High- 3 He Plume Origin and Temporal-Spatial Evolution of the Siberian Flood Basalts-Reference-Cited by-同舟云学术

High- 3 He Plume Origin and Temporal-Spatial Evolution of the Siberian Flood Basalts

Published:1995-08-11 Issue:5225 Volume:269 Page:822-825
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Basu Asish R.¹,Poreda Robert J.¹,Renne Paul R.²,Teichmann Friedrich¹,Vasiliev Yurii R.³,Sobolev Nikolai V.³,Turrin Brent D.⁴

Affiliation:

1. Department of Earth and Environmental Sciences, University of Rochester, Rochester, NY 14627, USA.

2. Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709-1211, USA.

3. Institute of Mineralogy and Petrology, Russian Academy of Sciences, Siberian Branch, Novosibirsk 630090, Russia

4. U.S. Geological Survey, Mailstop 901, 345 Middlefield Road, Menlo Park, CA 94025, USA, and Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709-1211, USA.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference35 articles.

1. APLONOV, S, AN ABORTED TRIASSIC OCEAN IN WEST SIBERIA, TECTONICS 7: 1103 (1988).

2. Early and Late Alkali Igneous Pulses and a High- 3 He Plume Origin for the Deccan Flood Basalts

3. Butakova, E. L., The Alkaline Rocks 172 (1974).

4. Synchronism of the Siberian Traps and the Permian-Triassic Boundary

5. CARLSON, R.W., COLUMBIA RIVER VOLCANISM - THE QUESTION OF MANTLE HETEROGENEITY OR CRUSTAL CONTAMINATION - REPLY, GEOCHIMICA ET COSMOCHIMICA ACTA 47: 845 (1983).

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