Events
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JSG | BEG | UTIG | EPS |
DeFord Lecture: Astrid Holzheid
Start:October 3, 2019 at 3:45 pm
End:
October 3, 2019 at 5:00 pm
Location:
JGB 2.324
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UTIG Seminar Series: Caroline Beghein, UCLA
Start:October 4, 2019 at 10:30 am
End:
October 4, 2019 at 12:00 pm
Location:
PRC ROC Room 1.603
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Host: Thorsten Becker
Title: Physical Constraints on the Oceanic Plate From Seismic Tomography and Thermodynamics
Abstract: The nature of the interface between the lithosphere and underlying asthenosphere in oceanic settings is still the subject of debate. In particular, questions remain regarding whether it is a temperature-dependent rheological transition, as expected in a thermal convection system, or it is additionally affected by the presence of melts and/or fluids. In this talk, I will present tomographic models of upper mantle seismic wave velocities and anisotropy under the Pacific plate and discuss their interpretation in terms of temperature, melt, and water content.
Our models resulted from the inversion of fundamental ande surface waves using both regularized inverse techniques and a Monte Carlo approach to quantify uncertainties. We found that both shear-wave velocity anomalies and azimuthal anisotropy patterns vary with seafloor crustal age. The thickness of the plate determined from isotropic velocities increases with crustal age, as expected for a thermal control, though uncertainties can be substantial. Similarly, the depth at which the azimuthal anisotropy is well aligned with the plate motion direction increases with age and tends to display a half-space cooling age dependence. In addition, we found that the depth of the Gutenberg discontinuity, which has been mapped in other studies with body wave data and is often associated with the lithosphere-asthenosphere boundary (LAB) and the presence of melts, coincides with high-vertical gradients in azimuthal anisotropy and is located within the age-thickening seismic lithosphere. We hypothesize that the Gutenberg discontinuity results from dehydration of the mantle underlying the mid-ocean ridge, resulting in a chemically depleted, viscous layer that translates away from the spreading center and becomes overprinted by lower temperatures as the plate cools down.
On the contrary, while radial anisotropy models obtained from inversions of Love and Rayleigh wave dispersion do not display any obvious age dependence, we found that they are generally less robust and reliable than azimuthal anisotropy and isotropic velocity models. They tend to differ in pattern depending on which surface wave dataset is employed and their uncertainties are sufficiently large that they cannot be used to constrain the LAB depth reliably.
To better constrain the physical nature of the LAB, we tested our isotropic shear wave velocity models against synthetic models calculated based on thermodynamic considerations for half-space and plate models. We tested the hypothesis that asthenospheric low seismic velocities may have a solid state origin and can be explained purely by thermal effects, including those on seismic attenuation, without any requirement for an additional effect of melt. Our results suggest that, while any direct signature of sub-ridge melt would be too small-scale to be resolved by our data, no significant fractions of melt are needed to explain the shear wave velocities. We note, however, that tomography uncertainties are large and some amount of melt could thus be present but not resolved. In addition, our tomography results are best explained by synthetic models that include a decrease in attenuation due to dehydration by melting at the ridge than by dry models or plate models. This is generally consistent with our azimuthal anisotropy model interpretation, but additional studies to refine the resolution of the anisotropy models are needed.
DeFord Lecture: Liviu Matenco
Start:October 10, 2019 at 3:45 pm
End:
October 10, 2019 at 5:00 pm
Location:
JGB 2.324
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UTIG Seminar Series: Chris Glein, Southwest Research Institute
Start:October 11, 2019 at 10:30 am
End:
October 11, 2019 at 12:00 pm
Location:
PRC ROC Room 1.603
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Speaker: Chris Glein, Southwest Research Institute San Antonio
Host: Duncan Young
Title: Enceladus: Pathfinder of alien oceans
Abstract: The past decade brought a remarkable transformation in humanity’s understanding of oceans. We used to really know only one ocean – the one that our species has grown up with on Earth. Now, we are starting to learn about other oceans that exist beyond Earth. This talk will focus on Saturn’s moon Enceladus, which is commonly called an “ocean world”. I will present a historical perspective of our exploration of Enceladus, primarily by NASA’s Cassini mission. I will also describe how we came to learn that Enceladus hosts a deep ocean under its icy exterior, and what the ocean is like mainly in terms of its geochemistry and potential habitability. Lastly, I will discuss ongoing efforts to use our experience at Enceladus to guide future exploration of Enceladus and other ocean worlds of great astrobiological interest, such as Jupiter’s moon Europa.
De Ford Lecture Series: Chris Bell
Start:October 17, 2019 at 3:45 pm
End:
October 17, 2019 at 5:00 pm
Location:
JGB 2.324
UTIG Seminar Series: Bob Kopp, Rutgers University
Start:October 18, 2019 at 10:30 am
End:
October 18, 2019 at 12:00 pm
Location:
PRC ROC Room 1.900
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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PLEASE NOTE: THIS WILL BE A REMOTE PRESENTATION
THE PRESENTATION WILL BE SCREENED LIVE AT ROC 1.900
Speaker: Bob Kopp, Rutgers University
Host: Pedro DiNezio
Title: Coasts in times of sea-level rise
Abstract: Around the world, sea levels are rising in response to warming oceans, melting glaciers, and shrinking ice sheets – and even faster rise is projected in the coming century. In this talk, I will explore the different physical processes driving sea-level rise, the geological record of past sea-level changes, methods for assessing the probability of different levels of future changes, and the implications for future coastal flood risks.
Hot Science - Cool Talk: Sustainability of Outer Space
Start:October 18, 2019 at 7:00 pm
End:
October 18, 2019 at 8:15 pm
Location:
William C. Powers Student Activity Center (WCP)
Contact:
Didey Montoya, didey@austin.utexas.edu, 5124714211
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Is it really true that there are over 20,000 junked satellites in outer space? What is their fate? Dr. Moriba Jah examines what we can do to make space safe, secure and sustainable in the long term.
Save the Date - Annual Tailgate Party
Start:October 19, 2019
End:
October 19, 2019
Location:
University of Texas at Austin campus
Contact:
Kristen Tucek, ktucek@jsg.utexas.edu, 512-471-2223
DeFord Lecture: Sharon Mosher
Start:October 22, 2019 at 3:30 pm
End:
October 22, 2019 at 5:00 pm
Location:
JGB 2.324
DeFord Lecture: Melissa Sims
Start:October 24, 2019 at 3:30 pm
End:
October 24, 2019 at 5:00 pm
Location:
JGB 2.324
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UTIG Seminar Series: Kelly Hereid, Chubb Corp.
Start:October 25, 2019 at 10:30 am
End:
October 25, 2019 at 12:00 pm
Location:
PRC ROC Room 1.603
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Speaker: Kelly Hereid, Chubb Corp.
Host: Pedro DiNezio
Title: Woolly problems in catastrophe modeling
Abstract: Insurance companies rely on catastrophe models, which simulate thousands of years of natural disasters, to quantify their exposure to extreme events. However, many of these extremes are highly susceptible to impacts from climate change. Here I highlight key emerging research areas in the science of catastrophe modeling that may be influenced by climate change, and how catastrophe modeling can be used to quantify economic impacts on the built environment. The effect of sea level rise on hurricane storm surge, expanding boundaries of hurricane impacts, compound disasters that incorporate extreme rainfall events, and high-resolution hazards with a complex relationship to climate change are all opportunities for climate research to inform risk management practices in the public and private sectors.
De Ford Lecture Series: Zoltan Sylvester
Start:October 31, 2019 at 3:30 pm
End:
October 31, 2019 at 5:00 pm
Location:
JGB 2.324
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UTIG Seminar Series: Melisa Diaz, The Ohio State UniversityMarch, 29 2024Time: 10:30 AM - 11:30 AMLocation: PRC 196/ROC 1.603 Speaker: Melisa Diaz, Assistant Professor, The Ohio State University Host: Benjamin Keisling Title: Biogeochemistry of a Greenland Ice-Marginal Lake Abstract: Due to polar amplification, nearly every glacier in Greenland has thinned and/or retreated in recent decades. The meltwater generated from these glaciers can take several paths, ultimately discharging into coastal waters or stored in closed-basin lakes. Ice-marginal lakes are a common but poorly understood feature in many glaciated regions, including Greenland. The lakes receive freshwater input from a combination of subglacial, supraglacial, terrestrial and meteoric sources, and a subset periodically drain, resulting in the rapid discharge of large volumes of water downstream (glacial lake outburst floods – GLOFs). In the case of drainages under adjacent marine terminating glaciers, GLOFs can deposit large amounts of sediment, nutrients, and freshwater directly into coastal waters and fjords. Lake Tininnilik, a large (~40 km2) ice-marginal lake that forms along Saqqarliup Glacier in west Greenland, drains ~2 km3 on quasi-cyclic decadal timescales into Saqqarleq Fjord to the north. For this talk, I will discuss the first comprehensive biogeochemical analysis of Lake Tininnilik and its potential influence on coastal primary productivity, including its major and minor nutrient stoichiometry and microbial composition. As the climate continues to warm, GLOFs are expected to become more frequent in Greenland. Therefore, it is imperative that we understand how these events can impact coastal community resilience. |
UTIG Discussion Hour: Kaitlin Schaible (UTIG)April, 02 2024Time: 2:00 PM - 3:00 PMLocation: ROC 2.201 |
UTIG Seminar Series: Chuanming Liu, UT AustinApril, 05 2024Time: 10:30 AM - 11:30 AMLocation: PRC 196/ROC 1.603 Speaker: Chuanming Liu, Distinguished Postdoctoral Fellow, UT Jackson School of Geosciences, Postdoctoral Fellow, University of Texas Institute for Geophysics Host: Thorsten Becker |
UTIG Discussion Hour: Soraya Alfred (UTIG)April, 09 2024Time: 2:00 PM - 3:00 PMLocation: ROC 2.201 |
UTIG Seminar Series: Tanner Miller, UTIGApril, 12 2024Time: 10:30 AM - 11:30 AMLocation: PRC 196/ROC 1.603 Speaker: Tanner Miller, Postdoctoral Fellow, University of Texas Institute for Geophysics Host: Peter Flemings |
UTIG Seminar Series: Crispin Little, University of LeedsApril, 12 2024Time: 2:00 PM - 3:00 PMLocation: PRC 196/ROC 1.603 Join us for a special seminar with Professor Cris Little. Speaker: Crispin Little, Professor, School of Earth and Environment, University of Leeds Host: Rowan Martindale Title: Biotic response to environmental perturbations in the Pliensbachian and Toarcian stages of the Lower Jurassic Abstract: The Lower Jurassic period was characterized by instability in global climate, with alternating greenhouse and icehouse states, and episodes of widespread oxygen depletion in the shallow marine environment. These episodes of oxygen depletion are marked by frequent intervals of increased organic carbon preservation in shallow marine sediments. The Pliensbachian stage of the Lower Jurassic was characterised by significantly cooler global temperatures than the preceding Sinemurian, and the following Toarcian stages, and ended with an extinction event (notably for ammonites) at the Pliensbachian-Toarcian boundary (Pl-To) ca. 184.2 Ma. About one Myr later the Toarcian Oceanic Anoxic Event (T-OAE) is characterized Corg rich black shale successions, particularly well developed in sedimentary basins in NW Europe, which display a negative ?13Corg excursion of -5 to -6‰, lasting 0.5 to 1.5 Myr. This excursion has been tied to a disruption of the global exogenic carbon cycle, but the ultimate source of the injected 12C is a matter of debate, with suggestions including methane hydrates, thermogenic methane produced by volcanism in the Karoo-Ferrar Large Igneous Province (LIP), wetlands, and permafrost destabilisation. The onset of the T-OAE in many (but importantly not all) sections is intimately linked to an extinction event that especially impacted the marine benthic macrofauna, but left the nekton largely unaffected. The recovery from this event is not well studied, but in one site, the Cleveland Basin of North Yorkshire, UK, although species richness recovered markedly as soon as environmental conditions ameliorated, other metrics of functional diversity and community structure did not attain pre-extinction levels until much later, some five million years after the extinction event. The talk will be of interest to those working on macroevolution, paleontology, and the effect of large scale climate change on marine ecosystems. |
UTIG Discussion Hour: Medha Prakash (UTIG)April, 16 2024Time: 2:00 PM - 3:00 PMLocation: ROC 2.201 |
UTIG Seminar Series: Emma \"Mickey\" MacKie, University of FloridaApril, 19 2024Time: 10:30 AM - 11:30 AMLocation: PRC 196/ROC 1.603 Speaker: Emma \"Mickey\" MacKie, Assistant Professor, Geological Sciences, University of Florida Host: John Goff |
Master\'s Thesis PresentationsApril, 19 2024Time: 2:00 PM - 5:00 PMLocation: JGB The Master of Science (MS) degree at the Jackson School of Geosciences is considered to be the professional degree for a career in the Geosciences. This degree is the foundation for students pursuing employment in the petroleum industry, environmental and hydrogeological fields, state and federal government agencies, and other related geoscience fields. Some students also use the MS degree as preparation for pursuing a Ph.D. The Energy & Earth Resources Interdisciplinary program provides the opportunity for students to prepare themselves in management, finance, economics, law and policy leading to analytical and leadership positions in resource-related fields. The private sector and government organizations face a growing need for professionals that can plan, evaluate, and manage complex resource projects, commonly international in scope, which often include partners with a variety of professional backgrounds. As requirements for these degrees, students must present a professional talk on Master\'s Thesis Presentations. |
Planetary Habitability Seminar SeriesApril, 22 2024Time: 1:00 PM - 2:00 PMLocation: PMA 15.216B UT Center for Planetary Systems Habitability Seminar Series. See website for speaker schedule and more details: View Events Join remotely: https://utexas.zoom.us/j/94052130734 In person: Classroom 15.216B, Physics, Math and Astronomy Bldg. UT Austin, Department of Astronomy 2515 Speedway, Stop C1400 Austin, Texas 78712-1205 |
UTIG Discussion Hour: Nicholas Montiel - PhD Talk (UTIG)April, 23 2024Time: 2:00 PM - 3:00 PMLocation: ROC 2.201 |
UTIG Seminar Series: Cornelia Rasmussen, UTIGApril, 26 2024Time: 10:30 AM - 11:30 AMLocation: PRC 196/ROC 1.603 Speaker: Cornelia Rasmussen, Research Associate, University of Texas Institute for Geophysics Host: Krista Soderlund |
Planetary Habitability Seminar SeriesApril, 29 2024Time: 1:00 PM - 2:00 PMLocation: PMA 15.216B UT Center for Planetary Systems Habitability Seminar Series. See website for speaker schedule and more details: View Events Join remotely: https://utexas.zoom.us/j/94052130734 In person: Classroom 15.216B, Physics, Math and Astronomy Bldg. UT Austin, Department of Astronomy 2515 Speedway, Stop C1400 Austin, Texas 78712-1205 |