Origin of the Felsic and Basaltic Dikes and Flows in the Rajula-Palitana-Sihor Area of the Deccan Traps, Saurashtra, India: A Geochemical and Geochronological Study-Reference-Cited by-同舟云学术

Origin of the Felsic and Basaltic Dikes and Flows in the Rajula-Palitana-Sihor Area of the Deccan Traps, Saurashtra, India: A Geochemical and Geochronological Study

Published:2001-12 Issue:12 Volume:43 Page:1094-1116
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Chatterjee Nilanjan¹,Bhattacharji Somdev²

Affiliation:

1. a Department of Earth, Atmospheric, and Planetary Sciences , Massachusetts Institute of Technology , Cambridge, Massachusetts, 02139

2. b Department of Geology , Brooklyn College of the City University of New York , Brooklyn, New York, 11210

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206810109465063

Reference54 articles.

1. Auden, J. B. 1949.Dykes in western India–a discussion of their relationships with the Deccan Traps, Vol. III/3, 127–157. India: Transactions of National Institute of Science.

2. Stratigraphy, composition and form of the Deccan Basalts, Western Ghats, India

3. Petrogenetic Aspects of Acid and Basaltic Lavas from the Paran Plateau (Brazil): Geological, Mineralogical and Petrochemical Relationships

4. Indian Intraplate and Continental Margin Rifting, Lithospheric Extension, and Mantle Upwelling in Deccan Flood Basalt Volcanism near the K/T Boundary: Evidence from Mafic Dike Swarms

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