Detection of real periodicity in the terrestrial impact crater record: quantity and quality requirements J. Lyytinen – L. Jetsu – P. Kajatkari – S. Abstract Aims. To determine the quantity and quality requirements for the terrestrial impact crater data which would allow reliable detection of real periodicity.
List of impact craters on Earth
Earth Syst. Burrows; M. Maltrud; X. Yang; Q. Zhu; N. Jeffery; X.
To date, there are confirmed impact structures in the database. When a meteor hits Earth, terrestrial rocks at the impact site can liquefy from the.
We use them to give you the best experience. If you continue using our website, we’ll assume that you are happy to receive all cookies on this website. Sign up here for GlobalData’s free bi-weekly Covid report on the latest information your industry needs to know. Minutes later, the jumbo jet, bound for Tokyo, struck an approach lighting structure at the end of the strip, significantly damaging the aircraft. Having managed to take off, the breached Boeing circled over the Pacific Ocean while jettisoning fuel, before safely touching back down shortly afterwards.
In the historical ledger of aviation accidents, these events from nearly half a century ago barely get a mention. There were no fatalities among the passengers, although two sustained serious injuries at the hands of rods from the lighting structure which tore through the passenger compartment. But the incident was deemed serious enough at the time by the US Federal Aviation Administration FAA to warrant the introduction of new rules around airport structures, designed to break, distort or yield on impact with an aircraft — thus minimising potential damage to life and property.
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40Ar/39Ar dating of sanidine and hydrothermally grown adularia separated from impact-metamorphosed gneiss from the Rochechouart impact structure yielded.
Search publications Advanced search. Steven Goderis UGent. Downloads Download. Goderis, Steven. Projectile identification in terrestrial impact structures and ejecta material. Ghent University. Faculty of Science. Goderis S. Faculty of Science;
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terrestrial impact craters.
Biren, Brian D. Monteleone, Jahandar Ramezani, John G. Spray, Lucy M. The accurate dating of meteorite impact structures on Earth has proven to be challenging. In cases where high-temperature shock metamorphism of the target materials has occurred without widespread melting, these isotopic chronometers may be partially reset and yield dates that are difficult to interpret unambiguously as the age of impact.
Nine zircons from a melt sheet sample yield a weighted mean age of In contrast, five apatites from this sample yield dates between
Frangible structures: minimum impact for maximum safety
Pidgeon, a A. Nemchin, a S. This article is one of a series of papers published in this Special Issue on the theme of Geochronology in honour of Tom Krogh. There have been a number of reports of the presence of shock features, such as planar fracturing and granulation, the transformation of zircon to reidite, and the breakdown of zircon to baddeleyite in zircons associated with terrestrial impacts.
It has also been proposed that the progressive development of these shock features, and the degree of disturbance of the zircon U—Pb isotopic system, could be used as a qualitative measure of the shock pressures and post-shock temperatures of the impact.
Currently, only 21 terrestrial impact structures are precisely and accurately dated, and the only proven age concordance is between the.
Darlington, V. The structure consists of a central area ca. The Century PbZn mine is located on the southern edge of the limestone annulus. The Limestone Annulus: The limestone annulus may be a unique structure for terrestrial impacts. It consists of beds that are tightly folded and faulted on a scale of several hundred meters, with little systematic structure apart from a generally circumferential orientation, and breccia dykes.
The thickness of the annulus is locally four times greater than adjacent undisturbed sections of the limestone. The width of the annulus varies from 2 km in the west to over 5 km in the east, and the margins of the annulus are grossly polygonal. Origin of the Limestone Annulus: The limestone annulus may have originated as sedimentary infill of a crater, ejecta around a rampart crater, or as an allochthonous deposit that occurred at the early crater modification stage within the transient crater.
The deformed but partially coherent nature of the limestone and its volume argue strongly against the first two possibilities.
Dating Terrestrial Impact Structures
Items in OPUS are protected by copyright, with all rights reserved, unless otherwise indicated. Show full item record. Schmieder, Martin. However, no geologic evidence for the multiple Late Triassic impact scenario has been presented since that time. The new results are set in the context of recent chronological data available for the Lake Saint Martin impact structure, geochemical data, and the physical background of impact crater chain formation.
Furthermore, paleoenvironmental implications are discussed.
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Special Topic: Terrestrial Impact Craters
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