International Ocean Discovery Program (IODP) Expedition 350 recovered roughly 2000 meters of volcaniclastic material. This paper focuses on the first 100 meters of this core which was almost entirely composed of tuffaceous mud. Tiny (micron) vitriclastic shards within this mud were analyzed to determine their chemistry and their morphology to make inferences about their source environment and eruptive mechanisms
Volcanic glasses recovered from four guyots during drilling along the Louisville Seamount Trail, sou...
Recent ocean sediments collected offshore Chile by Ocean Drilling Program Leg 202 contained layers o...
Glass separates from 115 ash layers derived from the Kamchatkan (DSDP Site 192; 34 layers), the east...
The inorganic portion of tuffaceous mud and mudstone in an oceanic island arc can be mostly volcanic...
To examine the processes and histories of arc volcanism and of volcanism associated with backarc rif...
Alteration of volcanogenic aluminosilicates (VAs) in marine sediments is recognized as critical in r...
Volcanic ash has long been recognized in marine sediment, and given the prevalence of oceanic and co...
During IODP NanTroSEIZE Expedition 322, four packages of tuffaceous sandstones (TST 1, 2, 3a, 3b) we...
This thesis discusses the processes that generate subaqueous, pumice-rich pyroclastic facies in belo...
none3noA detailed chemical investigation of volcanic glass fragments from volcaniclastic strata (6 t...
Precisely determined refractive indices of glass shards from 32 ash-rich, volcaniclastic sediments, ...
Volcaniclastic sediments of North Aoba Basin (Vanuatu) recovered during Ocean Drilling Program (ODP)...
Correlation of distal ash deposits with their proximal counterparts mainly relies on chemical and mi...
The 2012 silicic eruption at Havre volcano, in the Kermadec Arc, was the largest deep subaqueous eru...
Kīlauea Volcano is an outstanding natural laboratory in which to investigate basaltic volcanism, owi...
Volcanic glasses recovered from four guyots during drilling along the Louisville Seamount Trail, sou...
Recent ocean sediments collected offshore Chile by Ocean Drilling Program Leg 202 contained layers o...
Glass separates from 115 ash layers derived from the Kamchatkan (DSDP Site 192; 34 layers), the east...
The inorganic portion of tuffaceous mud and mudstone in an oceanic island arc can be mostly volcanic...
To examine the processes and histories of arc volcanism and of volcanism associated with backarc rif...
Alteration of volcanogenic aluminosilicates (VAs) in marine sediments is recognized as critical in r...
Volcanic ash has long been recognized in marine sediment, and given the prevalence of oceanic and co...
During IODP NanTroSEIZE Expedition 322, four packages of tuffaceous sandstones (TST 1, 2, 3a, 3b) we...
This thesis discusses the processes that generate subaqueous, pumice-rich pyroclastic facies in belo...
none3noA detailed chemical investigation of volcanic glass fragments from volcaniclastic strata (6 t...
Precisely determined refractive indices of glass shards from 32 ash-rich, volcaniclastic sediments, ...
Volcaniclastic sediments of North Aoba Basin (Vanuatu) recovered during Ocean Drilling Program (ODP)...
Correlation of distal ash deposits with their proximal counterparts mainly relies on chemical and mi...
The 2012 silicic eruption at Havre volcano, in the Kermadec Arc, was the largest deep subaqueous eru...
Kīlauea Volcano is an outstanding natural laboratory in which to investigate basaltic volcanism, owi...
Volcanic glasses recovered from four guyots during drilling along the Louisville Seamount Trail, sou...
Recent ocean sediments collected offshore Chile by Ocean Drilling Program Leg 202 contained layers o...
Glass separates from 115 ash layers derived from the Kamchatkan (DSDP Site 192; 34 layers), the east...