Search for microremnants of the Tunguska Cosmic Body
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Cited by (42)
New evidence of meteoritic origin of the Tunguska cosmic body
2013, Planetary and Space ScienceCitation Excerpt :The blast was estimated to be equivalent to 3–5 megatons of trinitrotoluene (e.g. Boslough and Crawford, 2008), and it burned and flattened taiga forests over an area >2000 km2. The origin of the Tunguska blast was explained by a huge meteorite impact (e.g. Yavnel, 1957; Florensky, 1963; Longo et al., 1994; Serra et al., 1994; Longo, 2007; Gasperini et al., 2007, 2009; Badyukov et al., 2011) or by a comet (e.g. Florensky et al., 1968a, 1968b; Golenetsky et al., 1977; Ganapathy, 1983; Zbik, 1984; Nazarov et al., 1990; Hou et al., 1998; Kolesnikov et al., 1999, 2003, 2005; Rasmussen et al., 1999; Gladysheva, 2007), or by a cosmic body. However, no clear differences between comet and meteorite impacts were established (Dolgov et al., 1973; Nazarov et al., 1983; Hou et al., 2000, 2004; Kolesnikov et al., 2005).
Wildfire and abrupt ecosystem disruption on California's Northern Channel Islands at the Ållerød-Younger Dryas boundary (13.0-12.9 ka)
2008, Quaternary Science ReviewsCitation Excerpt :Magnetic microspherules are concentrated at the base of the best dated of these distinctive black layers at Murray Springs, AZ (Haynes, 2008) and in association with an assemblage of numerous other exotic materials identified in many other terminal Clovis-age deposits (Firestone et al., 2007). Many of these exotic materials are found in sediments associated with documented extraterrestrial impact events (e.g., Cretaceous–Tertiary [K/T] boundary [Köeberl, 2007]; Tunguska [Longo et al., 1994]). Although much remains to be learned about this boundary layer, the co-occurrence of these exotic materials forms the basis of the Younger Dryas Boundary (YDB) cosmic impact hypothesis (Firestone et al., 2007).
Platinum group element abundances in a peat layer associated with the Tunguska event, further evidence for a cosmic origin
2004, Planetary and Space Science