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Tamara J. Goldin

Researcher at University of Vienna

Publications -  10
Citations -  1431

Tamara J. Goldin is an academic researcher from University of Vienna. The author has contributed to research in topics: Impact crater & Extinction event. The author has an hindex of 8, co-authored 10 publications receiving 1222 citations. Previous affiliations of Tamara J. Goldin include Tulane University & University of Arizona.

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The Chicxulub Asteroid Impact and Mass Extinction at the Cretaceous-Paleogene Boundary

TL;DR: Records of the global stratigraphy across this boundary are synthesized to assess the proposed causes of the Cretaceous-Paleogene boundary and conclude that the Chicxulub impact triggered the mass extinction.
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Footwall topographic development during continental extension

TL;DR: In this paper, the authors examine the progressive development of footwall topography associated with a set of active normal faults in the northeastern Basin and Range Province of the western United States and show that patterns of catchment area, footwall relief, and catchment outlet spacing vary predictably and are related to the growth of the rangebounding normal fault array.
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Self-shielding of thermal radiation by Chicxulub impact ejecta: Firestorm or fizzle?

TL;DR: In this article, the atmospheric reentry of spherules arriving at distal sites is modeled using a two-phase fluid flow code, which includes ejecta and air opacities in a radiative transfer calculation, and the models predict a pulse of thermal radiation at the surface peaking at 5-15 kW/m 2, analogous to an oven set on "broil" (~260° C).
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Revisiting wildfires at the K‐Pg boundary

TL;DR: In this article, the authors proposed that the desiccation of flora by ejecta reentry, as well as the effects of postimpact global cooling/darkness, left much of the terrestrial flora prone to fires, and that the volume of soot in the global K-Pg layer is explained by a combination of syn- and postimpact wildfires.
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Hydrocode Modeling of the Sierra Madera Impact Structure

TL;DR: In this article, the authors presented the first hydrocode simulations of the formation of the Sierra Madera structure (west Texas, USA), which was caused by an impact into a thick sedimentary target sequence.