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1. (U-Th)/He chronology: Part 1. Data, uncertainty, and reporting

   https://doi.org/10.1130/B36266.1  

   Flowers, R.M.; Zeitler, P.K.; Danišík, M.; Reiners, P.W.; Gautheron, C.; Ketcham, R.A.; Metcalf, J.R.; Stockli, D.F.; Enkelmann, E.; Brown, R.W. (April 2022, GSA Bulletin)

   The field of (U-Th)/He geochronology and thermochronology has grown enormously over the past ∼25 years. The tool is applicable across much of geologic time, new (U-Th)/He chronometers are under continuous development, and the method is used in a diverse array of studies. Consequently, the technique has a rapidly expanding user base, and new labs are being established worldwide. This presents both opportunities and challenges. Currently there are no universally agreedupon protocols for reporting measured (U-Th)/He data or data derivatives. Nor are there standardized practices for reporting He diffusion kinetic, 4He/3He, or continuous ramped heating data. Approaches for reporting uncertainties associated with all types of data also vary widely. Here, we address these issues. We review the fundamentals of the methods, the types of materials that can be dated, how data are acquired, the process and choices associated with data reduction, and make recommendations for data and uncertainty reporting. We advocate that both the primary measured and derived data be reported, along with statements of assumptions, appropriate references, and clear descriptions of the methods used to compute derived data from measured values. The adoption of more comprehensive and uniform approaches to data and uncertainty reporting will enable data to be re-reduced in the future with different interpretative contexts and data reduction methods, and will facilitate inter-comparison of data sets generated by different laboratories. Together, this will enhance the value, cross-disciplinary use, reliability, and ongoing development of (U-Th)/He chronology. 

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2. Thermochronometric and textural evidence for seismicity via asperity flash heating on exhumed hematite fault mirrors, Wasatch fault zone, UT, USA

   McDermott, R. G. (January 2017, Earth and planetary science letters)

   Exhumed faults record the temperatures produced by earthquakes. We show that transient elevated fault surface temperatures preserved in the rock record are quantifiable through microtextural analysis, fault-rock thermochronometry, and thermomechanical modeling. We apply this approach to a network of mirrored, minor, hematite-coated fault surfaces in the exhumed, seismogenic Wasatch fault zone, UT, USA. Polygonal and lobate hematite crystal morphologies, coupled with hematite (U–Th)/He data patterns from these surfaces and host rock apatite (U–Th)/He data, are best explained by friction-generated heat at slip interface geometric asperities. These observations inform thermomechanical simulations of flash heating at frictional contacts and resulting fractional He loss over generated fault surface time–temperature histories. Temperatures of >∼700–1200 °C, depending on asperity size, are sufficient to induce 85–100% He loss from hematite within 200 μm of the fault surface. Spatially-isolated, high-temperature microtextures imply spatially-variable heat generation and decay. Our results reveal that flash heating of asperities and associated frictional weakening likely promote small earthquakes (Mw≈−3 to 3) on Wasatch hematite fault mirrors. We suggest that similar thermal processes and resultant dynamic weakening may facilitate larger earthquakes. 

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3. Hematite Frictional Behavior and He Loss From Comminution During Deformation Experiments at Slow Slip Rates

   https://doi.org/10.1029/2023JB027514  

   DiMonte, A A; Ault, A K; Hirth, G; Meyers, C D (March 2024, Journal of Geophysical Research: Solid Earth)

   Deformation experiments on hematite characterize its slip‐rate dependent frictional properties and deformation mechanisms. These data inform interpretations of slip behavior from exhumed hematite‐coated faults and present‐day deformation at depth. We used a rotary‐shear apparatus to conduct single‐velocity and velocity‐step experiments on polycrystalline specular hematite rock (∼17 μm average plate thickness) at slip rates of 0.85 μm/s to 320 mm/s, displacements of primarily 1–3 cm and up to 45 cm, and normal stresses of 5 and 8.5 MPa. The average coefficient of friction is 0.70; velocity‐step experiments indicate velocity‐strengthening to velocity‐neutral behavior at rates <1 mm/s. Scanning electron microscopy showed experimentally generated faults develop in a semi‐continuous, thin layer of red hematite gouge. Angular gouge particles have an average diameter of ∼0.7 μm, and grain size reduction during slip yields a factor of 10–100 increase in surface area. Hematite is amenable to (U‐Th)/He thermochronometry, which can quantify fault‐related thermal and mechanical processes. Comparison of hematite (U‐Th)/He dates from the undeformed material and experimentally produced gouge indicates He loss occurs during comminution at slow deformation rates without an associated temperature rise required for diffusive loss. Our results imply that, in natural fault rocks, deformation localizes within coarse‐grained hematite by stable sliding, and that hematite (U‐Th)/He dates acquired from ultracataclasite or highly comminuted gouge reflect minor He loss unrelated to thermal processes. Consequently, the magnitude of temperature rise and associated thermal resetting in hematite‐bearing fault rocks based on (U‐Th)/He thermochronometry may be overestimated if only diffusive loss of He is considered. 

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4. Thermal history of the northern Great Valley forearc basin, California

   Orme, D.A.; Romero, M.C.; Oleson, E.; Weis, N (August 2023, Geological Society of America Penrose)

   The Great Valley Forearc basin of California preserves >15 km of strata deposited during latest Jurassic-earliest Cretaceous to Eocene sedimentation. Along the western margin of the central-northern Great Valley forearc, the oldest basin strata are preserved as an eastward dipping homoclinal belt. Previous work on the thermal history of the western outcrop belt has constrained sub-normal geothermal gradients (<20C/km) during middle Cretaceous to Eocene time related to subduction refrigeration. However, the timing of maximum burial and subsequent exhumation is restricted to a few local studies. This study applies apatite and zircon (U-Th)/He and apatite fission track thermochronology to quantify maximum burial temperatures and the timing and rate of cooling of latest Jurassic-middle Cretaceous strata of the western homocline and neighboring subsurface along 350 km of the basin margin. Zircon (U-Th)/He dates range from ~167 to 85 Ma, which are either older or bracket corresponding depositional ages. Apatite fission track dates range from ~162 to 90 Ma, with the majority of grains between ~110-90 Ma. All apatite (U-Th)/He dates are less than 50 Ma, with most grains yielding dates between ~40-20 Ma. Preliminary integration of these data into thermal history models indicate that maximum burial temperatures did not exceed 120-180 C. The timing of basin cooling ranges based on locality, with the western outcrop yielding rapid exhumation starting between ~100-65 Ma and subsurface cooling at ~50 Ma. Final cooling to modern temperatures, as constrained by apatite (U-Th)/He dates, generally coincides with the transition to a transform margin after ~30 Ma. 

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5. Orogens of Big Sky Country: Reconstructing the Deep‐Time Tectonothermal History of the Beartooth Mountains, Montana and Wyoming, USA

   https://doi.org/10.1029/2022TC007541  

   Ronemus, Chance B.; Orme, Devon A.; Guenthner, William R.; Cox, Stephen E.; Kussmaul, Christopher A. L. (January 2023, Tectonics)

   Abstract Archean rocks exposed in the Beartooth Mountains, Montana and Wyoming, have experienced a complex >2.5 Gyr thermal history related to the long‐term geodynamic evolution of Laurentia. We constrain this history using “deep‐time” thermochronology, reporting zircon U‐Pb, biotite⁴⁰Ar/³⁹Ar, and zircon and apatite [U‐Th(‐Sm)]/He results from three transects across the basement‐core of the range. Our central transect yielded a zircon U‐Pb concordia age of 2,805.6 ± 6.4 Ma. Biotite⁴⁰Ar/³⁹Ar plateau ages from western samples are ≤1,775 ± 27 Ma, while those from samples further east are ≥2,263 ± 76 Ma. Zircon (U‐Th)/He dates span 686.4 ± 11.9 to 13.5 ± 0.3 Ma and show a negative relationship with effective uranium—a proxy for radiation damage. Apatite (U‐Th)/He dates are 109.2 ± 23.9 to 43.6 ± 1.9 Ma and correlate with sample elevation. Multi‐chronometer Bayesian time‐temperature inversions suggest: (a) Cooling between ∼1.90 and ∼1.80 Ga, likely related to Big Sky orogeny thermal effects; (b) Reheating between ∼1.80 Ga and ∼1.35 Ga consistent with Mesoproterozoic burial; (c) Cooling to ≤100°C between Mesoproterozoic and early Paleozoic time, likely reflecting continental erosion; (d) Variable Paleozoic–Jurassic cooling, possibly related to Paleozoic tectonism and/or low eustatic sea level; (e) Rapid Cretaceous–Paleocene cooling, preceding accepted proxies for flat‐slab subduction; (f) Eocene–Miocene reheating consistent with reburial by Cenozoic volcanics and/or sediments; (g) Post‐20 Ma cooling consistent with Neogene development of topographic relief. Our results emphasize the utility of multi‐chronometer thermochronology in recovering complex, non‐monotonic multi‐billion‐year thermal histories. 

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