Upper Cretaceous to Holocene sediment samples from the Kerguelen Plateau ...
Four aspects of biogenic silica diagenesis are researched under this project: signatures of ongoing...
Cyclic changes in environmental conditions can be recorded in sediment by variations in their geoche...
In 2016 the International Ocean Discovery Program (IODP) Expedition 361 (“SAFARI”) recovered complet...
Deep-sea cores recovered from the N.W. Indian Ocean during Leg 23 of the Deep-Sea Drilling Project w...
Measurements of opal preservation in deep sea sediment cores have been presented in three ways: the ...
Since the 1970s, Ocean Drilling Program (ODP) and Deep Sea Drilling Program (DSDP) studies have docu...
The formation of marine opal-CT nodules or layers as early diagenetic deposits has been documented o...
From the equatorial Indian Ocean, carbonate-free portions of sediment samples of Paleocene to Miocen...
This study deals with the mineralogical variability of siliceous and zeolitic sediments, porcellanit...
The Mesoproterozoic porcellanite of the Vindhyan Super group is the oldest porcellanite deposit of ...
From the equatorial Indian Ocean, carbonate-free portions of sediment samples of Paleocene to Miocen...
Carbonate-free portions of Upper Cretaceous to Holocene sediment samples from the Kerguelen Plateau ...
A distinct porcellanite layer from the Southwest Indian Ridge intercalated in Pleistocene diatom ooz...
A single deep-sea core (MD982156) of 30.30 meters long which is obtained during the MD III-IMAGES IV...
Carbonate-free portions of Upper Cretaceous to Holocene sediment samples from the Kerguelen Plateau ...
Four aspects of biogenic silica diagenesis are researched under this project: signatures of ongoing...
Cyclic changes in environmental conditions can be recorded in sediment by variations in their geoche...
In 2016 the International Ocean Discovery Program (IODP) Expedition 361 (“SAFARI”) recovered complet...
Deep-sea cores recovered from the N.W. Indian Ocean during Leg 23 of the Deep-Sea Drilling Project w...
Measurements of opal preservation in deep sea sediment cores have been presented in three ways: the ...
Since the 1970s, Ocean Drilling Program (ODP) and Deep Sea Drilling Program (DSDP) studies have docu...