Carmen Winn Mentor: Mary Reid Northern Arizona University NASA Space Grant Symposium
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Transcript of Carmen Winn Mentor: Mary Reid Northern Arizona University NASA Space Grant Symposium
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Carmen WinnMentor: Mary Reid
Northern Arizona UniversityNASA Space Grant Symposium
MANTLE LITHOLOGIES OF THE ZUNI BANDERA VOLCANIC FIELD: DETERMINED BY MINOR
ELEMENT RATIOS OF OLIVINE
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WHAT’S MELTING UNDER THE COLORADO PLATEAU?
• Young, mafic volcanism on the margins of Colorado Plateau: no clear mechanism of origin
• Evidence for heterogeneous source: what are the roles of multiple rock types melting?
Image fromwww1.newark.ohio-state.edu/
Image fromwww.utexas.edu/tmm/npl/mineralogy
and/or Pyroxenite?
Peridotite
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TRANSITION METAL RATIOS (Zn/Fe):A WINDOW INTO MELT SOURCE COMPOSITION
• Melting a rock: different elements/minerals behave differently as melting progresses
• When source controlled by olivine Zn/Fe shouldn’t change much
• Transition metals not very affected by degree of melt
• Olivine crystals can preserve element equilibrium in earliest stages of crystallization (closest to melting conditions)
Image from www.nvcc.edu/
Fe Zn Cr CoMg
Mn Ni V
Image fromserc.carleton.edu/
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VISITING A SOURCE: ZUNI BANDERA VOLCANIC FIELD
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WHY ZUNI BANDERA VOLCANIC FIELD?• Zuni Bandera Volcanic Field:
young, mafic field on eastern Colorado Plateau margin
• Mantle (melt source) samples found nearby at Mt. Taylor: testing the Zn/Fe ratio
• Rocks from wide range of melting depths present
Image from umanitoba.ca/geoscience/
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COLLECTING THE DATA: FIELDWORK
• Flows with high Mg content (closest to melting conditions) targeted for sampling
Map produced and analyzed in ArcGIS usingpreviously published data to target collection sites
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COLLECTING THE DATA: LABWORK• Grains of olivine separated
and mounted
• Composition determined with Laser Ablation ICPMS
• Data from ICPMS calibrated to known basalt and mantle standards
Laser Ablation
ICPMS
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2
3
4
5
6
7
8
9
10
11
12
Shallower melts
Deeper melts
Sub-continental mantle
San Carlos mantle standard
Basalt standards
Zn/F
e ra
tio
Hawaii standard
Iceland standard
Zn/Fe RATIOS COMPARED TO MELT EVOLUTION
Increased differential melting
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MELTING CONDITIONS OF ZUNI BANDERA BASALTS
1000 1100 1200 1300 1400 1500 1600 1700 1800 19000.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
4.0
4.5
5.0
5.5
6.0
Temperature (C)
Pres
sure
(Gpa
)(D
epth
)
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DISCUSSION AND CONCLUSIONS
• Zn/Fe ratio changes little with increasing degree of melting• Good ‘window’ for olivine-rich vs olivine-poor lithologies
• Zn/Fe ratios show more fertile source than standard CO Plateau and mid-ocean ridge (Iceland) mantle• Not high enough for pyroxenite, but fertile peridotite possible• Possible ‘plums’ of fertile mantle beneath the CO Plateau volcanic fields to
induce melting
• Wide range of depth and temperature of melting with normal trends
• In the future: • A more detailed analysis of the geochemistry of Zuni Bandera: other
minor element ratios and trace elements
• What do other volcanic fields show about CO Plateau mantle?
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ACKNOWLEDGEMENTS
A big thank you to:
Mary Reid, Research Mentor
Kathleen Stigmon and Nadine Barlow
Sean Rudzitis and Corinne LaViolette
Arizona NASA Space Grant
Northern Arizona University
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QUESTIONS?
Image from www.nps.gov/elma, 2012