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Active Deformation at the Transition from Subduction to Oblique Collision in the Culverden Basin, Aotearoa New Zealand
FILLING IN THE MARGINS: 3D ARCHITECTURE OF CONVERGENT MARGINS AND THE TRANSFERABILITY FROM SUBDUCTION TO COLLISION I POSTER
tectonophysics | 12 december 2023
Josh Sayre, Colin B. Amos, Timothy A. Stahl, Natha...
A complete picture of plate boundary evolution requires an understanding of active crustal deformation across subduction zone terminations. In Aoteoro...
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Hillslope Morphology Drives Variability of Detrital 10Be Erosion Rates in Steep Landscapes
GEOPHYSICAL RESEARCH LETTERS
29 august 2023
Roman A. DiBiase, Alexander Neely, Kelin X. Whippl...
The connection between topography and erosion rate is central to understanding landscape evolution and sediment hazards. However, investigation of ...
Diverse Deformation Mechanisms and Lithologic Controls in an Active Orogenic Wedge: Structural Geology and Thermochronometry of the Eastern Greater Caucasus
TECTONICS
16 december 2022
Alexander Robert R. Tye, Nathan A. Niemi, Eric Cow...
Orogenic wedges are common at convergent plate margins and deform internally to maintain a self‐similar geometry during growth. New structura...
Reverse Faulting Within a Continental Plate Boundary Transform System
TECTONICS
09 november 2021
Kirk F. Townsend, Marin K. Clark, Nathan A. Niemi
Contractional deformation is common along transform plate margins where plate motion is oblique to the plate boundary. While faults that accommodat...
Know (all!) your assumptions, investigate the sensitivities: Towards more rigorous thermal history modeling practices
FRONTIERS IN DATA HANDLING, STATISTICS, INTERPRETATION METHODS, AND MODELING - PART 2: LIGHTNING TALKS & POSTER PRESENTATIONS
general program | 16 september 2021
Kendra E. Murray, Nathan A. Niemi
Thermal history models are interpretive tools that incorporate data from chronometers and implement the published kinetics in the context of independe...
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Extensional Strain Heterogeneity in the Northern Basin and Range Continental Rift Recorded in Low-Temperature Thermochronology
INTRACONTINENTAL DEFORMATION: FROM THE SURFACE TO THE UPPER MANTLE IV POSTERS
tectonophysics | 11 december 2020
Nikolas C. Midttun, Nathan A. Niemi
The Basin and Range extensional province of western North America is perhaps the greatest natural laboratory for studying protracted continental exten...
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Hillslope morphology drives variability of detrital 10Be erosion rates in steep landscapes
IS THE WORLD IN A GRAIN OF SAND? DEVELOPMENTS AND APPLICATIONS OF DETRITAL METHODS FOR INTERPRETING SURFACE PROCESSES AND LANDSCAPE EVOLUTION I POSTERS
earth and planetary surface processes | 10 december 2020
Roman A. DiBiase, Alexander Neely, Kelin X. Whippl...
The measurement of in situ produced 10Be in quartz-bearing river sediment emerged as the primary tool for characterizing patterns in erosion rates acr...
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Deltas in an estuary: clumped and triple oxygen isotope analyses reveal isotopically depleted headwaters in the early Eocene of Southern CA
UNDERSTANDING THE TERRESTRIAL HYDROLOGICAL RESPONSE TO ATMOSPHERIC CO<SUB>2</SUB>: LESSONS FROM THE CENOZOIC AND INSIGHTS INTO THE FUTURE II POSTERS
paleoceanography and paleoclimatology | 10 december 2020
Julia Kelson, Sierra V. Petersen, Nathan A. Niemi,...
The δ18O of carbonate minerals that form in the hydrosphere is widely used to investigate hydrologic processes in ancient high CO2 worlds. However, a...
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