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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/v1/55f1cc9fe4b0039bab395d87/0e6c6726-1e06-441f-9eff-800d0c9863c3/Johnson+et+al+2022.jpg Home - 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/v1/55f1cc9fe4b0039bab395d87/99669eec-2b4b-4440-b02a-60f7b1a4b380/Nepal2017.jpeg Home - 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/v1/55f1cc9fe4b0039bab395d87/5fef21d7-5f3a-40ab-b029-8c3f63328a6c/Tetons2018.jpeg Home - 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/v1/55f1cc9fe4b0039bab395d87/1470854845747-U4WC3TYVP153HRBE3EVL/tetondaypanoramasmallwm.jpg Home http://uktectonics.com/what-we-do daily 0.75 2018-01-25 https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1479588184217-S8TT9M1F9DJ2W4ZGDICP/image-asset.jpeg Salt Tectonics & Basin Evolution Set-up of simplified preliminary model (shown below) designed to test development of margin-scale halostatic pressure. (a) At t=0.0 Myr, an autochthonous salt layer 5 km thick (pink) is overlain by an elastic material (gray) 2 km thick, which is in turn overlain by a progradational sediment wedge (teal) that thins in the basinward direction. (b-d) From t=1.3 Myr to t=3.0 Myr, differential gravitational loading of the salt layer by the sediment wedge drives salt from left to right, resulting in the development of an uplifted arch at the basinward end of the model. An elastic material without a defined failure envelope was chosen for the roof carapace to prevent failure and allow the maximum possible halostatic pressure and differential stress to be generated at the downdip end of the margin. https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1516904175157-E8TIWJ8EJMOOAJN6WN5N/Fig+18-Diapir+mechanisms.jpg Salt Tectonics & Basin Evolution https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1479588212173-NLE0SPEQN6R4KF4NPQ2R/image-asset.jpeg Salt Tectonics & Basin Evolution Results of simplified preliminary model shown above. An elastic material was chosen for the cover sequence to prevent failure of the roof and determine the maximum pressure load that could be placed on the roof in the downdip end of the halostatic system. (c-e) Differential stress (max. stress minus min stress in the plane strain model) after 3 Myr of sediment loading. (d) Differential stress shows two compressional 'hotspots' on the underside of the downdip end of the arch (salt-roof carapace contact) and in the toe of the system where thrust faulting is often observed in natural systems. An extensional hotspot (>175 MPa diff. stress) is also recognized on the surface of the downdip arch. All three zones would be primary regions for failure localization in most natural systems. (e) Contours of differential stress overlain with vector orientations of minimum (red) and maximum (blue) compressive stress to show the complexity of the stress (and presumably strain) field that develops in these systems. It is important to note that all of these results are modeled as drained conditions, so pore pressure is not currently considered. https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1470854957543-LV22O08ANU3N7IUKU8VS/13442657_10104406979100413_2965007685907238905_o.jpg Salt Tectonics & Basin Evolution http://uktectonics.com/projects daily 0.75 2023-12-06 https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1599186755338-NLOGADT4T5B8KT95NPO2/Thrust_model.jpg Orogenic Evolution https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1599185141571-GLGCJEUERMYP9FB6YPWR/Orogen_model+copy.jpg Orogenic Evolution https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/dbb8fa13-a592-4bc2-a3d4-54cf7d2928be/STD_system_Annapurna.jpeg Orogenic Evolution - Make it stand out Sheared feldspar megacrysts in the Duerali normal-sense shear zone (top-down-to-the-north, to the right in the photo), South Tibetan Detachment system, Annapurna region, Nepal (2017 Field Season) https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/14c5ef71-36bb-4834-8b4c-6f0b2b319f2e/Langtang.jpeg Orogenic Evolution - Make it stand out Mountains of Langtang National Park as seen from the village of Kyangin Gompa, Nepal (2017 Field Season) https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/ce576658-6d19-4880-95e3-5b3799246c99/Channel_model.jpg Orogenic Evolution - Make it stand out The upper cross-section shows a schematic model of crustal channel flow, wherein melt-weakened crust flows from beneath the Tibetan plateau to be exhumed at the topographic break at the front of the Himalayan collisional system. Approximate position of the cross-section is shown on the map to the left. The lower cross-section shows the results of Reference Model 1 of Beaumont et al. (2004), which predicts the flow of crustal material from beneath the Tibetan plateau due to long wavelength lithostatic stress gradients driving orogen-normal flow of melt-weakened mid-crustal material. Black arrows indicate flow vectors in this modeled system. https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1701350035031-3K4XEN2AOVUSYQIURGIC/IMG_2141.jpg Orogenic Evolution http://uktectonics.com/projects-1 daily 0.75 2017-01-28 https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1479661037895-FLZW7V442V0PO078SVP7/13730986_10104523611777593_4921669283543447236_o.jpg Active Tectonics & Landscape Response https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1479661038746-4EXYK7F6ATW345OMVOWF/13698096_10104523608124913_3617593052745002255_o.jpg Active Tectonics & Landscape Response https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1479661428336-EIBVR5HKE601002ZSXQU/1275918_10101942087023893_1107825330_o.jpg Active Tectonics & Landscape Response https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1479661501465-5IMOLSAU35IFJK4KG018/13723980_10104545407768253_1977674311938874459_o.jpg Active Tectonics & Landscape Response https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1479661609547-HCBH5Z4EU1SK8VZSIG7X/13734932_10104523606538093_4019835004472179491_o.jpg Active Tectonics & Landscape Response https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1479661608572-WDUU8WIDUHE87K4FHP5B/13701085_10104545407344103_89233876541724994_o.jpg Active Tectonics & Landscape Response https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1479661711319-6EMMN102L6K0WG5SNSN2/13723980_10104545407768253_1977674311938874459_o.jpg Active Tectonics & Landscape Response http://uktectonics.com/teton-fault daily 0.75 2018-11-06 http://uktectonics.com/new-page daily 0.75 2020-02-23 http://uktectonics.com/erasing-mountain-ranges daily 0.75 2020-11-22 http://uktectonics.com/hazards daily 0.75 2023-11-23 http://uktectonics.com/people daily 0.75 2023-12-06 https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/8f4dcfbc-422c-40c3-af89-c7c5a0bda80e/Terri.jpg People - 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/v1/55f1cc9fe4b0039bab395d87/28ce2c64-9e85-4c5d-ab1b-7af50e3fb27b/Nicky.jpg People - 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/v1/55f1cc9fe4b0039bab395d87/46eb79d0-9a99-45c9-b74b-e30c76baaaa6/Gillian.jpg People - 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/v1/55f1cc9fe4b0039bab395d87/3ad3d7d0-0656-4d26-b51a-e98171018198/Riley.jpg People - 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/v1/55f1cc9fe4b0039bab395d87/cbd6837f-ceaf-4ccd-8235-68b3b7cd7fa2/JT.jpeg People - 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/v1/55f1cc9fe4b0039bab395d87/b670b714-7b84-42d7-9417-cb2e507c8339/elisha_tetons.jpg People - 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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/v1/55f1cc9fe4b0039bab395d87/e7fe1a68-2a2e-4a5a-8004-6cdc846db2f8/madison_tetons.jpg People - 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/v1/55f1cc9fe4b0039bab395d87/72241ab5-a7d2-461a-bd3a-3b88d75f248c/Rachl.jpg People - 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/v1/55f1cc9fe4b0039bab395d87/5b5d4274-a294-4648-a4ad-d3b95141c28a/Autumn.jpg People - Make it stand out Whatever it is, the way you tell your story online can make all the difference. http://uktectonics.com/ree-petrochronology daily 0.75 2023-12-06 https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/af50c10b-a975-4691-ac70-73edca039405/Fig+%3F-Zircon+Maps.jpg REE Petrochronology - Make it stand out Geologic map of the southern Appalachian Blue Ridge and Inner Piedmont in parts of TN, NC, SC, and GA. Data highlights our ongoing campaign style of geochronology and thermochronology to resolve the spatial and temporal “footprints” of Paleozoic metamorphism, deformation, and exhumation in the complex southern Appalachian system. This new data, when synthesized with our developing isochemical psuedosection models, quartz fabric analyses, and pre-existing geo- and thermochronology data in the region is giving us the ability to unravel multiple phases of Paleozoic orogeneis and in doing so, evaluate and/or reinterpret complex tectonic models of the region. https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/4f1e80be-ea15-4a6b-a7fb-f5635985848c/Fig+1-Tectonic+map.jpg REE Petrochronology - Make it stand out Regional tectonic map of the southern Appalachians. The areal extent of the metamorphic and geo-/thermochronology maps below are indicated by the dark blue outline. Modified from Merschat et al. (2017) and Thigpen et al. (2022). https://images.squarespace-cdn.com/content/v1/55f1cc9fe4b0039bab395d87/1701350109671-X54DUL1T2R3E74DHSYDS/IP-18-05-mg-ka%252528sp2%252529%252Bcopy.jpg REE Petrochronology