Jv
Member Since 2002
Jolante van Wijk
Science Manager, Los Alamos National Laboratory
AGU Research
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An Updated Tectonic Reconstruction for the Caroline Plate (Western Pacific) Incorporating Age Constraints on Oceanic Plateau Construction and Kinematic Effects of Plateau-Subduction Zone Interaction
QUANTIFYING DEFORMABLE PLATE MODELS OF CIRCUM-PACIFIC AND TETHYAN DOMAINS POSTER
tectonophysics | 14 december 2023
Samuel Martin, Nicholas Ellis, Jolante van Wijk
New age constraints on oceanic plateau construction in the western Pacific elucidate a history of plateau-subduction zone interaction and its influenc...
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Ongoing Developments for the Probabilistic Volcanic Hazard Assessment of Valles Caldera and the Jemez Mountains Volcanic Field, NM, USA
DISTRIBUTED VOLCANIC FIELDS: SCIENCE, HISTORIES, AND HAZARDS POSTER
volcanology, geochemistry and petrology | 13 december 2023
Matthew R. Sweeney, Anita Lavadie-Bulnes, Charlott...
Large caldera systems can pose hazards long after their last voluminous eruptions, often times in the form of more distributed, smaller volume eruptio...
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End-Loading by Short Flat Slabs: Numerical Modeling Applied to the Laramide and Sierra Pampeanas Orogenies
OROGENY AND ITS PROCESSES I POSTER
tectonophysics | 12 december 2023
Noah Hobbs, Jolante van Wijk
Driving mechanisms for compressional deformation of continental lithosphere far (>800 km) from current or fossil subduction zones such as the Creta...
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What Causes Cyclic Stratigraphy on Rifted Margins?
FROM CONTINENTAL RIFTS TO RIFTED MARGINS III POSTER
tectonophysics | 11 december 2023
Jolante van Wijk, Reilly Blocho
Cyclic stratigraphy on rifted margins has traditionally been explained by eustatic sea level changes, resulting in the creation of sea level history c...
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Lateral Rift Propagation: A Top-Down or Bottom-Up Process?
FROM CONTINENTAL RIFTS TO RIFTED MARGINS I ORAL
tectonophysics | 11 december 2023
Folarin Kolawole, Rasheed Ajala, Jolante van Wijk
Continental rift systems grow by the lateral propagation, interaction, linkage, and coalescence of isolated rift segments. Prior to linkage and coales...
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Progressive flat-slab coupling as a driving mechanism for the Laramide orogeny
UNUSUAL SUBDUCTION PROCESSES III ORAL
study of earth's deep interior | 16 december 2022
Noah Hobbs, Jolante van Wijk, Gary J. Axen
Plate boundary conditions (i.e., end loading vs basal traction) that drive intraplate deformation along inherited weaknesses are poorly studied by geo...
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Steps Toward Developing a Volcano Hazard Assessment for the Jemez Mountains Region, Northern New Mexico, USA
VOLCANO HAZARD MONITORING USING STATISTICAL METHODS AND ARTIFICIAL INTELLIGENCE II ORAL
volcanology, geochemistry and petrology | 16 december 2022
Charlotte A. Rowe, Jolante van Wijk, Matthew R. Sw...
The Jemez Volcanic Field in Northern New Mexico, situated within the actively extending Rio Grande mid-continental rift zone, is one of many volcanic ...
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Indus and Bengal Fan Loading of the Indian Plate Explains Intraplate Deformation Patterns
CONTINENTAL COLLISIONS: STRUCTURE AND EVOLUTION IV ORAL
tectonophysics | 13 december 2022
Jolante van Wijk, Joseph Zinecker, David D. Coblen...
The northern Indian Plate provides a unique location to evaluate the combined effects of large-scale tectonics and small-scale geomorphological proces...
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