2 Known and 6 Suspected Large-Bolide Impacts on Earth, with Plate Boundaries and Current GPS Plate Horizontal Velocities. 

Click here to download the Google Earth KMZ implementation of this map (GPSmotions.kmz  1KB)

Far-field strains on Earth from 2 known (Chicxulub and Chesapeake) and 6 suspected impact sites (Canada basin, Congo basin, Mid-Pacific Mountains, Norfolk basin, Shaanxi, South Georgia) are shown below. Splash rings are shown using colored line traces at 660, 1550 and 2900 km radius around each impact. The rings trace circumferential regions of uplift and subsidence around each site. Black vectors show current, horizontal azimuth and magnitude of tectonic-plate motions based on NASA JPL GPS data. Vector lengths are variably-scaled with the horizontal velocity for each GPS station multiplied by 0.25 geographic degrees. The average horizontal velocity for the crustal plates is about 27 mm/yr based on time-series data for 778 GPS stations. Station points are color coded blue for stations having negative vertical motion (subsidence) and green for positive (uplift), respectively. Red-dashed lines originate at impact craters and extend foreland of each crater in the direction of crustal compression; in line with interpreted paths of oblique descent for the different projectiles.  The thin-dashed, colored lines trace surface features including ocean-floor transform faults and other continental lineaments that highlight crustal fractures and faults that either stem from far-field strains associated with the different impact events, or are perturbed by them. Tectonic-plate boundaries are shown as thick maroon and black lines. The thin gray lines on the sea floor trace the M34 magnetic isochron.

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2 Known and 6 Suspected Impacts, Plate Boundaries and Motions

Plate motions worldwide currently diverge northward away from the suspected South Georgia impacts in the Southwest Atlantic Basin. Exceptions are plate motions associated with the Chicxulub impact and a suspected (Middle Paleozoic?) impact in the Shaanxi province of China. In both of these latter instances, plates pivot around impact sites. These relationships are intended to show that large impact events produce long-lasting geodynamic responses,  probably operating to dissipate energy fluxes imparted by large-impact events.  Moreover, most of these impacts show nearby fragmentation of tectonic plates, especially in hinterland regimes of crustal extension. Large-bolide impacts therefore appear to drastically influence Earth geodynamics to a degree that we are only beginning to realize. The South Georgia event may have occurred in the Middle Miocene during the Langhian (13.65–15.97 mya) stage when there was a sudden warming trend in Antarctica (~15.7 mya ), changes in  Atlantic and Pacific ocean circulation, and subsequent extinction waves of  terrestrial and aquatic life forms (~14.8 to 14.5 mya). The distribution of tektites in the North American tektite strewn field also shows a remarkable spatial coincidence with the proposed foreland trajectory of the Argentine impact even though it is currently thought to stem from the Chesapeake impact of Eocene age (~35 Ma).

www.impacttectonics.org  03052008