Serpentinization as a Possible Cause of High Heat-flow Values in and near the Oceanic Ridges
- 1 February 1964
- journal article
- Published by Springer Nature in Nature
- Vol. 201 (4921), 807-808
- https://doi.org/10.1038/201807b0
Abstract
No abstract availableKeywords
This publication has 5 references indexed in Scilit:
- Equilibrium calculations in the system Mg, Fe, Si, O, H, and NiAmerican Journal of Science, 1963
- Hypothesis of Earth's BehaviourNature, 1963
- Evidence from Islands on the Spreading of Ocean FloorsNature, 1963
- Properties of water; part VI, Entropy and Gibbs free energy of water in the range 10-1000 degrees C and 1-250,000 barsAmerican Journal of Science, 1960
- THE SYSTEM MgO—SiO2—H2OGSA Bulletin, 1949