The Melting Curve of Iron to 250 Gigapascals: A Constraint on the Temperature at Earth's Center-Reference-Cited by-同舟云学术

The Melting Curve of Iron to 250 Gigapascals: A Constraint on the Temperature at Earth's Center

Published:1987-04-10 Issue:4798 Volume:236 Page:181-182
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Williams Quentin¹,Jeanloz Raymond¹,Bass Jay²,Svendsen Bob³,Ahrens Thomas J.³

Affiliation:

1. Department of Geology and Geophysics, University of California, Berkeley, CA 94720.

2. Department of Geology and Geophysics, University of Illinois at Champaign-Urbana, Champaign, IL 61820.

3. Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference33 articles.

1. AHRENS, T.J., CONSTRAINTS ON CORE COMPOSITION FROM SHOCK-WAVE DATA, PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY OF LONDON SERIES A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES 306: 37 (1982).

2. ANDERSON, O.L., PROPERTIES OF IRON AT THE EARTHS CORE CONDITIONS, GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY 84: 561 (1986).

3. High Pressure Research in Mineral Physics 1987

4. BIRCH, F, MELTING RELATIONS OF IRON, AND TEMPERATURES IN EARTHS CORE, GEOPHYSICAL JOURNAL OF THE ROYAL ASTRONOMICAL SOCIETY 29: 373 (1972).

5. BIRCH, F, ELASTICITY AND CONSTITUTION OF THE EARTH INTERIOR, JOURNAL OF GEOPHYSICAL RESEARCH 57: 227 (1952).

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