Jared Gooley is a Research Geologist at the USGS Alaska Science Center in Anchorage, AK. His work focuses on the tectonic and stratigraphic evolution of sedimentary basins.
Jared Gooley leads the Alaska Basins and Petroleum Systems Project, and his work supports the USGS Energy Resource Program. He also contributes to the Gulf Coast Geologic Energy Assessment and Research (GEAR) Project. Jared’s research investigates sedimentary basins using field and subsurface mapping, sediment provenance, and geochronology to reconstruct paleolandscapes and understand changing tectonic conditions. Ongoing work includes basin framework studies in Arctic Alaska and sediment provenance studies of the Gulf Coast and Atlantic margins. Past and ongoing projects also include Cenozoic tectonic evolution of the western United States and New Zealand.
Professional Experience
2022 - Present: Research Geologist, USGS Alaska Science Center, Anchorage, AK
2020 - 2022: USGS Geology, Energy & Minerals Science Center, Reston, VA
2014 - 2020: Graduate Fellow, Teaching, & Research Assistant, Stanford University, Stanford, CA
2012 - 2014: Exploration Geologist, Chevron, Eastern Gulf of Mexico Exploration, Houston, TX
2010 - 2012: Development Geologist, Chevron, East Texas Asset Development, Houston, TX
2008 - 2010: Graduate Research Assistant, University of Utah, Salt Lake City, UT
2009: Earth Science Intern, Chevron, Permian Basin Asset Development, Houston, TX
Education and Certifications
Ph.D. 2020 Stanford University Geological & Environmental Sciences
M.S. 2010 University of Utah Geology
B.S. 2008 Miami University Geology
Affiliations and Memberships*
Alaska Geological Society (AGS), 2020–present
Northern California Geological Society (NCGS), 2018–present
Society for Sedimentary Geology (SEPM), 2015–present
American Geophysical Union (AGU), 2014–present
American Association of Petroleum Geologists (AAPG), 2008–present
Geological Society of America (GSA), 2005–present
Science and Products
Gulf Coast Geologic Energy Research
Alaska Petroleum Systems
Crustal block-controlled contrasts in deformation, uplift, and exhumation in the Santa Cruz Mountains, California, USA, imaged through apatite (U-Th)/He thermochronology and 3-D geological modeling
Spatial distribution and variability of lobe facies in a large sand-rich submarine fan system: Neoproterozoic Zerrissene Group, Namibia
Peak Cenozoic warmth enabled deep-sea sand deposition
New Idria serpentinite protrusion, Diablo Range, California: From upper mantle to the surface
Detrital zircon provenance of the Cretaceous-Neogene East Coast Basin reveals changing tectonic conditions and drainage reorganization along the Pacific margin of Zealandia
Assessment of undiscovered gas resources in Upper Devonian to Lower Cretaceous strata of the western North Slope, Alaska, 2021
Non-USGS Publications**
**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
Science and Products
- Science
Gulf Coast Geologic Energy Research
The Gulf Coast Geologic Energy Assessments and Research (GEAR) project also conducts research on the properties and processes relevant to the Gulf Coast Jurassic-Cretaceous-Tertiary composite total petroleum system (TPS). This research aims to improve ongoing and future undiscovered, technically recoverable hydrocarbon resources assessments on the onshore and State waters portion of the Gulf Coast...Alaska Petroleum Systems
The Alaska Petroleum Systems project has three main objectives: (A) conduct research that increases our understanding of Alaska petroleum systems, (B) conduct assessments of undiscovered oil and gas resources, and (C) deliver energy-resource information to land and resource managers, policy makers, and the public. - Multimedia
- Publications
Crustal block-controlled contrasts in deformation, uplift, and exhumation in the Santa Cruz Mountains, California, USA, imaged through apatite (U-Th)/He thermochronology and 3-D geological modeling
Deformation along strike-slip plate margins often accumulates within structurally partitioned and rheologically heterogeneous crustal blocks within the plate boundary. In these cases, contrasts in the physical properties and state of juxtaposed crustal blocks may play an important role in accommodation of deformation. Near the San Francisco Bay Area, California, USA, the Pacific−North American plaAuthorsCurtis William Baden, David L. Shuster, Jeremy H. Hourigan, Jared T. Gooley, Melanie Cahill, George E. HilleySpatial distribution and variability of lobe facies in a large sand-rich submarine fan system: Neoproterozoic Zerrissene Group, Namibia
The deposits of the upper Neoproterozoic Zerrissene Group of central-western Namibia represent a large siliciclastic deep-water depositional system that showcases the intricacies of facies and architectural relationships from bed-scale to fan-system-scale. The lack of vegetation in the Namib Desert and regular east–west repetition of folded stratigraphy (reflecting ca 50% tectonic shortening) provAuthorsNora Maria Nieminski, Tim McHargue, Jared T. Gooley, Andrea Fildani, Donald R LowePeak Cenozoic warmth enabled deep-sea sand deposition
The early Eocene (~ 56–48 million years ago) was marked by peak Cenozoic warmth and sea levels, high CO2, and largely ice-free conditions. This time has been described as a period of increased continental erosion and silicate weathering. However, these conclusions are based largely on geochemical investigation of marine mudstones and carbonates or study of intermontane Laramide basin settings. HerAuthorsZachary FM Burton, Tim McHargue, Christopher H. Kremer, Richard B Bloch, Jared T. Gooley, Chayawan Jailka, Jake Harrington, Stephan A. GrahamNew Idria serpentinite protrusion, Diablo Range, California: From upper mantle to the surface
The New Idria serpentinite body in the Coast Ranges of California is a diapir that resulted from the interaction of the migrating Mendocino trench-ridge-transform fault triple junction, transpression, metasomatic fluids, and previously subducted oceanic crust and mantle. Northward propagation of the San Andreas fault progressively eliminated the original subduction zone, allowing seawater to penetAuthorsRobert G. Coleman, Jared T. Gooley, Robert T. Gregorory, Stephan A. GrahamDetrital zircon provenance of the Cretaceous-Neogene East Coast Basin reveals changing tectonic conditions and drainage reorganization along the Pacific margin of Zealandia
The Upper Cretaceous–Pliocene strata of New Zealand record ~100 m.y. of Zealandia’s evolution, including development of the Hikurangi convergent margin and Alpine transform plate boundary. A comprehensive, new detrital zircon U-Pb data set (8315 analyses from 61 samples) was generated along a ~700 km transect of the East Coast Basin of New Zealand. Age distributions were analyzed and interpreted iAuthorsJared T. Gooley, Nora Maria NieminskiAssessment of undiscovered gas resources in Upper Devonian to Lower Cretaceous strata of the western North Slope, Alaska, 2021
Using a geology-based assessment methodology, the U.S. Geological Survey estimated a mean of 1,407 billion (1.4 trillion) cubic feet of gas in conventional accumulations in Upper Devonian to Lower Cretaceous strata of the western North Slope, Alaska.AuthorsDavid W. Houseknecht, Tracey J. Mercier, Christopher J. Schenk, Thomas E. Moore, William A. Rouse, Julie A. Dumoulin, William H. Craddock, Richard O. Lease, Palma J. Botterell, Margaret M. Sanders, Rebecca A. Smith, Christopher D. Connors, Christopher P. Garrity, Katherine J. Whidden, Jared T. Gooley, John W. Counts, Joshua H. Long, Christina A. DeVeraNon-USGS Publications**
Kukla, T., Ibarra, D.E., Caves Rugenstein, J.K., Gooley, J.T., Mullins, C.E., Kramer, S., Moragne, D.Y., and Chamberlain, C.P., (2021), High-resolution paleotopography of the John Day region, Oregon, USA: Frontiers in Earth Science, doi: 10.3389/feart.2021.635181.
Gooley, J.T., Grove, M., and Graham, S.A., 2021, Tectonic evolution of the central California margin as reflected by detrital zircon composition in the Mount Diablo region, in Sullivan, R., Sloan, D., Unrah, J.R., and Schwartz, D.P., eds., Regional Geological Framework of Mount Diablo, California: Its Tectonic Evolution on the North America Plate Boundary: Geological Society of America Memoir 217, p. 305–329, doi: 10.1130/2021.1217(14).Gooley, J.T., Sharman, G.R., and Graham, S.A., 2021, Reconciling along-strike disparity in slip displacement of the San Andreas fault, central California, USA: Geological Society of America Bulletin, v. 133, no.7–8, p. 1441–1464, doi:10.1130/B35681.1.Hilley, G.E., Sare, R.M., Aron, F., Baden, C.W., Castillo, C.M., Dobbs, S.C., Gooley, J.T., Johnstone, S.A., Lieu, F., McHargue, T.R., Nevitt, J.M., Paull, C.K., Shumaker, L.E., Traer, M.M., and Young, H.H., 2020, Coexisting seismic behavior of transform faults revealed by high-resolution bathymetry: Geology, v. 48, p. 379–384, doi:10.1130/G46663.1.Dobbs, S.C., McHargue, T., Malkowski, M.A., Gooley, J.T., Jaikla, C., White, C.J., and Hilley, G.E., 2019, Are submarine and subaerial drainages morphologically distinct?: Geology, v. 47, doi: 10.1130/G46329.1.
Rech, J., Currie, B.S., Jordan, T.E., Riquelme, R., Lehmann, S.B., Kirk-Lawlor, N.E., Li, S., and Gooley, J.T., 2019, Massive middle Miocene gypsic paleosols in the Atacama Desert and the formation of the Central Andean rainshadow: Earth and Planetary Science Letters, v. 506, p. 184–194, doi: 10.1016/j.epsl.2018.10.040.Gooley, J.T., Johnson, C.J., and Pettinga, L., 2016, Spatial and temporal variation of fluvial architecture in a prograding clastic wedge of the Late Cretaceous Western Interior Basin (Kaiparowits Plateau), USA: Journal of Sedimentary Research, v. 86, n. 3, p. 125–147, doi:10.2110./jsr.2016.11.
Allen, J.L, Johnson, C., Gallin, W., Gooley, J., and Heumann, M., 2012, New technology and methodology for assessing sandstone composition: a case study using a Quantitative Electron Microscope Scanner (QEMSCAN), in Rasbury T., Hemming, S., and Riggs, N. (eds.), Geochemical Approaches to Provenance: Geological Society of America Special Publication, v. 487, p. 177–194.**Disclaimer: The views expressed in Non-USGS publications are those of the author and do not represent the views of the USGS, Department of the Interior, or the U.S. Government.
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government