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its age is estimated to be about 600 million years (late neoproterozoic).
vârsta sa este estimată la 600 milioane ani (neoproterozoicul timpuriu).
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==geology==during the neoproterozoic, older parts of the armorican massif formed the northern margin of the paleocontinent gondwana.
În timpul neoproterozoicului, părțile mai vechi ale masivului armorican au făcut parte din marginea nordică a paleocontinentului gondwana.
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impact took place after folding of the paleoproterozoic rocks but before deposition of neoproterozoic and cambrian rocks which overlie them, thus constraining the impact event to the interval between about 1660 and 600 ma.
impactul a avut loc după plierea rocilor din paleoproterozoic, dar înainte de depunerea din neoproterozoic și a rocilor din cambrian, astfel, evenimentul de impact este estimat pentru intervalul dintre 1660 milioane ani și 600 milioane ani.
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==references==* carr, j and link, pk, 1999, neoproterozoic conglomerate and breccia in the formation of leaton gulch, grouse peak, northern lost river range, idaho: relation to beaverhead impact structure, in hughes, s.s., and thackray, g.d., eds., "guidebook to the geology of eastern idaho": pocatello, idaho museum of natural history, p. 21-29.
== vezi și ==* lista craterelor de impact de pe pământ* lista craterelor de impact din america de nord* craterul chesapeake bay== referințe ==== bibliografie ==* carr, j and link, pk, 1999, neoproterozoic conglomerate and breccia in the formation of leaton gulch, grouse peak, northern lost river range, idaho: relation to beaverhead impact structure, in hughes, s.s., and thackray, g.d., eds., "guidebook to the geology of eastern idaho": pocatello, idaho museum of natural history, p. 21-29.
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