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https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588088492729-89JH3BKI6W63AJ9GAWX7/1914384_159007800145_6966942_n_159007800145.jpg Tibet 2009 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588088492940-J52GEKKZWK6ZYVSKP5H7/1914384_159007805145_1720843_n_159007805145.jpg Tibet 2009 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588088493125-HRVGIYXLF40995DJL8VK/1914384_159007810145_6707950_n_159007810145.jpg Tibet 2009 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588088493285-8VT99QC52XJ9MKY5TSYN/1914384_159007815145_7979874_n_159007815145.jpg Tibet 2009 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588088493553-PQ23KTWC9K3Z6L0YQQXH/1914384_159007820145_1590989_n_159007820145.jpg Tibet 2009 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588088493728-9QFL1Y1PNOHB4FX8WCAT/1914384_159007825145_8067578_n_159007825145.jpg Tibet 2009 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588088493930-MR3DFZW6UCNAM4UO2UZT/1914384_159007830145_7742354_n_159007830145.jpg Tibet 2009 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588088494193-BD5JF3SGZD0ZI6W2PIB7/1914384_159007835145_1101619_n_159007835145.jpg Tibet 2009 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588088494312-5HX79P9YW8VKQTN7ILM4/1914384_159007840145_2195262_n_159007840145.jpg Tibet 2009 https://www.kurtsundell.com/home daily 1.0 2025-09-10 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1623999036557-OIO1P69UJ5SOTJHKIM25/isu_logo.png Home https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588347301690-OSM2NDEJSX6CQU9OK6VH/IMG_0308.JPG Home Standing in some huge(!!!) mud cracks in southern Tibet during a 2019 field campaign. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1538234948498-VC01WKE3GNR86APYM2RM/DSC00492.JPG Home https://www.kurtsundell.com/publications daily 0.75 2024-09-08 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1597604108293-DBI2A0RT0XNX6WP33X6R/IMG_4962.jpg Publications Tangra Yumco Rift in southern Tibet, summer 2019 https://www.kurtsundell.com/central-andes daily 0.75 2020-09-20 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598404314620-M4AQQTH2CIQK0MNGDG1S/AP.jpg Central Andes In the middle of nowhere, Altiplano https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598412575532-LCCX9HWB9KBDS63690OY/Figure_02_Age_Province_Map.png Central Andes Simplified age province map of South America modified from Pepper et al. (2016) and references therein. Andean Tectonics. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588187019049-7HEH3D1RLRGCHF0WSJN1/DSC00514.JPG Central Andes Early morning drive from Cusco to Punacancha. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1587234912456-23M3IA62WJSMZSM82JNJ/mudstone.png Central Andes Calcareously cemented mudstone interpreted at the transition from lacustrine to fluvial depositional environment. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1587239080928-YGKIUI7B2RA7AG316UI3/Figure_03_Stratigraphy_revised.jpg Central Andes Composite Cenozoic stratigraphic section of the northernmost Altiplano showing lithofacies codes to the right corresponding to observations and interpretations of depositional processes listed in Table 1 and described in section 3.1.1. The base of each section is specified by the beginning of the formation name to the left of the section. Paleocurrent data are shown as black arrows (north is up, arrow points toward sediment transport direction; N = stations, n = individual measurements). Conglomerate clast count results are shown as pie diagrams. From Sundell et al. (2018), Tectonics. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598408239554-E8N9UI9GBS5U6G4XKIHU/image-asset.png Central Andes Isotopic lapse rates used to calculate paleoelevation and surface uplift magnitude. Lapse rates include: thermodynamically-derived non-linear Rowley (2007); isotope-tracking general circulation model (GCM) with 25, 50, 75, and 100% of Andean elevations Insel et al. (2012); linear empirical ; and GCM with 50 and 100% Andean elevation Poulsen et al. (2010). Note the similarity in the Insel et al. (2012) and Rowley (2007) best-fit lapse rates. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598413424714-DX1W481VYXUSRR99MDF2/image-asset.png Central Andes Combined U-Pb–εHf(t) results plotted as bivariate kernel density estimates for (A) Andean zircons <200 Ma (5 Myr and 2ε unit set kernel bandwidths) and (B) pre-Andean zircons 2000–200 Ma (50 Myr and 2ε unit set kernel bandwidths). (C) Two-dimensional (2D) view of three-dimensional (3D) plot in part A. (D) 2D view of 3D plot in part B. DM = depleted mantle. White lines represent 95% of the maximum intensity in each plot. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598413343703-G55QS8X3F6Z884AYM5DI/Figure_04_U-Pb_eHf_Results.png Central Andes Combined detrital zircon U-Pb geochronology and εHf(t) geochemical results. (A) All U-Pb–εHf(t) data from the Cenozoic Altiplano from this study (n = 305). (B) Kernel density estimates of U-Pb ages from this figure (20 Myr set kernel), including ages from this study and from Sundell et al. (2018), and characteristic age ranges for detrital zircon data in the northern central Andes shown as vertical bars in all plots. (C) Combined U-Pb–εHf(t) results for Miocene strata (lower and upper Paruro Formation). (D) Combined U-Pb–εHf(t) results for middle to late Oligocene strata (lower and upper Punacancha Formation). (E) Combined U-Pb–εHf(t) results for Paleocene–Eocene strata (Quilque, Kayra, and Soncco formations). DM = depleted mantle. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598408707112-KHIDNMM9SHFLTZQQGW5B/Presentation2.png Central Andes Extreme modern crustal thickness of the northern Central Andes (Sundell et al., in prep). https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598406487624-VK0AZAWZVXH3UDGRBZAL/IMG_4491.jpg Central Andes Standing next to some overturned strata in the Altiplano https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598407733425-ZZPN9N5IJD8XTR6XHZWW/380.JPG Central Andes Another beautiful day of fieldwork in the Tincopalca basin in the Western Cordillera of southern Peru! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1587227088935-TDURCIUU5Y2EY46690M9/Figure_02_Geologic_Map_Study_Area.png Central Andes Geologic map of the study area modified from the Instituto Geológico Minero y Metalúrgico and Carlotto (2013). DZ = detrital zircon. From Sundell et al. (2018), Tectonics. Map Location Here! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598408109716-30FCT59ODECH75F65C21/image-asset.jpeg Central Andes Sampling location in the Eastern Cordillera in southern Peru near Macusani. Glass from these ~10 Myr volcanic rocks is in isotopic disequilibrium with the modern river water. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1587235459433-CKDQACOG0UJXMW0DMHU7/sstone.png Central Andes Overturned trough cross strata. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1587235411822-HEIJ7EPXI4PD0B5AJP3H/sstone2.png Central Andes Beautiful ripple cross stratification. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598408265262-2T05ELZ0FZKFVSLTG7PX/image-asset.png Central Andes Paleoelevation results compared to published paleoelevation estimates and ancillary geological data. (A) Sample locations for this and previous studies; only absolute elevation estimates are included. Results reveal variable surface uplift records consistent with previous studies for the (B) central Western Cordillera (15°S–15.5°S), (C) southern Western Cordillera (15.5°S–17°S), (D) Altiplano, and (E) Eastern Cordillera. Paleoelevations were calculated based on the thermodynamic lapse rate (Garzione et al., 2007) and incorporate a climate correction that accounts for Oligocene – Pleistocene global cooling. Youngest low elevation age for Kar et al. (2016) calculated assuming a linear sedimentation rate in the Descanso Formation. Shaded horizontal colored bars in parts B-E are ±1σ standard deviation of modern elevation. Scientific Reports. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598408160128-UTMMIO38OOED2NAY62R3/DSC04079.jpeg Central Andes Field assistants hard at work near Puquio in the Ayacucho region of southern Peru. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598407934190-56KUTPJJ7SKIQHHB4N68/Figure_01_Maps_Topo_Swaths_REVISION3.png Central Andes Study area, sample locations, and modern water elevation modeling. (A) Digital elevation model showing the northern extent of the Andean plateau generated from Shuttle Radar Topography Mission (SRTM) 90m elevation data. Physiographic regions characterizing the central Andes: AY = Ayacucho, WC = Western Cordilleran, AP = Altiplano. EC = Eastern Cordillera. Topographic swaths along a–a’ and b–b’ are 140 and 340 km wide, respectively; the dashed line is an arbitrary cutoff between the topographic swaths and modern water data shown in part (B). Modern water data include results from Bershaw et al. (2016), and volcanic samples include results from Saylor and Horton12. (B) Topographic swaths showing mean, minimum, maximum, and 1σ standard deviation elevation. Modern water measurements are color-coded to d-excess values. White circles are mean catchment elevations calculated from modern waters using a modified non-linear isotopic lapse rate (Rowley and Garzione, 2007). Sundell et al. (2019), Scientific Reports. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598413517366-STTCK52LD52KINEXB996/image-asset.png Central Andes Previously published (A) detrital εHf(t) data and (B) in situ εHf(t) data plotted over contoured bivariate kernel density estimates of U-Pb–εHf(t) for 2000–200 Ma from Fig. 5D. (C) Published in situ εNd(t) data from crustal provinces in South America. DM = depleted mantle. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598404282761-VK4KPC4X98ITKD3IULT7/image-asset.jpeg Central Andes Richard Styron measuring some strange blue stratigraphy https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598408764935-8OZ1NPIAH6A5FDIBGLY0/download.png Central Andes Method for deterining crustal thickness changes from intermediate igneous rocks with 60 to 70 percent silica by weight. This window avoids deep mafic melts that undergo major diversification during homogenization in the MASH zone, and highly fractionated melts or melting of metasedimentary rocks in the upper crust that tell us little about crustal thickness (Sundell et al., in prep). https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588185952967-PX1EFVCABCKDQYZ7ZDW7/Figure_12_Foreland_to_Hinterland_transition.png Central Andes (a) Foreland basin evolution in the context of a migrating foreland basin system (DeCelles & Giles, 1996). WC = Western Cordillera; EC = Eastern Cordillera. Timing of punctuated shortening (magenta boxes) inferred from mixture modeling. (b) Sediment accumulation rates calculated from measured sediment thicknesses and detrital zircon U-Pb maximum depositional ages (note that sediment compaction has not been taken into account). From Sundell et al. (2018), Tectonics. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598408585376-YLBD2JV3G2YNMLNK396R/IMG_2869.jpg Central Andes Sampling igneous rocks in the desolate far reaches of Western Cordillera in Bolivia. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598404224619-R7MDA2SGH9RBG3E45D40/DSC03943.jpeg Central Andes Joel Saylor measuring volcanic stratigraphy near Puquio, Peru https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598402769035-IKLQI89CGK4UKJHLMQ1R/412.JPG Central Andes Ausangate in the southern Peruvian Eastern Cordillera https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598412771564-TSL7LZWJEMUYVFFRPO2I/image-asset.png Central Andes Map of the study area and Cenozoic stratigraphy modified from Sundell et al. (2018). Geologic map was originally sourced from Instituto Geológico Minero y Metalúrgico (INGEMMET) and Carlotto (2013). Triangles on fault lines indicate thrust hanging wall. Green map units are Cretaceous sedimentary rocks. Light blue lines are measurement locations for the composite stratigraphic section. Blue filled circles are sampling locations for detrital zircon U-Pb and Hf analysis. Numbers right of Cenozoic timescale are single-grain maximum depositional ages. Paleocurrent measurements from (N = stations, n = individual measurements). Andean Tectonics. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1587226584740-K2R10C8MCSNE36NVU8R6/styron_jake.png Central Andes Richard Styron using the ‘hands of geology’ to properly orient this overturned Eocene strata. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1588186271051-R5ZOS92QUQNNYA4T007N/Figure_13_Foreland_Basins_Andean_Plateau.png Central Andes Sediment accumulation curves of foreland basin strata documented in the modern Altiplano and Eastern Cordillera for the Andean plateau. Note the systematically younger onset of rapid sediment accumulation to the south and thicker foredeep deposits in the north. From Sundell et al. (2018), Tectonics. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598404337407-7HFBBOD9A5L6GDAKMJ3I/AP1.jpg Central Andes Paola Zapata walking a beautiful section next to Lake Titicaca https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598413560996-15NZKCRHS3ZWDDRZ8XY9/image-asset.png Central Andes Comparison of Cenozoic Altiplano U-Pb–εHf(t) 95% density contours for 2000–200 Ma detrital zircons from central Andean modern rivers and beaches (Pepper et al., 2016), Cenozoic Altiplano sandstones (this study), and Paleozoic sandstones (Reimann et al., 2010). Note that the Paleozoic contour does not share the significant late Neoproterozoic isotopic pull down of the Cenozoic and modern U-Pb–εHf(t) contours. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1587234585505-ZCDW1T5ESBEVDJTT5839/dustin_cgl.png Central Andes Dustin Villarreal checking out razor sharp non-erosive surface at the base of a thick clast-supported cobble to boulder conglomerate. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598407977663-3SL8LEC1BXF8435FX5ND/SciReports_Figure_02_Modern_Water2.png Central Andes Modern water stable isotope results, lapse rates, and residuals. (A) Modern water δDw and δ18Ow (relative to VSMOW) compared to GMWL and color-coded to d-excess. Negative d-excess values are interpreted to be the result of moisture modified by evaporative effects, whereas positive d-excess values are interpreted to be the result of moisture recycling. Results include water data from Bershaw et al. (2016) (B) δDw values converted to elevation based on a non-linear isotopic lapse rate modified from Rowley and Garzione (2007). (C) Residuals (mean catchment elevations – modeled elevations); the majority of water values yield overestimates in catchment mean elevation resulting in a negative mean residual (-246 ± 427 m at 1σ). Sundell et al. (2019), Scientific Reports. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1587226033744-PXDKMM558XVHMSQ3I0I4/Figure_01_Maps.jpg Central Andes (a) Digital elevation model (DEM) of the Andean plateau from HYDRO1K data. (b) Physiographic regions of the northern extent of the Andean plateau. PC = Precordillera; SAZ = Subandean zone. (c) Regional geologic map of southern Peru showing Cenozoic stratigraphic formations and Paleozoic-Cenozoic intrusive units (modified from Carlotto, 2013) overlain upon a hillshade DEM generated from Shuttle Radar Topography Mission 90 m data. Sundell et al. (2018), Tectonics. Map Location Here! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1587227006611-OR9U6EB4WHHGKYPOX0OX/horiz_lam.png Central Andes Horizontally laminated very fine grained sandstone. Evidence of high velocity, shallow supercritical fluid flow. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598403949600-KXRJV5IOXOQ05QWTSXFV/IMG_2808.jpg Central Andes Active stratovolcanoes in the Bolivian Western Cordillera https://www.kurtsundell.com/geochronology daily 0.75 2020-09-20 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1597627501487-P8SJY8Q9DI0BPS7FSQU3/Figure_01_Four_Methods.png Geochronology Four methods for rapid acquisition of zircon U-Pb dates at rates of (a) 120 analyses/h, (b) 300 analyses/h, (c) 600 analyses/h, and (d) 1,200 analyses/h. All methods are time resolved analysis (TRA) at 0.2 s resolution where 1 index = 0.2 s. Data shown here are background subtracted. Time zero (t0) is the time laser firing begins and has a resolution of ± 0.2 s; background subtraction and on-peak measurements do not include indexes immediately before and after t0. Downhole correction is applied for the 120 analyses/h rate due to the long 15 s ablation time, all other acquisition methods use total counts (see Data Reduction section). Each plot shows real data from a test analytical session. Wash. = washout. Back. = background. Sundell et al. (2020), Geostandards and Geoanalytical Research. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1597611104797-0ACYCZYNFIZC2WFNBPAK/Nu7.jpeg Geochronology Arizona LaserChron Center Photon Machines Analyte-G2 ArF 193 nm excimer laser with a HelEx sample cell connected to a Nu plasma high-resolution (HR) multicollector mass spectrometer via aerosol rapid introduction system (ARIS). Photo: Martin Pepper. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1600622378763-VFIR9HCP9GMRRY0R25JA/image7.jpeg Geochronology Arizona LaserChron Center Nu plasma high-resolution (HR) multicollector mass spectrometer. Photo: Martin Pepper. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1597627662011-L00QEWIL5TJ4UZ3YQOC3/image-asset.png Geochronology Concordia diagrams. Purple ellipses are 1,200 analyses/h (3s/analysis). Green ellipses are 600 analyses/h (6s/analysis). Blue ellipses are 300 analyses/h (12s/analysis). Red ellipses are 120 analyses/h (30s/analysis). All uncertainty ellipses are 2σ. See Table 2 for reference material information. Note that the young reference materials (FCT and GHR1) are slightly positively discordant. This is because a compromise has to be made in the common Pb correction. Specifically, all panels in this figure share the same concordia line, and forcing these young zircons concordant by increasing the severity of the common Pb correction results in positively discordant older reference materials (e.g., Tan-Br-A and OG1). Sundell et al. (2020), Geostandards and Geoanalytical Research. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1600620506869-V4SP8BH2N820L5HBGRTT/Figure_09_MDS_Internal_Cross_Corr.png Geochronology Three-dimensional multidimensional scaling (MDS) plot of results from then detrital application (see Section 5). Red circles = 120 analyses/h; blue circles = 300 analyses/h; green circles = 600 analyses/h; purple circles = 1,200 analyses/h; white circle = all accepted dates produced in this study. Black arrows correspond to the nearest neighbor. The comparison metric used is 1 – Cross correlation of Kernel density estimates (KDE) with a 15 Myr bandwidth to produce dissimilarity measure used to produce the MDS plot. Sundell et al. (2020), Geostandards and Geoanalytical Research. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1597627376999-BTE3TPMMH9O9PRN9D0DF/image-asset.png Geochronology Time resolved analysis (TRA) plotted as time series for the first 90 s of sample measurement from Session 1 on April 19, 2019. (a) 120 analyses/h (30s/analysis): background measurements are applied sample by sample. (b) 300 analyses/h (12s/analysis): background measurements are grouped for every 4 samples. (c) 600 analyses/h (6s/analysis): background measurements are grouped for every 10 samples. (d) 1,200 analyses/h (3s/analysis): background measurements are grouped for every 25 samples. Sundell et al. (2020), Geostandards and Geoanalytical Research. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1597627541726-MKUQKIENIZ2XBIAWXGMH/Figure_05_TIMS_Offset_panels.png Geochronology Age offset plots. Circles = Session 1 (runs 1–4) on April 19, 2019. Squares = Session 2 (runs 5 – 8) April 20, 2019. (a) 120 analyses/h (30s/analyses) includes downhole correction, all other methods are calculated with total counts. (b) 300 analyses/h (12s/analysis). (c) 600 analyses/h (6s/analysis). (d) 1,200 analyses/h (3s/analysis). Offset is calculated as measured date – ID-TIMS date; left of 0% is young offset and right of 0% is old offset. Dates < 1,200 Ma are 206Pb/238U and ages > 1,200 Ma are 206Pb/207Pb. Random uncertainties are 1σ. Sundell et al. (2020), Geostandards and Geoanalytical Research. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1597627738566-KV1EDG1YZHH0HT49LDN6/Figure_08_CP40_PDPs_KDEs.png Geochronology Results for detrital sample CP40 (Dickinson and Gehrels 2008). Age distributions for eight separate analytical sessions. The same number of zircons were analyzed at each rate (i.e., 120 unknowns were analyzed at 120 analyses/h; 300 unknowns were analyzed at 300 analyses/h). Y-axis probability corresponds only to probability density plots (PDP). Kernel density estimates (KDE) were constructed using a 15 Myr bandwidth. CC = Cross-correlation. L = Likeness. S = Similarity. All quantitative comparisons were calculated using DZstats (Saylor and Sundell 2016) version 2.3 for macOS. Sundell et al. (2020), Geostandards and Geoanalytical Research. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1597630319387-BAN78ZV50LIDQVU090I9/laserchron%2Blogo.jpg Geochronology https://www.kurtsundell.com/agecalcml daily 0.75 2022-07-02 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598334556890-L6RVK4BL3452UNEHYHWO/laserchron%2Blogo.jpg AgeCalcML https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1607879388109-WFNGPEYZRT6R2VNL126Q/AgeCalcML_screengrab.png AgeCalcML https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599612445400-H03HVT7GS8HOUEIE81PN/USER_MANUAL_HStacked_Concordia.png AgeCalcML Horizontally-stacked Wetherill concordias — coming soon! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599611208630-K3VPXK1AYCRGKOFHX9SU/USER_MANUAL_Concordia.png AgeCalcML Basic Wetherill U-Pb concordia plotter — coming soon! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598331326248-UCGVIJU8EUH6RVN19JDU/USER_MANUAL_Download_and_Open_as_Desktop_Icon.png AgeCalcML Quick guide to downloading the source code and opening in MATLAB https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599612237768-Q309W6X7SGBD5XOBR3QQ/image-asset.png AgeCalcML Basic Weighted Mean Plotter with MSWD — coming soon! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599603737269-9H0JRFIXRFVLIDXOU1WL/USER_MANUAL_DR_Nu_U-Pb_IAM.png AgeCalcML Tutorial on producing publication-ready plots and data tables — coming soon! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599611879762-O2Y84B0MXDV2JJTI3B6N/image-asset.png AgeCalcML Tutorial on producing publication-ready plots and data tables — coming soon! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599612563120-2EJ146MXEWOG87EWQ876/image-asset.png AgeCalcML Vertically stacked Histograms, PDPs, and KDEs — coming soon! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598331187196-1YHP655I8367R848CK9L/INFORMATION_Geochron.org.png AgeCalcML Upload AgeCalcML results to the IEDA (Interdisciplinary Earth Data Alliance) Database https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598330569788-7CKHR35IDJX2R8WXGBML/image-asset.png AgeCalcML Latest MATLAB code available in our GitHub Repository, download and/or contribute! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598331262477-ST7E4KYF8BMFQPCVTN9H/USER_MANUAL_Download_and_Open_as_Desktop_Icon.png AgeCalcML Quick guide to downloading the programs for Mac (.app) and PC (.exe) https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/e1c78b14-5d3b-471d-8a13-a6a900a91b31/isu-stacked2.jpeg AgeCalcML - Make it stand out Whatever it is, the way you tell your story online can make all the difference. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598331049657-L1P9U4BXZL88RD30WC3A/INFORMATION_Quick_Description_and_Examples.png AgeCalcML Brief description of what AgeCalcML is and a few example plots, and proper citations https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598330954646-H90HSQ8D90G2A5YIP9QX/DOWNLOAD_Latest_Release_PC.png AgeCalcML Latest compiled release for PC. This requires the MATLAB Runtime Compiler (link here!) https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598331493162-MGCJ3T6QLZ6U84S1B9JW/image-asset.png AgeCalcML Tutorial on producing publication-ready plots and data tables https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599606658371-S1AMD8L6TD25B2IJW03J/image-asset.png AgeCalcML Tutorial on producing publication-ready plots and data tables — coming soon! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599604605236-LII6VKRMU1PWLF9S49PS/image-asset.png AgeCalcML Tutorial on producing publication-ready plots and data tables — coming soon! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598330454749-R0XFWXUBCQ2UEADQGNGA/DOWNLOAD_Latest_Release_Mac.png AgeCalcML Latest compiled release for Mac. This requires the MATLAB Runtime Compiler (link here!) https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598333181240-JBN77T3TM57UOJIOTECC/DOWNLOAD_Geochron.org_BLANK.png AgeCalcML Blank spreadsheet template that can be uploaded here at Geochron.org https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599616128651-4RLE09A6FDLPAPSLQFK8/image-asset.png AgeCalcML Example data for all five data visualization tools. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598330396632-0XPVIMJSEWZBEMRKOONL/DOWNLOAD_Example_Data.png AgeCalcML Example data sets; these work for all versions — Running in MATLAB or compiled programs https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599611440205-UQSBB4YZ7V2K7WDMJEGG/image-asset.png AgeCalcML Age Distributions: Histograms, PDPs, and KDEs — coming soon! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598333068863-FGGL3C8RO6LLXFM5TLNL/image-asset.png AgeCalcML Completed spreadsheet template that can be uploaded here at Geochron.org https://www.kurtsundell.com/hafniumplotter daily 0.75 2022-07-02 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598573938971-7K1UR53IQZO09G3HFPZI/DOWNLOAD_Latest_Release_PC.png HafniumPlotter Latest compiled release for PC. This requires the MATLAB Runtime Compiler (link here!) https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1607880095199-ZC9G9EF9AK95IRNKBZV5/Fig+13+Hf.png HafniumPlotter Figure from Thomas et al. (2020), Geosphere: “Detrital zircons and sediment dispersal in the eastern Midcontinent of North America.” Comparisons of εHft data for the Michigan, Illinois, and Forest City basins with respect to the Appalachian basin (A—Mississippian samples; B—Pennsylvanian–Permian samples, except those in panel C; C—Pennsylvanian samples with strong Pan-African/Brasiliano age concentrations). https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1607874398100-KH05OPOZUGEJ779T7EM2/HfPlotter.png HafniumPlotter Figure from Sundell et al. (2019), Andean Tectonics: “Sediment provenance and recycling of detrital zircons from Cenozoic Altiplano strata in southern Peru and implications for the crustal evolution of west-central South America.” Bivariate kernel density estimates of detrital zircon U-Pb and εHf(t) data from Peruvian Altiplano Cenozoic strata shown as three-dimensional volume (left) and two-dimensional view parallel to the z-axis (right). https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598573499675-0R49PAVO13DEHKATPGHH/image-asset.png HafniumPlotter Latest MATLAB code available in our GitHub Repository, download and/or contribute! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598575092519-OTNRQ5NJ1UTBBNCCJCQH/image-asset.png HafniumPlotter Tutorial on producing publication-ready plots and data tables — coming soon! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598573510817-C57QWBVFCJNBHTHNI8K6/INFORMATION_Quick_Description_and_Examples.png HafniumPlotter Brief description of what HafniumPlotter is and a few example plots https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1607879932504-5HQ8YM8TUKWQDE4HK26Z/HafniumPlotter_screengrab2.png HafniumPlotter https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599702705381-QJW5766W8LQWDV3KR44P/laserchron%2Blogo.jpg HafniumPlotter https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/0a39a75f-94cd-4c76-848a-c65d7faac4e6/isu-stacked2.jpeg HafniumPlotter - Make it stand out Whatever it is, the way you tell your story online can make all the difference. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1607880556598-3HTH8S4N2MB3QXV306N4/thomas_et_al_2019_Hf_fig.png HafniumPlotter Figure from Thomas et al. (2019), Geosphere: “Detrital zircons and sediment dispersal from the Coahuila terrane of northern Mexico into the Marathon foreland of the southern Midcontinent.” Plot of εHft data to compare results from Laurentia and the Appalachians, Gondwana/Amazonia (from Pepper et al., 2016), Southern Oklahoma igneous rocks (from Thomas et al., 2016), and Marathon foreland. The Appalachian data exclude identified Gondwanan accreted terranes in the Appalachian internides but include detrital zircons from Gondwanan sources in the Appalachian foreland (from Thomas et al., 2017). The Amazonia data are from various primary sources in South America (from Pepper et al., 2016). Data from the Wichita granites show the distinctive positive εHft values for Iapetan synrift rocks (Thomas et al., 2016). https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598575076842-SQHJAL3LXYJN51S9F9F9/image-asset.png HafniumPlotter Example data sets; these work for all versions — Running in MATLAB or compiled programs https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598573840558-PZDN9B077S9RUT7GB0MK/DOWNLOAD_Latest_Release_Mac.png HafniumPlotter Latest compiled release for Mac. This requires the MATLAB Runtime Compiler (link here!) https://www.kurtsundell.com/dznmf daily 0.75 2022-07-02 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599702079285-RR7AZG416HOUPW52IY15/laserchron%2Blogo.jpg DZnmf https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1607882267572-6IDC3JCD8K6LIC8DZMTG/DZnmf_screengrab.png DZnmf https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599660759014-TK7UR4132LK4XDOHER7C/image-asset.png DZnmf Example data sets; these work for all versions — Running in MATLAB or compiled programs https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599660770153-MU6F55TSR8SLVNA6JSC8/DOWNLOAD_Latest_Release_Mac.png DZnmf Latest compiled release for Mac. This requires the MATLAB Runtime Compiler (link here!) https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599660730718-4TB2DHN0AGQVUOI6B7OZ/image-asset.png DZnmf Latest compiled release for PC. This requires the MATLAB Runtime Compiler (link here!) https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599661854053-Y5K290Z8OXNZ8QOXMCHK/USER_MANUAL_Basic_Functionality.png DZnmf User manual for all functionality https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599702153513-83IHX9MWSPM2G4QM3O4O/ubc.png DZnmf https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599660715731-Y7S4GLPGN2XOC7RJP3BM/image-asset.png DZnmf Latest MATLAB code available in our GitHub Repository, download and/or contribute! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/c1e9795f-1410-4d55-9e6c-0308ca2c27b8/isu-stacked2.jpeg DZnmf - Make it stand out Whatever it is, the way you tell your story online can make all the difference. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599660690217-EEVMKPCQAS7LCYKJRKHA/INFORMATION_Quick_Description_and_Examples.png DZnmf Brief description of what DZnmf is, proper citation, and a few example plots https://www.kurtsundell.com/uh-data-reduction daily 0.75 2020-09-10 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599710066618-LHKL0SLU9A1REQ1N725F/logo-uh-2x.png UH Data Reduction https://www.kurtsundell.com/southern-tibet daily 0.75 2020-09-20 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599527489204-LUKWRYO7A29KWMOERIMH/lunggar.jpg Southern Tibet The North Lunggar Rift, west-central southern Tibet https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599527581708-4SB0KU76R9C3TVCUZAH9/IMG_5186.jpg Southern Tibet Deep in the Tangra Yumco rift footwall https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599528075262-5B3ZLOFK4BPDY5AHCRGE/lookin_busy.jpg Southern Tibet Lookin’ busy, sampling modern river sediments https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599528919032-D39HHXQ3VZEO32SBYQRC/IMG_5629.jpg Southern Tibet Caden Howlett, on a sampling transect psyched as usual! https://www.kurtsundell.com/collaborative-research daily 0.75 2020-09-20 https://www.kurtsundell.com/dzmds daily 0.75 2022-07-02 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599705984492-0OZVRNLL82I3B73VC4T9/USER_MANUAL_Basic_Functionality.png DZmds User manual for all functionality https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1607881704783-LU1XYNPD6BSJQFV3613R/DZmds_screengrab.png DZmds https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599702153513-83IHX9MWSPM2G4QM3O4O/ubc.png DZmds https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599702079285-RR7AZG416HOUPW52IY15/laserchron%2Blogo.jpg DZmds https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599705917707-LAFN5EQK4O2APBMOYL3W/INFORMATION_Quick_Description_and_Examples.png DZmds Brief description of what DZmds is, proper citation, and a few example plots https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/d21a1f64-0af5-448b-886b-a6b4d14a816a/isu-stacked2.jpeg DZmds - Make it stand out Whatever it is, the way you tell your story online can make all the difference. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599705807578-C2T3GJ382PI05C2HQGPQ/DOWNLOAD_Example_Data.png DZmds Example data sets; these work for all versions — Running in MATLAB or compiled programs https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599705779533-VQI0FCKQDWPP4L7HIM4T/DOWNLOAD_Latest_Release_PC.png DZmds Latest compiled release for PC. This requires the MATLAB Runtime Compiler (link here!) https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599705479351-8PQUR4VVBA4Y45FDR7A0/image-asset.png DZmds Latest MATLAB code available in our GitHub Repository, download and/or contribute! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599705763808-8BV6Y88G0EVOZF340Y77/DOWNLOAD_Latest_Release_Mac.png DZmds Latest compiled release for Mac. This requires the MATLAB Runtime Compiler (link here!) https://www.kurtsundell.com/dzmix daily 0.75 2022-07-02 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599708061855-7N3Z29QX7POAM3IO66SP/DOWNLOAD_Example_Data.png DZmix Example data sets; these work for all versions — Running in MATLAB or compiled programs https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599708013445-GGUIFZTEIS07OFZYBQAE/DOWNLOAD_Latest_Release_PC.png DZmix Latest compiled release for PC. This requires the MATLAB Runtime Compiler (link here!) https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/9c77f16d-e3b7-4702-a933-e4b3b9109ec0/isu-stacked2.jpeg DZmix - Make it stand out Whatever it is, the way you tell your story online can make all the difference. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599707920662-5NCQ75WPM331505SJTRE/DOWNLOAD_Latest_Release_Mac.png DZmix Latest compiled release for Mac. This requires the MATLAB Runtime Compiler (link here!) https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1607881450161-CE9WH44C6BPCSLYX6HQ4/DZmix_screengrab.png DZmix https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599708086989-8E9KMCE3R386CN4Q48XV/INFORMATION_Quick_Description_and_Examples.png DZmix Brief description of what DZmds is, proper citation, and a few example plots https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599707902781-812BTHUQJAAI75IQQEZ4/DOWNLOAD_Source_Code.png DZmix Latest MATLAB code available in our GitHub Repository, download and/or contribute! https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599708483956-FHEM9FX4H8BELX2O1BD8/USER_MANUAL_Basic_Functionality.png DZmix User manual for all functionality https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599702079285-RR7AZG416HOUPW52IY15/laserchron%2Blogo.jpg DZmix https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599702153513-83IHX9MWSPM2G4QM3O4O/ubc.png DZmix https://www.kurtsundell.com/dzstats daily 0.75 2022-07-02 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599709282522-AOQIYIA0J94LICT3HLBF/DOWNLOAD_Latest_Release_PC.png DZstats Latest compiled release for PC. This requires the MATLAB Runtime Compiler (link here!) https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599702153513-83IHX9MWSPM2G4QM3O4O/ubc.png DZstats https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1607881909809-A3FA6PU1H47MP6TLQ11I/DZstats_screengrab.png DZstats https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599709376041-64UGG51KMI0F7QQF5WE5/DOWNLOAD_Example_Data.png DZstats Example data sets; these work for all versions — Running in MATLAB or compiled programs https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599709533554-CH5T38DH6XZUGEX5QNHG/INFORMATION_Quick_Description_and_Examples.png DZstats Brief description of what DZmds is, proper citation, and a few example plots https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1f561a5e-bb87-473a-8e0a-1ecf8d2f9aef/isu-stacked2.jpeg DZstats - Make it stand out Whatever it is, the way you tell your story online can make all the difference. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599709564429-YHHWXGP5PE77ELQOW3D3/USER_MANUAL_Basic_Functionality.png DZstats User manual for all functionality https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599702079285-RR7AZG416HOUPW52IY15/laserchron%2Blogo.jpg DZstats https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599709233515-DMVNMO1GWWG5I3TNRNAX/DOWNLOAD_Latest_Release_Mac.png DZstats Latest compiled release for Mac. This requires the MATLAB Runtime Compiler (link here!) https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1599709196782-UBMRM15JTR8E9G1AKRLC/DOWNLOAD_Source_Code.png DZstats Latest MATLAB code available in our GitHub Repository, download and/or contribute! https://www.kurtsundell.com/resources daily 0.75 2025-09-10 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/4aadf96c-3ae0-4a5d-9df8-b6120100b2f9/ubc-vancouver.png Resources - Make it stand out Whatever it is, the way you tell your story online can make all the difference. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/9c780886-f9a3-4e2f-a8d2-9801a509b4e9/laserchron+logo.jpg Resources - Make it stand out Whatever it is, the way you tell your story online can make all the difference. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/e8bdbb60-31b1-49fe-a944-53364deb4e82/isu-stacked2.jpeg Resources - Make it stand out Whatever it is, the way you tell your story online can make all the difference. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/e2588ef3-1053-47ab-9b02-0bc89b71932e/uarkansas_logo.png Resources - Make it stand out Whatever it is, the way you tell your story online can make all the difference. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/1598334556890-L6RVK4BL3452UNEHYHWO/laserchron%2Blogo.jpg Resources https://www.kurtsundell.com/belt-db daily 0.75 2023-07-28 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/6b6666c5-0254-4d57-9815-5e7c43bb3f32/isu_logo.png Belt-DB - Make it stand out Whatever it is, the way you tell your story online can make all the difference. https://www.kurtsundell.com/students daily 0.75 2023-07-18 https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/0e3c266d-f4bd-4081-82ca-1cf38d612f55/IMG_0321.jpeg Students ISU graduate and undergraduate students on a recent field trip to Canyonlands, UT. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/eb0edfbd-8400-4fb2-9f35-7c598b3e41eb/IMG_3147.jpeg Students - Make it stand out Kyle recently completed his BS in Geology. In his undergraduate Kyle used detrital zircon to investigate hypothesized Belt Supergroup stratigraphy of the southernmost Lemhi Range near South Creek in Howe, ID. Kyle’s work characterized a previously unclassified quartzite unit that underlies the Neoproterozoic to Cambrian Wilbert Formation in an angular unconformity was investigated as a previously unidentified exposure of Belt Supergroup. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/5fd451b5-78eb-4958-95bd-4c21e7511924/Picture1.jpg Students - Make it stand out Cassie recently completed her BS. Her project focused on the Cenozoic geology of central Peru. Cassie’s project involved quantifying stable isotopic variations of modern waters along the Central Andes of South America where she collected over 130 water samples from modern rivers and streams across and along central and southern Peru, spanning nearly 4000 meters (>13,000 feet) in elevation, with samples as high as ~4600 meters (>15,000 feet!). Cassie determined a revised empirical lapse rate for the Central Andean rain shadow, and tested her results against theoretical lapse rates to determine the timing and rate of attainment of the high plateau of the Central Andes using ancient water preserved in volcanic glass. Cassie starts her MS degree this fall at the University of Oklahoma. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/ab9b4430-72a2-4045-82f9-05003c2be641/IMG_0120.jpeg Students - Make it stand out Robbie is a second-year MS student studying hypothesized Eocene wedge-top strata in southern Peru to test geodynamic drivers of retroarc foreland basin subsidence during the Cenozoic construction of the Central Andes. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/5fea4ecc-c0ca-4160-a0e0-a4cd1007c725/IMG_1947.jpeg Students Maria is a second-year MS student studying the sediment routing history of the Bengal Fan. Specifically, Maria is using mixture modeling to test hypotheses involving climate and tectonics to explain observed changes in sediment provenance at the Plio-Pleistocene transition. Maria recently completed her field work sampling major tributaries to the Ganges River drainage basin in northern India. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/11f97d73-1753-4f71-b4c4-9e6d8bd84c15/Bartelt_Cheyenne_Web.jpeg Students Cheyenne is a first-year MS student working on characterizing the detrital zircon geochemistry of major drainages in Idaho for comparison to whole rock chemistry to determine potential sources of bias in applications of detrital zircon. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/3b582f2e-e741-4fb7-9b36-535be82fe39f/IMG_7808.jpeg Students - Make it stand out Jon recently completed his MS focused on Mesoproterozoic strata of Leaton Gulch near Challis, ID. Jon applied detrital zircon geochronology and geochemistry to place previously unidentified strata into the context of the Belt Supergroup. https://images.squarespace-cdn.com/content/v1/590bb57a46c3c4d418bfa9b0/fd56f8a6-3748-4af9-a0ae-cc5f68246fe9/1613948572679.jpeg Students - Make it stand out Ryan completed a senior thesis focused on characterizing the Lu-Hf geochemistry of volcanic rocks in southern Peru for comparison to records of surface uplift. Ryan is currently a Ph.D. student at the University of California, Santa Barbara.