Physical and chemical fractionation processes in subaerial and subaqueous pyroclastic rocks
Thesis/Dissertation
·
OSTI ID:6721006
Chemical and physical fractionation in subaerial rocks focuses upon the Cerro Toledo Rhyolite, a series of Pleistocene high silica rhyolite lave domes and tephras the crop out in the Jemez Mountains of northern New Mexico, USA. The Cerro Toledo Rhyolite is situated stratigraphically between the Lower Bandelier Tuff (LBT) and Upper Bandelier Tuff (UBT) and was erupted after the formation of Toledo caldera at 1.45 Ma and before that of Valles caldera at 1.12 Ma. The bulk of the Cerro Toledo Rhyolite tephra sequence exhibit progressive enrichment upsection of trace elements such as Rb, Cs, HREE, Y, Nb, Th, U and decline of Sr and K/Cs. Hf/Cs and La/Cs ratios initially decline, then level off upsection, indicating that crystallization of zicron and allanite/chevkinite was suppressed with time. Physical and chemical fractionation in subaqueous pyroclastic rocks focuses upon the current state of knowledge, lithofacies codes, and an Archean-age example from northwestern Ontario, Canada. A conceptual framework for understanding explosive subaqueous volcanism is presented comprising three essential aspects: (1) environment of the eruption, (2) orientation of the eruption, and (3) composition of the juvenile debris. A set of lithofacies codes for subaqueous volcaniclastic rocks is presented to describe deposits in the field and to make genetic and environmental interpretations. The codes may be used to distinguish between pyroclastic and epiclastic emplacement. Data collected from subaqueous volcaniclastic deposits at Confederation Lake, Ontario, reveal that the rocks are relatively primary products from explosive eruptions, probably from dome fragmentation, but that emplacement may not have occurred directly after eruption.
- Research Organization:
- Toronto Univ., ON (Canada)
- OSTI ID:
- 6721006
- Country of Publication:
- United States
- Language:
- English
Similar Records
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Journal Article
·
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·
OSTI ID:437410
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· J. Geophys. Res.; (United States)
·
OSTI ID:5940237
Volcanism and sedimentation along the western margin of the Rio Grande rift between caldera-forming eruptions of the Jemez Mountains volcanic field, north-central New Mexico, USA
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Thu Sep 21 00:00:00 EDT 2006
· Journal of Volcanology and Geothermal Research
·
OSTI ID:1459627
Related Subjects
58 GEOSCIENCES
580000* -- Geosciences
ACTINIDES
ALKALI METALS
ALKALINE EARTH METALS
CALDERAS
CANADA
CESIUM
CHEMICAL COMPOSITION
CHEMICAL REACTIONS
CHEMISTRY
CRYSTALLIZATION
ELEMENTS
ENRICHMENT
FEDERAL REGION VI
FRACTIONATION
GEOCHEMISTRY
GEOLOGY
HAFNIUM
IGNEOUS ROCKS
LANTHANUM
MECHANICS
METALS
MOUNTAINS
NEW MEXICO
NIOBIUM
NORTH AMERICA
ONTARIO
PHASE TRANSFORMATIONS
POTASSIUM
RARE EARTHS
RHYOLITES
ROCK MECHANICS
ROCKS
RUBIDIUM
SEPARATION PROCESSES
STRATIGRAPHY
STRONTIUM
THORIUM
TRACE AMOUNTS
TRANSITION ELEMENTS
URANIUM
USA
VOLCANIC ROCKS
VOLCANISM
YTTRIUM
580000* -- Geosciences
ACTINIDES
ALKALI METALS
ALKALINE EARTH METALS
CALDERAS
CANADA
CESIUM
CHEMICAL COMPOSITION
CHEMICAL REACTIONS
CHEMISTRY
CRYSTALLIZATION
ELEMENTS
ENRICHMENT
FEDERAL REGION VI
FRACTIONATION
GEOCHEMISTRY
GEOLOGY
HAFNIUM
IGNEOUS ROCKS
LANTHANUM
MECHANICS
METALS
MOUNTAINS
NEW MEXICO
NIOBIUM
NORTH AMERICA
ONTARIO
PHASE TRANSFORMATIONS
POTASSIUM
RARE EARTHS
RHYOLITES
ROCK MECHANICS
ROCKS
RUBIDIUM
SEPARATION PROCESSES
STRATIGRAPHY
STRONTIUM
THORIUM
TRACE AMOUNTS
TRANSITION ELEMENTS
URANIUM
USA
VOLCANIC ROCKS
VOLCANISM
YTTRIUM