Mineralogical, lithological, and geospatial data of drill cuttings from exploration production wells in Beowawe, Dixie Valley and Roosvelt Hot Springs. These data support whole rock analyses for major, minor and critical elements to assess critical metals in produced fluids from Nevada and Utah geothermal fields. The samples were analyzed by x-ray diffraction (legacy data) and then checked by thin section analysis.

This dataset contains 8 data tables provided in .csv format that contain sample location data, whole-rock geochemical data, argon-argon geochronologic data, sulfur, oxygen, and hydrogen isotope data, and mineralogical data from shortwave infrared spectrography (SWIR) and X-ray diffraction (XRD) analyses collected from igneous rocks on Brokeoff and Maidu volcanoes, northeastern California, USA. The data table files are Sample_Location_Data.csv, Argon_Data.csv, Geochemistry_Data.csv, SWIR_Data.csv, Whole_Rock_XRD.csv, Clay_XRD.csv, Sulfur_Isotope.csv, and Oxygen_Hydrogen_Data.csv. Fields in the data tables are defined in 8 corresponding data dictionaries, Sample_Location_Data_Dictionary.csv, Argon_Data_Dictionary.csv, Geochemistry_Data_Dictionary.csv, Whole_Rock_XRD_Dictionary.csv, Clay_XRD_Data_Dicitonary.csv, Sulfur_Isotope_Data_Dictionary.csv, Oxygen_Hydrogen_Isotope_Data_Dictionary.csv, and SWIR_Data Dictionary.csv. Analytical techniques are described in AnalyticalTechniques.txt.

This data release contains analytical data and images for a suite of drill core samples from the Mineral Hill alkaline complex (MHAC), northeastern Wyoming. Geochemistry data include major and trace element analytical results for 103 alkaline igneous rock samples. Images include hand sample photographs of halved core and full thin section images captured in transmitted, plane-polarized and cross-polarized light. Samples are from two core holes drilled by Humble Oil Company in 1970, and subsequently acquired and stored by Felix Mutschler at Eastern Washington University. The two skeletonized (incomplete) drill cores were acquired by the U.S. Geological Survey Geology, Minerals, Energy, and Geophysics Spokane office in 2019, through a co-operative agreement with Eastern Washington University. The collection contains full-core pieces from select intervals representative of the different lithologies and textures in the complex. Mineral Hill is a Paleogene-age, ring-shaped, multi-phase alkaline (miaskitic) igneous complex that intrudes Precambrian schists and lower Paleozoic units of the Tinton uplift on the northwest flank of the broader Black Hills uplift (Welch, 1974; Ray, 1979). The outer ring of the complex is composed of foid syenite and compositionally similar rocks, whereas clinopyroxenite (jacupirangite) and other foid-bearing mafic rocks (ijolite and melteigite) form an irregular inner ring. The center of the complex is composed of a central feldspathic diatreme breccia pipe that exhibits pervasive potassic and sulfidic alteration (DeWitt and others, 1986). Alkali feldspar trachyte/latite porphyry is exposed as large masses in a steep-walled, columnar-jointed zone peripheral to foid syenite of the Mineral Hill dome and as high-angle sills within the central area (Ray, 1979). Alkalic lamprophyres throughout the complex are thought to be related to clinopyroxenite and may have formed from a volatile-rich fraction of the pyroxenite magma (Ray 1979). Pseudoleucite porphyry and melteigite/feldspathic ijolite may be variations of foid syenite and foid clinopyroxenite, respectively. Historic mineral production in the area occurred between the 1870s and 1930s: principally alluvial gold, gold and silver at the Treadwell Mine, and gold and copper at the Interocean Mine. Exploration since 2000 has shown that gold and silver at the Treadwell Mine is related to epithermal-style mineralization and adularia-bearing potassic alteration (Eurasian Minerals Inc., 2016). Higher temperature, porphyry-style potassic alteration associated with gold and copper was identified near the Interocean Mine. Investigations of critical mineral potential in the area have focused on Precambrian pegmatites in the Tinton district which produced some cassiterite (Sn) and tantalite-columbite (Ta) ore, and the Spotted Tail and Sand Creek gold placers which produced some cassiterite (Sn) (Smith and Page, 1941; Hausel, 1990). The critical mineral potential of Paleogene intrusive rocks of the Mineral Hill complex has received comparatively little attention. All samples were analyzed by the U.S. Geological Survey contract laboratory, AGAT Laboratories. Major and trace element concentrations were determined by wavelength dispersive X-ray fluorescence, inductively coupled plasma-optical emission spectrometry or inductively coupled plasma-mass spectrometry (ICP-MS). Additional analytical methods included determination of carbonate carbon by combustion and infrared detection (IR); gold, platinum and palladium by lead fusion fire assay and ICP-MS; fluoride by ion-selective electrode; ferrous iron by titration; non-essential and essential water by gravimetric methods; total sulfur by IR; and gold and platinum group elements by nickel sulfide fire-assay followed by instrumental neutron activation analysis. For each method outlined above, an acceptable criteria for the data has been identified based on 1) if recovery of each element is within a designated percentage at

This data release is the result of a hydrogeochemical sampling campaign during summer 2021 to investigate whether high resolution geochemical analysis of waters for element chemistry can be used as an exploration tool for identifying gold-rich occurrences in parts of the Big Delta B-1 and B-2 quadrangles, within the Yukon-Tanana Upland region, Alaska. Historical USGS conventional stream sediment geochemical data yielded variable indications of geochemical anomalies in conventional stream sediment geochemistry results, probably related to relative exposure of mineralized rock. Previous studies of waters in the Pogo area (western part of current study) utilized conventional analytical methods not capable of measuring low concentrations of many elements (Wang et al., 2005). In the current study, water samples were collected from 36 stream sample sites, with a focus on streams around Black Mountain to the east and the Pogo Au deposit area to the west. Both areas have known gold-rich mineral occurrences. In the eastern Black Mountain area, this included the Gray Lead, Blue Lead, and Michigan prospects, among others (U.S. Geological Survey, 1996). Sampling in the Pogo area was restricted to streams outside Leise Creek area due to anthropogenic disturbance as part of mining. Stream water samples were collected in 2021 and analyzed for cation and anion concentrations using high-resolution ICP-MS for cations and ion chromatography (IC) for anions.

Bulk organic geochemical, major and trace element, and mineralogical data have been collected for core and cuttings samples of the Eocene Green River Formation from thirty-four wells in the Uinta Basin of Utah. The samples were collected from the U.S. Geological Survey Core Research Center in Denver, CO and the Utah Core Research Center in Salt Lake City, UT and represent multiple distinct stratigraphic intervals, including several that are being targeted for tight oil production in the northwestern part of the basin. These data have been collected since the previous assessment of the informal Uteland Butte member of the Green River Formation in 2015 and will inform future research and assessments of this unique lacustrine petroleum system. Much of this data is also relevant to various other petroleum-related resources (oil shale, gilsonite, tar sands) in eastern and southern parts of the basin.

Four boreholes (MW1, MW1UZ, MW2, MW2.1) were drilled in the fall of 2017 and summer of 2018 in upper Redwell Basin, a headwater catchment underlain by hydrothermally altered sedimentary rock in the Elk Mountains near the town of Crested Butte, Colorado. The boreholes were continuously cored using a wireline HQ-sized coring system and sample a combination of Quaternary-aged surficial colluvium and the Cretaceous-aged Mesaverde Formation. In-situ injection-based hydraulic tests were performed in MW1 and MW2 during drilling while advancing using a single-packer apparatus in tandem with an in-line flow meter and interval pressure monitoring. Borehole geophysical logging was performed in MW1, MW1UZ, and MW2.1 in the open holes. The boreholes were completed as vertically discrete nested monitoring wells. Pressure transducers have been deployed in selected wells to monitor groundwater level and fluid temperature over time. This data release includes borehole location and well completion information as well as related hydrologic and geophysical data. The borehole geophysical data directory contains borehole geophysical logs. The hydraulic test data directory contains in-situ packer test data and laboratory permeability/porosity results from selected core samples. The hydrologic monitoring data directory contains groundwater level and temperature data for selected wells.

Boreholes were drilled in 2017 and 2018 in Redwell Basin, a headwater catchment underlain by hydrothermally altered sedimentary rock in the Elk Mountains near the town of Crested Butte, Colorado. Two boreholes were completed as vertically discrete nested monitoring wells (MW1 as MW1A-MW1D and MW2.1 as MW2.1A-MW2.1C) and one borehole was completed as a single monitoring well (MW2 as RP8). Site locations and well construction are documented under the main page of this data release. Absolute (non-vented) pressure and temperature data loggers (PTDs) were deployed in these wells to monitor groundwater levels and fluid temperature over time. The period of record covers August 2018-September 2019 for all wells; the period of record for MW1D covers October 2017 to September 2019. Barometric pressure and surface temperature were monitored with a single PTD at the ground surface inside one well cover for the majority of the period of record. In addition to long-term monitoring, manual measurements of well water levels were collected as depth-to-water measurements (MW1A-D and RP8) or well-head gauge pressures (MW2.1A-C). Pressure, temperature, and water-level elevation data are provided for each well over the available period of record. Manual water level measurements are also provided. Unprocessed records are archived in a separate compressed (zip) directory. Attributes for all files are described in the data directory.