North American Plate, Mid-Atlantic Inversion Resulting from the Chesapeake Invader

Download the New Jersey region  KMLZs/2015 Chesapeake Invader Virginia USA.kmz (3.5 MB)                                        Rev. 05/2017

A hypervelocity bolide of about 3-5 km diameter indented the Chesapeake Bay about 35 million-years ago. The impact probably directed a northward tectonic push in the direction of the flight path, assumed to be  moderately inclined to the Earth's surface along the NW axis of the bay as illustrated below. The strain field stemming from the impact is shown as being centered in the Pennsylvania Salient, including the Juniata Culmination (JC). The field is wedge shaped and includes three major river courses radiating outward from the point of impact toward the foreland, cutting through crustal strata along zig-zagged paths that mimic currently rising and subsiding regions. It is quite possible that a regional uplift would have resulted after the impact from crustal contraction with impact-generated sets of fractures, folds, and faults. The river courses may have developed along paths of dense fracturing with unroofing of  foreland areas beginning in the Late Eocene. Nearby oceanic margin deposits now include a regional Oligocene unconformity topped by Miocene age and younger strata.

Netectonic Framework Mid-Atlanitc, NAP

The Potomac, Susquehanna, and Delaware river systems continue to feed the continental shelf today. These major rivers my have formed or modified as part of the strain reposnses to impact stresses. Sets of fractures, folds and faults that developed at relatively late stages in the tectonic history of the Mesozoic Newark Basin, Pennsylvania and New Jersey (nb - above), indicate NE directed strain (JW above). Wise (2004) shows that late-stage extension fractures joints fanned out laterally across the culmination in Paleozoic rocks. Naiser and others (2001) report that major east-flowing Mid-Atlantic rivers did not breach the Blue Ridge until early or middle Miocene time. Impact-related fractures therefore may have formed within a contracted crustal wedge lying above deep-seated, crustal block faults that may have readjusted, or perhaps formed in direct response to impact stresses.  Eocene igenous rocks occur along the southern margin of the proposed wedge near the upper reaches of the Potomac river near a linear swarm of historical seismicity. Crustal isotopic data from sulfide-mineralzied fault breccia through the foreland wedge not only date back to the event, but have crustal concetrations indicating impact-related fractures penetrated to mantle depths. A pronounced, closed gravity anomaly (yellow) occupies a congruent position on the other side of the culmination to the NE. It therefore appears that the Chesapeake Invader (Poag, 1999) helped shape today's regional landscape and current neotectonic setting of the mid-Atlantic foreland region.

Lithosphere manuscript Figure 5

Screen capture of a GE display showing the Chesapeake impact crater with respect to the resulting crustal blast pattern, regional basement structure contours (feet) atop Precambrian basement (Rickard , 1973; Baranoski, 2013),  CAMP dolerite dikes (Herman and others, 2015) deep basement faults of the Rome trough (deWitt, 1993), and linear traces of strong aeromagnetic positive amomolies seen in the global potential field data of Maus and others (2017). Crustal-compaction values gained from calcite-strain-guage data  by Engelder (1979), Spang and Groshong (1981), Lomando and Engelder (1984), Craddock and others (1993), and Ong and others (2007).  Green circles trace approximate crestlines of lithospheric arches lying circumferential to the crater shown at 300 and 760 kilometers radius from the crater that bracket interening troughs represented in profile in figure 6. The Westminster arch (Campbell, 1929) is highlighted using yellow structural contours and a red, doubly plunging crestline.   This arch affects only lowest Tertiary gravels laid down prior to impact.

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