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1.
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The Eocene Thermal Maximum 2 (ETM2) and Hyperthermal 2 (H2) events are Paleogene hyperthermal events occurring ~53.7 mya and ~53.6 mya, respectively, and are characterize [...]
2016 |
Thesis |
Geology Department Student Theses 2015-16 |
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2.
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Clastogenic flows form by coalescing from accumulated spatter. Due to the viscous nature of spatter, agglutinate remobilization behaves according to the Bingham flow law. [...]
2016 |
Thesis |
Geology Department Student Theses 2015-16 |
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3.
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Exceptional coastal exposures of Miocene lava sequences on Banks Peninsula, New Zealand provide an opportunity to understand the emplacement processes of over-thickened l [...]
2016 |
Thesis |
Geology Department Student Theses 2015-16 |
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4.
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The Australian- Pacific plate boundary on the South Island of New Zealand comprises a zone of distributed deformation along active right lateral strike slip faults of the [...]
2016 |
Thesis |
Geology Department Student Theses 2015-16 |
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5.
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This project is focused on the study of climate, hydrology, and surface processes of western North America during the late Cretaceous (~75 million years ago) in what is n [...]
2016 |
Thesis |
Geology Department Student Theses 2015-16 |
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6.
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Lava flows of the intraplate Miocene Akaroa Volcanic Complex (AVC), Banks Peninsula, New Zealand, display a cyclical geochemical trend from picrite to benmoreite. When ob [...]
2016 |
Thesis |
Geology Department Student Theses 2015-16 |
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