Izett G A, Dalrymple G B, Snee L W
Science. 1991 Jun 14;252(5012):1539-42. doi: 10.1126/science.252.5012.1539.
(40)Ar/(39)Ar dating of tektites discovered recently in Cretaceous-Tertiary (K-T) boundary marine sedimentary rocks on Haiti indicates that the K-T boundary and impact event are coeval at 64.5 +/- 0.1 million years ago. Sanidine from a bentonite that lies directly above the K-T boundary in continental, coal-bearing, sedimentary rocks of Montana was also dated and has a (40)Ar/(39)Ar age of 64.6 +/- 0.2 million years ago, which is indistinguishable statistically from the age of the tektites.
最近在海地白垩纪-古近纪(K-T)边界海洋沉积岩中发现的玻陨石的氩-氩(Ar/Ar)年代测定表明,K-T边界和撞击事件发生在同一时期,即6450万年前,误差范围为正负0.1百万年。对蒙大拿州含煤大陆沉积岩中位于K-T边界正上方的膨润土中的透长石也进行了年代测定,其氩-氩(Ar/Ar)年龄为6460万年前,误差范围为正负0.2百万年,在统计学上与玻陨石的年龄无法区分。