Grant: Discovery Grants Program - Individual
Brock University
$22,000.00
Reconstructing geologic histories of volcanic fields on Earth and Mars
EF 2010-11
Résumé
The style, timing, distribution, and composition of small-volume basaltic volcanic eruptions are influenced by the climate and tectonic regime in which they form. The proposed research program investigates clusters of diverse volcanoes and volcanic rocks on both Earth and Mars.
Gusev Crater, Mars
The Mars Exploration Rover Spirit has discovered diverse volcanic and hydrothermally altered rocks. A technique is needed to differentiate primary rock compositions from overprinting alteration. Once rock compositions are deconvolved, they may be used to correlate layered units, alteration conditions, and the mapping of local alteration gradients in order to unravel the magmatic and aqueous history of Mars.
Terrestrial volcanic fields
I propose to investigate the lifespan, eruption rates, and compositional variability of volcanism in Fort Rock-Christmas Lake (FRCL Basin) in Oregon and in Red Hill Volcanic Field (RHVF) in New Mexico by geologic mapping, whole rock geochemistry, and 40Ar/39Ar geochronology. The timing and alteration of hydrovolcanism will give indication of past climate. Whole rock compositions and petrologic modeling will give insight to mantle melting in back arc setting and heterogeneity and assimilation rates of the upper (lithospheric) mantle.
Programme
Discovery Grants Program - Individual
Bénéficiaire
Emplacement
Ontario, Canada
Type de bénéficiaire
Academia
Type
Grant
Source
NSERC's Awards Data
Tel que publié
Application id
385955-2010
Name nom
Schmidt, Mariek
Department département
Earth Sciences
Organization id
22
Institution établissement
Brock University
Province en
Ontario
Province fr
Ontario
Country en
CANADA
Country fr
CANADA
Fiscal year exercice financier
2010
Competition year année de concours
2010
Award amount
22000
Program id
RGPIN
Program name en
Discovery Grants Program - Individual
Program name fr
Programme de subventions à la découverte - individuelles
Group en
Discovery grants programs
Group fr
Programmes de subventions à la découverte
Committee code
1506
Committee name en
Geosciences
Committee name fr
Géosciences
Area of application code
1203
Area of application group en
Advancement of knowledge
Area of application group fr
Avancement des connaissances
Area of application en
Earth sciences
Area of application fr
Sciences de la terre
Research subject code
4002
Research subject group en
Earth science
Research subject group fr
Sciences de la terre
Research subject en
Petrology, igneous and metamorphic geology
Research subject fr
Pétrologie, géologie ignée et métamorphique
Partie
1
Nb partie
5
Application title
Reconstructing geologic histories of volcanic fields on Earth and Mars
Keyword
NSERC
Application summary
The style, timing, distribution, and composition of small-volume basaltic volcanic eruptions are influenced by the climate and tectonic regime in which they form. The proposed research program investigates clusters of diverse volcanoes and volcanic rocks on both Earth and Mars.
Gusev Crater, Mars
The Mars Exploration Rover Spirit has discovered diverse volcanic and hydrothermally altered rocks. A technique is needed to differentiate primary rock compositions from overprinting alteration. Once rock compositions are deconvolved, they may be used to correlate layered units, alteration conditions, and the mapping of local alteration gradients in order to unravel the magmatic and aqueous history of Mars.
Terrestrial volcanic fields
I propose to investigate the lifespan, eruption rates, and compositional variability of volcanism in Fort Rock-Christmas Lake (FRCL Basin) in Oregon and in Red Hill Volcanic Field (RHVF) in New Mexico by geologic mapping, whole rock geochemistry, and 40Ar/39Ar geochronology. The timing and alteration of hydrovolcanism will give indication of past climate. Whole rock compositions and petrologic modeling will give insight to mantle melting in back arc setting and heterogeneity and assimilation rates of the upper (lithospheric) mantle.