Abstract-More than 30 impact structures have been discovered in the last three decades in northeastern Eurasia, which includes Russia, Ukraine, Belarus, Lithuania, Latvia, Estonia, Kazakhstan, and Mongolia. The largest impact events of the twentieth century also occurred here: the Tunguska and Sikhote Alin events in Siberia and Primorye, respectively. Many of these impact structures have been studied in detail. This is particularly the case for the largest examples: Popigai (1 00 km), Puchezh-Katunki (80 km), and Kara (65 km). Detailed data and descriptions of the geological characteristics, morphology, and the nature of the impact breccias and impactites (impact-melt rocks) are to be found in numerous publications published mostly in Russian. As these data and descriptions are not generally available to non-Russian scientists, this review summarizes the current state of knowledge on these impact structures. It also provides references to the urincipal publications detailing them.

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Abstract-About three decades ago, a formerly unknown genetic type of natural diamonds was discovered in impact craters. Impact diamonds are currently known from a number of impact structures in Europe, Asia and North America, and it's likely that the number of finds will increase with time. The Popigai crater, Northern Siberia, where impact diamonds were first found, was specifically investigated in terms of geology, geophysics, petrography and mineralogy. Large resources of industrial impact diamonds were discovered, and these minerals were studied in detail.Authigenic impact diamonds occur in situ in shocked graphite-bearing gneisses that are found as inclusions in impact melt rocks: tagamites and suevites. According to the observed transformation of coexisting minerals, the lower estimated pressure of the coherent martensite transition of graphite to diamonds is 35 GPa. Impact diamonds inherit the original shape of graphite crystals and are composed of a polycrystalline structured aggregate of cubic and probably hexagonal carbon microcrystals 1-5 pm across. Numerous properties of diamonds depend on the high density of defects in the crystal lattice. Allothigenic impact diamonds occur in rocks produced by the homogenization and solidification of impact melt, which originated from the complete fusion of graphite-bearing precursor gneisses. These diamonds usually reflect the influence of the hot melt and are strongly corroded.Diamond-bearing tagamites and suevites in the Popigai crater interior occur as extended lens and sheets bodies and also as irregular small bodies. Diamond distribution depends on the original abundance of precursor graphite in the target rocks, on the superimposed shock-metamorphic zonation, and on the character of the ejection of shocked and melted material along different trajectories and azimuths. This has resulted in radial and concentric inhomogeneities in diamond distribution in the crater interior. On a second order, the distribution depends on the scale of melt contamination by clasts and fragments and by the duration of cooling of certain melt bodies and their constituents. Enrichment in diamonds at the margins of thick tagamite sheets is the result of rapid cooling, which prevents combustion of diamonds. A positive correlation between diamond content and the amount of phosphorus pentoxide in impactites indicates links to C and P probably in organic matter of the primary sedimentary rocks, which were subjected to granulitic metamorphism 2.4 Ga ago and melted at the time of impact 35.7 Ma ago.