Events
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JSG | BEG | UTIG | EPS |
UTIG Seminar Series: Emily Warren-Smith, GNS Science, New Zealand
Start:October 1, 2020 at 2:30 pm
End:
October 1, 2020 at 3:30 pm
Location:
Zoom Meeting
Contact:
Constantino Panagopulos, costa@ig.utexas.edu
Speaker: Emily Warren-Smith, Seismologist, Geological Society of New Zealand
Host: Shuoshuo Han
Title: Stress and Fluid Processes During Northern Hikurangi SSEs: What Can We Learn From Microseismicity?
Abstract The occurrence of slow motion earthquakes, or slow slip events (SSEs), in subduction zones has been proposed to be linked to the presence of, and fluctuations in near-lithostatic fluid pressures (Pf) within the megathrust shear zone and subducting oceanic crust. In particular, the ‘fault-valve’ model is used to describe occasional, repeated breaching of a low-permeability interface shear zone barrier, which caps an overpressured hydrothermal fluid reservoir. In this model, a precursory increase in fluid pressure may therefore be anticipated to precede megathrust rupture. However, physical observations of such increases, and subsequent decreases, particularly within the subducting slab where hydrothermal fluids are sourced, remain elusive. Here we use earthquake focal mechanisms recorded on an ocean-bottom seismic network to identify changes in the stress tensor within subducting oceanic crust during four slow-slip events in New Zealand’s Northern Hikurangi subduction zone. We propose that these changes represent precursory accumulation and subsequent release of fluid pressure within overpressured subducting oceanic crust via a ‘valving’ model for megathrust slip behaviour. We also considermicroseismicity datasets alongside geophysical observations to identify spatially heterogeneous hydrological coupling between the two plates which we propose may be the source of fluids triggering shallow SSEs. We identify patches of co-located, differing seismic behavior, including: interface micro-seismicity, pre-SSE swarms, lower plate strike-slip earthquakes, long-term repeating earthquakes and elevated Vp/Vs zones. These patches correlate well with conductive interface regions constrained by magnetotelluric studies and thermal springs exhibiting mantle helium isotopic signatures. We propose these patches represent ‘vent’ sites where hydrological coupling between the plates is increased, facilitating episodic fluid valving which may be linked to SSE timing. These observations are important for future targeted efforts to monitor localised changes in fault zone properties during SSE cycles, in a bid to understand their physical behaviour and episodicity.
DeFord Lecture: Asmeret Asefaw Berhe
Start:October 1, 2020 at 4:00 pm
End:
October 1, 2020 at 5:00 pm
Location:
https://utexas.zoom.us/j/95162389947
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Looking deeper: role of sub-soils in Organic Matter Dynamics
About Dr. Asmeret Asefaw Berhe
Interests in soil science and global change science; understanding the effect of changing environmental conditions on vital soil processes, most importantly the cycling and fate of essential elements in the critical zone
DeFord Lecture Series
Since the 1940’s, the DeFord (Technical Sessions) lecture series, initially the official venue for disseminating EPS graduate student research, is a forum for lectures by distinguished visitors and members of our community. This is made possible through a series of endowments.
LEO Seminar Series: Scott Tinker and Varun Rai
Start:October 7, 2020 at 1:00 pm
End:
October 7, 2020 at 2:00 pm
Location:
https://utexas.zoom.us/j/96638474275
Host: Geoscience Leadership Organization for Women (GLOW)
The purpose of LEO is to create a more inclusive and educated community within the JSG by sharing and listening to each other’s stories. Speakers will interview each other and talk about why they are involved in Diversity, Equity, and Inclusion efforts and the heart behind their work. By learning more about why individuals are involved in DEI, we will broaden our understanding of the impacts the JSG is making on students, faculty, staff, and greater society. Taking initiative to get to know each other, ask questions, and Listen to Each Other is a skill that will propel us further to be leaders in the geosciences.
UT Paleontology Seminar
Start:October 8, 2020 at 11:00 am
End:
October 8, 2020 at 12:00 pm
Location:
Zoom link
DeFord Lecture: Kuheli Dutt
Start:October 8, 2020 at 4:00 pm
End:
October 8, 2020 at 5:00 pm
Location:
https://utexas.zoom.us/j/96111367919
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Advancing Diversity and Inclusion in the GeoSciences
About Dr. Kuheli Dutt
Chief diversity officer for Lamont-Doherty Earth Observatory of Columbia University; leads diversity, equity, and inclusion efforts at Lamont; interests in addressing implicit bias and STEM diversity.
DeFord Lecture Series
Since the 1940’s, the DeFord (Technical Sessions) lecture series, initially the official venue for disseminating EPS graduate student research, is a forum for lectures by distinguished visitors and members of our community. This is made possible through a series of endowments.
UTIG Seminar Series: Kennda Lynch, Lunar and Planetary Institute
Start:October 9, 2020 at 10:30 am
End:
October 9, 2020 at 11:30 am
Location:
Zoom Meeting
Contact:
Constantino Panagopulos, costa@ig.utexas.edu
Speaker: Kennda Lynch, Lunar and Planetary Institute
Host: Duncan Young
Title: S^3 (Subsurface, Subaqueous, and Salty): Looking For Life in All the Right Places
WCE Seminar Series
Start:October 9, 2020 at 12:00 pm
End:
October 9, 2020 at 1:00 pm
Location:
https://utexas.zoom.us/j/9627120440
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Habitability Seminar: Prof. Ryan P. Russell, UT Austin
Start:October 12, 2020 at 1:00 am
End:
October 12, 2020 at 2:00 am
Location:
Zoom Meeting
Contact:
Cornelia Rasmussen, crasmussen@utexas.edu
A seminar from the Center for Planetary Systems Habitability
Title: Spacecraft Dynamics for Outer Planet Moons Missions: Challenges of Searching for Life at Icy Worlds
Speaker: Prof. Ryan P. Russell, University of Texas at Austin
Abstract: Finding life beyond the Earth within our solar system is an age old quest. The icy moons of the outer planets are among the leading candidate search sites due to the abundance of water and internal heat sources driven by strong tides. In many observed cases, water transports to the surface and beyond via cracks in the dynamically shifting ice crust. Planetary scientists and other life hunters have long dreamed of sending in-situ robots to these exotic locations. While NASA has successfully executed and is currently planning flyby missions to icy world moons, orbiters and landing missions have not yet made it past the proposal stage. In this talk, we will discuss the challenges of designing such missions, primarily from a spacecraft dynamics perspective. Multiple phases of the mission will be discussed including the heliocentric planetary tour phase, the planetary capture and moon tour phases, the moon science orbit phase and optional landing excursions. The icy world moons lie deep in the gravity well of their gas giants parents. Exploration with current technology, therefore requires the extensive use of gravity assists in lieu of large propulsive maneuvers. The design space is extraordinarily large, as typical decade-long itineraries include hundreds of gravity assists and thousands of revolutions, while traversing every level of the sun-planet-moon solar system hierarchy. The open dynamical questions include which body to flyby and when, and where should the precious reserve of propellant be expelled. Intense radiation and perturbations due to third-body and non-spherical gravity make for a hostile environment near the planetary moons. Such constraints require hard limitations on radiation exposure and careful exploitation of the flow and equilibria of the natural dynamical system. Several recent and ongoing advances in the design of such missions will be discussed, including new algorithms to assess reachability, to solve the pathfinding combinatorial optimization problem, to locally optimize promising solutions in high fidelity, to find long-life science orbits, to solve and archive databases of periodic orbits, to identify feasible landing options, and to automate the whole process.
Softrock Seminar Series
Start:October 12, 2020 at 12:00 pm
End:
October 12, 2020 at 1:00 pm
Location:
Zoom link
UTIG Discussion Hour: Lindsey Yazbek, UT Green Labs
Start:October 13, 2020 at 2:00 pm
End:
October 13, 2020 at 3:00 pm
Location:
Zoom Meeting
Speaker: Lindsey Yazbek, Green Labs Coordinator, UT Green Labs
DeFord Lecture: Jérôme Gaillardet
Start:October 13, 2020 at 4:00 pm
End:
October 13, 2020 at 5:00 pm
Location:
https://utexas.zoom.us/j/91292288538
What the geochemistry of rivers tells us about critical zone processes and representation
About Dr. Jérôme Gaillardet
Chemical potamology; the global role of chemical weathering in the Earth’s chemical engine; focus on the « drainage basin » approach both at large scale and small scale; geochemistry of sediments transported by rivers and produced by chemical weathering in soils.
DeFord Lecture Series
Since the 1940’s, the DeFord (Technical Sessions) lecture series, initially the official venue for disseminating EPS graduate student research, is a forum for lectures by distinguished visitors and members of our community. This is made possible through a series of endowments.
LDE Seminar Series
Start:October 14, 2020 at 12:00 pm
End:
October 14, 2020 at 1:00 pm
UTIG Seminar Series: Jeanine Ash, Rice University
Start:October 16, 2020 at 10:30 am
End:
October 16, 2020 at 11:30 am
Location:
Zoom Meeting
Contact:
Constantino Panagopulos, costa@ig.utexas.edu
Speaker: Jeanine Ash, Rice University
Host: Chris Lowery
Title: Making and Breaking Molecules
Abstract: Methane is fundamentally significant to Earth’s habitability and the evolution of life. Its concentration in the atmosphere is the result of constant interplay between biological and geological process. My work focuses on the enzyme-level chemical reactions that make and break methane molecules, and how recent advances in isotope ratio mass spectrometry can provide new tools for tracing these reactions at the global level. In this talk I’ll introduce the concept of multiply-substituted isotopologues (commonly called “clumped” isotopes), and share experimental and case studies that show how these tools can be used to illuminate methane creation and destruction processes in the deep.
UTIG Discussion Hour: JSG Alumni Talks - Novi Labs
Start:October 20, 2020 at 2:00 pm
End:
October 20, 2020 at 3:00 pm
Location:
Zoom Meeting
Speaker: JSG Alumni Talks – Novi Labs: Kris Darnell, Kiran Sathaye, and Ted Cross
LEO Seminar Series: Leah Turner and Dev Niyogi
Start:October 21, 2020 at 1:00 pm
End:
October 21, 2020 at 2:00 pm
Location:
https://utexas.zoom.us/j/98581748000
Host: American Association of Petroleum Geologists (AAPG)
The purpose of LEO is to create a more inclusive and educated community within the JSG by sharing and listening to each other’s stories. Speakers will interview each other and talk about why they are involved in Diversity, Equity, and Inclusion efforts and the heart behind their work. By learning more about why individuals are involved in DEI, we will broaden our understanding of the impacts the JSG is making on students, faculty, staff, and greater society. Taking initiative to get to know each other, ask questions, and Listen to Each Other is a skill that will propel us further to be leaders in the geosciences.
UT Paleontology Seminar: Travis Stone (JSG)
Start:October 22, 2020 at 11:00 am
End:
October 22, 2020 at 12:00 pm
Location:
https://utexas.zoom.us/j/99193844298
Contact:
John A Moretti, jamoretti@utexas.edu
View Event
Exploring Reef Dynamics in the Late Triassic and Early Jurassic.
DeFord Lecture: Gaby Katul
Start:October 22, 2020 at 4:00 pm
End:
October 22, 2020 at 5:00 pm
Location:
https://utexas.zoom.us/j/91292288538
View Event
Evapotranspiration: From kinetic theory to the limits of plant life
About Dr. Gaby Katul
Micro-meteorology and near-surface hydrology with emphasis on heat, momentum, carbon dioxide, water vapor, ozone, particulate matter, water transport in the soil-plant-atmosphere system and implications to hydrological, ecological, atmospheric and climate change-related problems; new modeling tools to diagnose forest vulnerability to drought in order to better predict the future of the water and carbon cycles.
DeFord Lecture Series
Since the 1940’s, the DeFord (Technical Sessions) lecture series, initially the official venue for disseminating EPS graduate student research, is a forum for lectures by distinguished visitors and members of our community. This is made possible through a series of endowments.
UTIG Seminar Series: Michele Koppes, University of British Columbia
Start:October 23, 2020 at 10:30 am
End:
October 23, 2020 at 11:30 am
Location:
Zoom Meeting
Contact:
Constantino Panagopulos, costa@ig.utexas.edu
Speaker: Michele Koppes, University of British Columbia, Canada
Host: Demian Saffer
Title: Reading the story of climate change in the landscape
Abstract: Climate change is causing more than warmer oceans and erratic weather. It can also change the shape of the planet. Glaciers are a fundamental link between climate and the tectonic and surface processes that create topography. Mountain ranges worldwide have undergone extensive reshaping due to the erosive action of ice, and yet, the mechanisms that control the timing of this reshaping and the rate by which ice erodes remain poorly understood. We find a wide range of erosion rates from individual ice masses over varying timescales, suggesting that modern erosion rates exceed long-term averages by two to three orders of magnitude. We also see that glaciers in temperate climates erode 103 times faster than they do in the polar regions today. These rapid erosion rates are most likely due to the dynamic acceleration of ice masses as both air and ocean temperatures have warmed, and the ice has thinned and retreated over the past few decades. The repercussions of the increasing pace of erosion add to the already complex effects of climate change in polar and high mountain regions. Shrinking and accelerating glaciers destabilize valley slopes, increasing the risk of landslides and tsunamis, and deliver more sediment and nutrients to downstream basins, disrupting aquatic habitat and access to clean freshwater for mountain and coastal communities. The dramatic increase in recent erosion rates in the Arctic and the Antarctic Peninsula, two of the most rapidly warming regions in the world, suggest that polar ice masses are on the brink of a major geomorphic shift as mean temperatures warm above 0ºC.
UTIG Discussion Hour: Erik Fredrickson, University of Washington
Start:October 27, 2020 at 2:00 pm
End:
October 27, 2020 at 3:00 pm
Location:
Zoom Meeting
UTIG Seminar Series: Brian Boston, Lamont-Doherty Earth Observatory
Start:October 30, 2020 at 10:30 am
End:
October 30, 2020 at 11:30 am
Location:
Zoom Meeting
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
Speaker: Brian Boston, Lamont-Doherty Earth Observatory, Columbia University
Host: Harm van Avendonk
Title: From Construction to Collapse of the Hawaiian-Emperor Seamount Chain
Abstract: The Hawaiian-Emperor seamount chain is one of the most well-known geological features on Earth, covering ~6,000 km from the Island of Hawaii to the Meiji seamount near the Aleutian Trench. Consisting of a mixture of volcanic islands, atolls, seamounts and guyots, this feature was first explained by the motion of the Pacific plate moving over a focused spot of melting that has produced the age-progressive volcanic chain. Here, I will present recently acquired deep penetration, active-source seismic data collected with R/V Marcus G. Langseth as part of the Hawaiian-Emperor Seismic Experiment. During this two-cruise experiment in 2018 and 2019, R/V Langseth acquired multichannel seismic reflection data and wide-angle seismic data across the Hawaiian Island Chain, the youngest part of the chain, and along and across the Emperor Seamount Chain, the oldest part of the chain. This wide separation in space and time of formation enables us to investigate how magmatic addition has varied with time and study the time-dependent response of the oceanic lithosphere to the resulting volcanic load. Furthermore, gravitational collapse soon after the formation of the Islands produced some of the largest landslides on Earth, which were also targeted for the experiment. For acquisition of the seismic reflection data, we used a 6,600 in3 tuned air gun array and a 15-km-long hydrophone streamer cable, and for wide-angle seismic data, we used the same source with ocean-bottom seismometers spaced at ~15 km, with ocean-bottom seismometers provided by Scripps Institution of Oceanography, Woods Hole Oceanographic Institution, and GEOMAR Helmholz Centre for Ocean Research. Integrated analyses of data from both cruises allows us to capture the effects of wide variations in the time elapsed since loading, the age of the lithosphere at the time of loading, and timing and volume flux of magma emplacement. In addition, I will discuss potential volcanic spreading features from the Hana Slump caused by the collapse of the Haleakala Volcano on East Maui to the giant landslide of the Waianae Volcano on the western half of the Island of Oahu, highlighting the dynamic evolution of the Hawaiian-Emperor seamount chain.
MG&G Field Course Presentation DayMay, 30 2025Time: 10:00 AM - 12:00 PMLocation: ROC 1.603 Each Maymester, the University of Texas Institute for Geophysics (UTIG) offers a field course designed to provide hands-on instruction for graduate and upper-level undergraduate students in the collection and processing of marine geological and geophysical data. The course covers high-resolution air gun and streamer seismic reflection, CHIRP seismic reflection, multibeam bathymetry, sidescan sonar, sediment coring, grab sampling and the sedimentology of resulting seabed samples (e.g., core description, grain size analysis, x-radiography, etc.). Scientific and technical experts in each of the techniques first provide students with several days of classroom instruction. The class then travels to the Gulf Coast for a week of at-sea field work and on-shore lab work. Two small research vessels are used concurrently: one for multibeam bathymetry, sidescan sonar, and sediment sampling, and the other for high-resolution seismic reflection and CHIRP sub-bottom profiling. Students rotate daily between the two vessels and lab work. Upon returning to Austin, students work in teams to integrate data and techniques into a final project that examines the geologic history and/or sedimentary processes as typified by a small area of the Gulf Coast continental shelf. Students spend one week learning interpretation methods using industry-standard, state-of-the-art software (Focus, Landmark, Caris, Fledermaus). On the last day, students present their final project to the class and industry sponsor representatives. |