Physical Sciences and Mathematics Commons^™

Using Olivine-Hosted Melt Inclusions To Better Understand The Transcrustal Architecture Beneath Mount Baker (Koma Kulshan), North Cascades, Washington, Amanda Florea

WWU Graduate School Collection

The Schriebers Meadow cinder cone is located on the southern flank of Mount Baker and produced the Sulphur Creek lava flows and SC tephra deposits ~9.8 ka. Mount Baker, a Cascade volcano, is located ~50 km east of Bellingham, Washington. Previous work on the Sulphur Creek lava flows show that the eruption comprised two primary bulk rock compositions, ranging from basalt at the toe to basaltic andesite closer to the vent. However, little is known about the relative composition and eruption timing of the SC tephra from the same vent. In this thesis, I quantify compositional variations through the explosive …

Source And Parental Melts Of Poikilitic Shergottites: Implications For Martian Magmatism, Evan W. O'Neal

UNLV Theses, Dissertations, Professional Papers, and Capstones

Martian poikilitic shergottite meteorites are cumulate rocks that can be used to understand melt evolution on Mars from the bottom of the crust (~10 kbar) all the way up to near-surface shallow depths (~1 kbar). There is a general lack of knowledge regarding shergottites including, parental magma compositions, crystallization ages, and the location of the enriched geochemical source of the shergottites in the martian mantle. Through a comprehensive petrographic and geochemical study, we have attempted to better understand poikilitic shergottite formation and the evolution of the martian interior during the Amazonian period (~3 Ga – present day). We studied a …

Crystal Mush Dynamics Of Mount St. Helens And Lassen Volcanic Center: Insights From Melt Inclusions And Titanium-In-Quartz Thermobarometry, Jeremy S. Rosen

WWU Graduate School Collection

In order to better understand magma chamber dynamics at Lassen Volcanic Center (LVC) and Mount St. Helens (MSH) I examine quartz cathodoluminescent textures along with trace element abundances in quartz and compositions of quartz-hosted melt inclusions from multiple samples over a wide range of ages (LVC: 116 ka-1915; MSH: 272 ka to 84 ka). I use melt inclusion compositions to estimate quartz crystallization temperatures using zircon saturation thermometry and titanium abundances in quartz are used to estimate quartz crystallization pressures. When examined from core to rim within an individual grain, these data, along with internal CL-zoning textures reveal the dynamic …

Melt Inclusions And Their Application - New Perspective On The Subsurface Architecture Of Cerro Negro Volcano, Nicaragua, John M. Hamilton

Earth and Planetary Sciences ETDs

Volatiles are the drivers of volcanic eruptions and monitoring and measurement in quiescent times are the key in determining when unrest within a volcanic system is beginning leading to possible cataclysms. Previous studies have focused on direct measurements from volcanic plumes or fumaroles, however, this study proposes the use of melt inclusions from tephra to determine volatile contents from the 1992 eruption of Cerro Negro Volcano, Nicaragua. The analysis of melt inclusions adds a new technique to the volatile analytical toolbox and can help to determine volatile contents from past eruptions and their subsequent evolution within a volcanic system.

Though …

Magma Chamber Processes At Mutnovsky Volcano, Russia, Kelly L. Robertson

UNLV Theses, Dissertations, Professional Papers, and Capstones

This dissertation is composed of two manuscripts about the evolution of Mutnovsky Volcano in Kamchatka, Russia. Mutnovsky has been active for the past approximately 80,000 years, during which there was the formation and subsequent eruption of four major stratocones. These four eruptive centers, named Mutnovsky I, II, III, and IV from oldest to youngest, have a range of erupted product compositions from basalt to dacite. The first major goal of this project was to investigate the melt source for Mutnovsky. Whole rock trace element and Nd, Sr, and Pb isotopic data were used to determine that the melt source was …

Magmatic Sulfur And Chlorine Abundances At Stromboli, Italy And Their Role In The Formation Of Vesicle-Hosted Metal Alloys, Nichelle Lynn Baxter

Theses and Dissertations

Strand et al. (2002) discovered small metal alloy grains rich in Cu, Co, and Sn (maximum size 150 µm) in vesicles of lava from Kilauea Volcano. These alloys are also found in basaltic rocks of several Italian volcanoes. To better understand the origin of these metal-rich grains, bombs from Stromboli Volcano were examined. Two bomb types were collected from Stromboli: pumiceous bombs and scoriaceous bombs. Bulk rock trace element geochemistry indicates that there are no significant differences in Cu, Co, or Sn (the three major components of the metal alloys) between the pumiceous and scoriaceous bombs. Comparison of olivine melt …

Origin, Sedimentary Geochemistry, And Correlation Of Middle And Late Ordovician K-Bentonites: Constraints From Melt Inclusions And Zircon Morphology, Carsten Schirnick

Geology Theses and Dissertations

The present study of Paleozoic K-bentonites demonstrates that the geochemistry of melt inclusions and the morphology of zircons can be studied by inexpensive and simple-to-use methods, which rely on phenocrysts. Constraints are obtained that lead to (a) the origin of these altered volcanic ashes, (b) the geochemistry of ash-to-K-bentonite-alteration, and (c) the reliable correlation of extensively altered volcanic ashes (i.e. K-bentonites).
Silicic melt inclusions (i.e. non-devitrified) have been found in quartz and zircon phenocrysts contained within Ordovician and Devonian K-bentonites from New York State, the Upper Mississippi Valley, and Pennsylvania. Origin, source, and tectonic setting of the volcanism that produced …