The use of heavy mineral correlation for determining the source of impact ejecta: A Manicouagan distal ejecta case study

Author:

Thackrey S.,Walkden G.,Indares A.,Horstwood M.,Kelley S.,Parrish R.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference42 articles.

1. Isotopic comparison of K/T boundary impact glass with melt rock from the Chicxulub and Manson Impact structures;Blum;Nature,1993

2. Origin and diagenesis of K/T impact spherules — from Haiti to Wyoming and beyond;Bohor;Meteoritics,1995

3. Low-temperature alteration of volcanic glass: hydration, Na, K, O18 and Ar mobility;Cerling;Chem. Geol.,1985

4. Transformation of Fe–Ti gabbro to coronite, eclogite and amphibolite in the Baie du Nord segment, Manicouagan imbricate zone, eastern Grenville province;Cox;J. Metamorph. Geol.,1999

5. Geology and petrology of the Manicouagan resurgent caldera, Quebec;Currie,1972

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