Comment on: "did Deccan volcanism pre-date the Cretaceous-Tertiary transition?"

Earth and Planetary Science Letters

Volumn 122, Issue 1-2, 1994, Pages 259-262

  Feraud G ^a   Courtillot, V ^b  

^a CNRS   (France)

^b INSTITUT DE PHYSIQUE DU GLOBE DE PARIS   (France)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 0001023462     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/0012-821X(94)90068-X     Document Type: Article

References (19)

1. Did Deccan volcanism pre-date the Cretaceous/Tertiary transition?
2. Rapid eruption of the Deccan flood basalts at the Cretaceous-Tertiary boundary
3. 39Ar stepwise degassing technique
4. 39Ar dating
5. 40Ar dating
6. 39Ar ages for the alkaline volcanism and the basement of Gorringe Bank, North Atlantic Ocean
7. 39Ar dating of the Siberian Traps, USSR: Evaluation of the ages of the two major extinction events relative to episodes of flood-basalt volcanism in the USSR and the Deccan Traps, India
8. Deccan flood basalts and the Cretaceous/Tertiary boundary
9. Paleomagnetism and age determinations of Deccan traps: results of a Nagpur-Bombay traverse and review of earlier work
10. 39Ar age of Cretaceous-Tertiary boundary tektites from Haiti
11. Datation par la méthode potassium-argon de la limite Crétacé-Paléogène en milieu marin:aˆge des verres de Béloc (Haïti)
12. 39Ar ages of 65.0 million years ago from Chicxulub crater melt rock and Cretaceous-Tertiary boundary tektites
13. New links between the Chixculub impact structure and the Cretaceous/Tertiary boundary
14. A radiometric age for the Cretaceous-Tertiary boundary based upon KAr, RbSr and UPb ages of bentonites from Alberta, Saskatchewan and Montana
15. Deccan flood basalts at the Cretaceous/Tertiary boundary?
16. Paleomagnetic constraints on the structure of the Deccan traps
17. Duration of Deccan trap volcanism: A statistical approach
18. The Cretaceous/Tertiary boundary impact hypothesis and the paleontological record
19. Gradual mass extinction, species survivorship, and long-term environmental changes across the Cretaceous-Tertiary boundary in high latitudes