81 Investigating Earth’s History With Continental Scientific Drilling
This session brings together research exploring Earth using subsurface geological datasets from continental scientific drilling, intended to be a broad showcase of research spanning structural geology, tectonics, natural hazards, sedimentology/stratigraphy, geothermal energy, critical minerals, deep biosphere, paleoclimatology, paleolimnology, and paleobiology.
Monday, 20 October 2025
8:00 AM - 12:00 PM
HBGCC, 214C
Drilling a Fault is No Bore: Preliminary Analysis and Lessons Learned from Drilling a 2-Kilometer Deep Corehole in the Rock Valley Fault Zone, Southern Nevada
Paper number: 81-0
Program: Technical Sessions
Time: 8:00 AM – 8:15 AM
Authors
-
Clayton FreimuthNevada National Security Sites, Mercury
-
Jesse BonnerLawrence Livermore National Laboratory, Livermore
-
Catherine SnelsonLos Alamos National Laboratory, EES-17, Los Alamos
-
William WalterLawrence Livermore National Laboratory, Livermore
-
Ethan AlgerLawrence Livermore National Laboratory, Livermore
-
Robert AbbottSandia National Laboratories, Albuquerque
-
Morgan AittamaNevada National Security Sites, Mercury
-
Nicholas DownsNevada National Security Sites, Mercury
-
Hali MontanoNevada National Security Sites, Mercury
-
Jennifer LarotondaNevada National Security Sites, Mercury
-
Devon SmithNevada National Security Sites, Mercury
-
Andrew MillerNevada National Security Sites, Mercury
-
Jesse PineNevada National Security Sites, Mercury
-
Jennifer WilsonSandia National Laboratories, Albuquerque
Abstract
The Rock Valley Fault Zone (RVFZ), located in southern Nevada, is an active, transtensional fault zone that developed in the late Paleogene and produced a sequence of shallow earthquakes in 1993. Understanding the RVFZ and Rock Valley stratigraphy is important because this section records syntectonic deposition and deformation associated with the onset of regional Basin and Range extension and may inform the Cenozoic tectonic evolution of southern Nevada. The Rock Valley Direct Comparison (RV/DC) project is investigating signature differences between subsurface explosions and earthquakes in this area. Conducting these dynamic experiments in a tectonically active region requires a comprehensive subsurface geology model of the region. Research conducted as part of the project is providing critical ground-truth constraints for the model. It will also improve our understanding of fault development and basin evolution in transtensional systems, offering valuable insight for both geologic hazard assessment and regional tectonic models. The RV/DC project recently drilled a 2-kilometer deep vertical corehole, named UE-27a, targeted near the hypocenter zone of the 1993 earthquake sequence. The uniquely shallow nature of these earthquakes provided a novel opportunity to drill near a recent fault. Drilling UE-27a produced PQ-sized core (85-mm diameter) from 0 to 1274 meters and HQ-sized core (64 mm diameter) from 1274 to the total depth of 2090 meters. The corehole was completed ahead of schedule, with our scientific goals of 98% core recovery and multiple datasets from downhole geophysical surveys accomplished. We present how we navigated challenging project conditions during the drilling program. We also show preliminary scientific data acquired from core and downhole geophysical surveys, which indicate a more developed Cenozoic basin than predicted. At least two distinct units with varied depositional environments are interpreted in the Cenozoic section of the core, which lies disconformably on Paleozoic carbonate rocks at 1183-meter depth. Subsequent detailed logging and interpretation of these data aid geologic modeling required for the RV/DC project, provide important context for basin evolution at Rock Valley, and give insight into a complex history of strain within the RVFZ. This work was done by Mission Support and Test Services, LLC, under Contract No. DE-NA0003624 with the U.S. Department of Energy and the National Nuclear Security Administration, Office of Defense Nuclear Nonproliferation. DOE/NV/03624--2227
Geological Society of America Abstracts with Programs. Vol. 57, No. 6
doi: 10.1130/abs/2025AM-412092
© Copyright 2025 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.