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Showing 1–8 of 8 results

Advanced filters: Author: Gail Christeson Clear advanced filters

Inconsistent correlation of seismic layer 2a and lava layer thickness in oceanic crust

Gail L. Christeson
Kirk D. McIntosh
Jeffrey A. Karson
Research25 Jan 2007
Nature

Volume: 445, P: 418-421
A geological carbon cycle sink hosted by ocean crust talus breccias

Mass-wasting deposits that accumulated against mid-ocean ridge faults have high porosity in which calcium carbonate precipitated, storing seawater carbon dioxide, as revealed by cores of a 61-million-year-old seafloor talus deposit.

Rosalind M. Coggon
Elliot J. Carter
Trevor Williams
ResearchOpen Access24 Nov 2025
Nature Geoscience

Volume: 18, P: 1279-1286
Size and morphology of the Chicxulub impact crater

Jo Morgan
Mike Warner
Alberto Trejo
Research04 Dec 1997
Nature

Volume: 390, P: 472-476
Journal club

Gail Christeson
Research Highlights10 Jun 2009
Nature

Volume: 459, P: 755
Importance of pre-impact crustal structure for the asymmetry of the Chicxulub impact crater

The final geometry of an impact crater can be significantly influenced by the geological and geomorphological structure of the impact site; therefore, it may not on its own provide accurate information regarding the direction and angle of impact.

Sean P. S. Gulick
Penny J. Barton
Mike R. Warner
Research13 Jan 2008
Nature Geoscience

Volume: 1, P: 131-135
Rapid recovery of life at ground zero of the end-Cretaceous mass extinction

Micro- and nannofossil, trace fossil and geochemical evidence from the Chicxulub impact crater demonstrates that proximity to the asteroid impact site did not determine rates of recovery of marine ecosystems after the end-Cretaceous mass extinction.

Christopher M. Lowery
Timothy J. Bralower
William Zylberman
Research30 May 2018
Nature

Volume: 558, P: 288-291
Author Correction: Rock fluidization during peak-ring formation of large impact structures

Ulrich Riller
Michael H. Poelchau
Timothy J. Bralower
Amendments and Corrections13 Nov 2018
Nature

Volume: 564, P: E36
Rock fluidization during peak-ring formation of large impact structures

Catastrophic rock weakening upon impact of a meteorite, and hence flow, is shown to be followed by regained rock strength that enabled the formation of the peak ring during cratering.

Ulrich Riller
Michael H. Poelchau
Timothy J. Bralower
Research24 Oct 2018
Nature

Volume: 562, P: 511-518